"Gates of the Arctic National Park and Preserve Scenery" by U.S. National Park Service , public domain
Gates Of The Arctic
National Park & Preserve - Alaska
Gates of the Arctic National Park and Preserve is a U.S. National Park in Alaska. It is the northernmost national park in the U.S. (the entirety of the park lies north of the Arctic Circle) and the second largest at 8,472,506 acres (3,428,702 ha), slightly larger in area than Belgium. The park consists primarily of portions of the Brooks Range of mountains. A large part of the park is protected in the Gates of the Arctic Wilderness which covers 7,167,192 acres (2,900,460 ha). The wilderness area adjoins the Noatak Wilderness Area and together they form the largest contiguous wilderness in the United States.
Map of Winter Recreation in the White Mountains National Recreation Area and Steese National Conservation Area in Alaska. Published by the Bureau of Land Management (BLM).
Map of Summer Recreation in the White Mountains National Recreation Area and Steese National Conservation Area in Alaska. Published by the Bureau of Land Management (BLM).
Map of the National Parks in Alaska. Published by the National Park Service (NPS).
https://www.nps.gov/gaar/index.htm
https://en.wikipedia.org/wiki/Gates_of_the_Arctic_National_Park_and_Preserve
Gates of the Arctic National Park and Preserve is a U.S. National Park in Alaska. It is the northernmost national park in the U.S. (the entirety of the park lies north of the Arctic Circle) and the second largest at 8,472,506 acres (3,428,702 ha), slightly larger in area than Belgium. The park consists primarily of portions of the Brooks Range of mountains. A large part of the park is protected in the Gates of the Arctic Wilderness which covers 7,167,192 acres (2,900,460 ha). The wilderness area adjoins the Noatak Wilderness Area and together they form the largest contiguous wilderness in the United States.
This vast landscape does not contain any roads or trails. Visitors discover intact ecosystems where people have lived with the land for over ten thousand years. Wild rivers meander through glacier-carved valleys, caribou migrate along age-old trails, endless summer light fades into aurora-lit night skies of winter. Virtually unchanged, except by the forces of nature.
Gates of the Arctic is a wilderness park, with no roads or trails into the park lands, so visitors must fly or hike into the park. Access begins in Fairbanks, Alaska & there are several small airlines that provide daily flights into the communities of Bettles, Anaktuvuk Pass, and Coldfoot. Most visitors access the park by air taxi or hike in from the Dalton Highway or from the village of Anaktuvuk Pass. River crossings are necessary from both locations.
Anaktuvuk Pass Ranger Station
The Anaktuvuk Pass Ranger Station is staffed during the summer season from April through September, typically Monday-Friday, 9-5:30. Here you can learn about the park, and gain advice on hiking routes in the area. Bear Resistant Food Containers are available to borrow as well. Outside display is open year-round.
The Anaktuvuk Pass Ranger Station is located in the center of the village, on Main Street.
Arctic Interagency Visitor Center
Multi-agency visitor center located on the Dalton Highway in Coldfoot, Alaska
West side of Dalton Highway, opposite of Coldfoot Camp
Bettles Ranger Station and Visitor Center
The Bettles Ranger Station is situated outside of the boundaries of Gates of the Arctic National Park & Preserve, in Bettles, Alaska. This small ranger station and visitor center has exhibits, park-related films, interpretive programs, and trip-planning tools.
Across Airport Road from the Bettles airport
Fairbanks Alaska Public Lands Information Center
Explore world-class exhibits, watch a free informative movie, and receive assistance on your trip planning needs while at the Alaska Public Lands Information Center, located inside of the Morris Thompson Cultural & Visitors Center in Fairbanks, Alaska.
Located in downtown Fairbanks, on the corner of Wendell and Dunkel Streets
Alatna River
Aerial view of the Alatna River as it winds through a valley
Aerial view of the Alatna River as it winds through a valley
Arrigetch Peaks
Alpenglow on the granite cliffs of mountains
A spring alpenglow brightens the granite walls of the Arrigetch Peaks
Entering Oolah Valley
A hiker crosses a stream with mountains in the background
A hiker crosses a stream and enters Oolah Valley.
Blueberries
Handful of blueberries
Pausing to pick blueberries can result in a handful of delicious snacks.
Hikers crossing a mountain pass
Two hikers climb up a mountain pass
Hikers choose river valleys as corridors when hiking over mountain passes.
Nellie Cashman
Learn about Nellie Cashman: businesswoman, miner, prospector, philanthropist, voter.
painting of a young woman
Home, home on your range?
Read the abstract and get the link to a paper published in the Journal of Wildlife Management about the overlap across four Arctic caribou herds: Prichard, A. K., L. S. Parrett, E. A. Lenart, J. R. Caikoski, K. Joly, and B. T. Person. 2020. Interchange and overlap among four adjacent Arctic caribou herds. Journal of Wildlife Management 1-15.
Caribou in brushy northern forest.
Permafrost Resource Brief for the Arctic Network
Permafrost underlies most of the Arctic Network and affects nearly everything in the arctic ecosystem. Thawing permafrost also changes the local hydrology and creates the second-greatest disturbance to boreal forests, after wildfires. Recent warm and wet conditions caused some thaw of ice masses and surface subsidence in Arctic parks that ultimately led to a record number of drained of shallow lakes. This brief provides an update on permafrost monitoring in the Arctic Network
Polygonal shaped tundra due to underlying permafrost
Rachel Riley
As one of the last remaining persons to have completed The Long Walk - a major and permanent move to the final destination of the previously nomadic Nunamiut people - Rachel Riley was a leading advocate for the continuing knowledge and practice of the traditional Nunamiut culture. Rachel's most prominent role was as an Inupiaq language teacher.
Rachel Riley as a child in 1949, soon after completing The Long Walk as an eight-year-old girl.
Arctic Cryosphere: snow, water, ice, and permafrost
This article is a summary of findings from the Snow, Water, Ice, and Permafrost in the Arctic report by the Arctic Council Arctic Monitoring and Assessment Programme.
A person dwarfed in the expansive snow-covered tundra of the Arctic.
Snowshoe Hare
Snowshoe hares live in the boreal forests of North America and are active year-round. They gain their curious name from their very large hind feet form a snowshoe, supporting their weight on the surface of the snow. Hares greatly influence the world around them, including the vegetation, predators, and other herbivores and omnivores that live in the same habitats.
a white colored hare under a shrub in snow
A Soil Survey from the Early 1990s Valuable in Today's Decisions
A Soil Survey from the Early 1990s Valuable in Today's Decisions
Abandoned Mine Lands in Alaska National Parks—An Overview
From the thousands of mining claims that existed at when Congress created most national parks in Alaska, around 750 still remain. These are mainly abandoned sites and features, in various stages of disrepair and failure. Since 1981, the NPS has worked to quantify the number and type of hazards posed by these sites and has pursued a variety of solutions to mitigate the issues, such as visitor safety hazards, presented by relic mining features.
dilapidated wood building in a mountainous setting
Subsistence
The study of subsistence resources in parks has been a mix of long-term work and projects instigated by issues facing the Federal Subsistence Board.
Winter hunting is an important subsistence activity in many Alaska communities and park areas.
Alaska Native Place Names in Arctic Parks
Indigenous place names are rich ethnographic and historical resources. Many of them refer to activities that regularly took place at the site; others tell of historical events that occurred there. These names have been replaced by English names on modern maps; this article discusses efforts to document these names into the future.
a group of people near a canvas tent, alongside a large river
Red Fox
Despite the name, red foxes come in a variety of colors. They're found throughout the United States and are not uncommon sightings in many national parks.
two red foxes
Science in Wilderness Marine Reserves
ANILCA establishes the largest scientific laboratory...ever!
A spawning salmon struggles to get back into the water.
A Tribute: Dave Spirtes, 1948-2004
A tribute to a lost colleague and friend, Dave Spirtes.
Dave Spirtes holds an award presented to him by Ron Arnberger, Alaska Regional Director (retired).
2016 Science Education Grant Recipients
The Murie Science and Learning Center (MSLC) funds numerous outreach projects through the Science Education Grant program. These grants help MSLC partner parks pay for science education outreach projects. Funding for the Science Education grant program is provided by Alaska Geographic. Read about the 2016 Science Education Grant recipients and their outreach projects.
a photographer takes a picture in the grass while the sun sets
Prehistoric Obsidian Procurement and Transport in Gates of the Arctic National Park and Preserve
Since the discovery of a prominent obsidian source near the Indian River, a tributary of the Koyukuk, numerous researchers have investigated obsidian use in prehistoric Alaska. Learn more about the studies from Gates of the Arctic National Park and Preserve that have illuminated evidence of an elaborate network of long distance trade and cultural interaction throughout prehistoric Alaska and beyond.
close up of a piece of obsidian with the sunlight shining through it
In Celebration of ANILCA
Former President, Jimmy Carter, offers a sentimental introduction to the 25th Anniversary Edition of Alaska Park Science and the Alaska National Interest Lands Conservation Act (ANILCA).
Black and white photo of six white men standing in front of an old National Park Service Building.
A History of Science in Alaska's National Parks
National park units in Alaska precede the establishment of the National Park Service in 1916. The first park unit, Sitka National Monument, was conceived in 1908, and by the mid-1920s four national monuments along with Alaska’s first national park were part of the growing park system. Discover how the early 1900s and observations of a few helped to establish the National Park Service in Alaska.
Black and white photo of Arno Cammerer sitting at his desk looking through papers.
Old is Getting Older
In the last 25 years, persistent archaeological survey and improved scientific techniques have resulted in new data which confirms that Alaska sites are actually much earlier than we once believed.
NPS archaeologist works at Amakomanak site in Noatak National Preserve.
Tent Ring Archaeology in Gates of the Arctic National Park and Preserve
This article explores what a tent ring is and what cultures of Alaskan people once created them. A big question asked in this article is "Are all the tent rings in Gates of the Arctic attributed to Nunamiut occupations?" Through a series of comparisons of different tent rings, the author eventually reaches an answer to the question and realizes the importance of archaeology in Gates of the Arctic.
A tent ring.
Download Alaska Park Science: Volume 16, Issue 1
Download a print-friendly copy of Volume 16, Issue 1 of Alaska Park Science.
a group of muskox running across a field
Arctic brown bears like salmon, too!
Read the abstract and get the link to an article on the use of salmon streams by brown bears in the Arctic: Sorum, M. S., K. Joly, and M. D. Cameron. 2019. Use of salmon (Oncorhynchus spp.) by brown bears (Ursos arctos) in an Arctic, interior, montane environment. The Canadian Field-Naturalist 133(2):151-155.
A bear stands in a river fishing with two cubs on the bank.
NPS Geodiversity Atlas—Gates Of The Arctic National Park, Alaska
Each park-specific page in the NPS Geodiversity Atlas provides basic information on the significant geologic features and processes occurring in the park.
lone hiker in large valley
Lichens as Indicators
Read the abstract and link to an article on Arctic lichens published in The Bryologist: Nelson P. R., B. McCune, and D. K. Swanson. 2015. Lichen traits and species as indicators of vegetation and environment. The Bryologist 118(3):252-263.
A tiny community of Arctic lichens, including the "pixie cup" Cladonia species.
Fire Communication and Education Grants Enhance Fire Interpretation and Outreach in the National Parks in 2015 and Beyond
The 2015 National Park Service Fire Communication and Education Grant Program provided funding for projects, programs, or tasks in twelve parks around the country.
A woman studies a small coniferous tree while a younger woman looks on.
Land Ownership in National Park System Units in Alaska and Possibilities for Mining and Other Developments
There are over 54 million acres of National Park System units in Alaska, which is 65 percent of the entire National Park System. Although most of those lands are in federal ownership and are managed by the NPS, there are over two million acres of non-federally owned lands within those units. These non-federal lands are in private, state, borough, or municipal ownership. The existence of these lands creates the possibility of mining and other developments within the boundaries
rustic buildings near a creek, hills and mountains in the distance
Studying Arctic Marine Mammals in the Shipping Age
Pod of narwhals, one of the few mammals endemic to the Arctic Ocean. Photo used by permission from Kristin Laidre
A pod of narwhals surfaces in the Arctic.
Fire Ecology Annual Report 2018 Fire Season
Despite the relatively quiet fire season in Alaska in 2018, the National Park Service saw 24 wildfires spanning over 36,000 acres burning within and adjacent to park boundaries. Six of those fires were in Cape Krusenstern National Monument.
An anvil-shaped smoke plume rises above the tree line on the Yukon River.
Building PIO capacity in Alaska
National Park Service Public Information Officers were in short supply last fire season. To help bolster the numbers, NPS Alaska recruits 12 new staff members to assist with all hazard and wildfire incidents.
A fire public information officer highlights updates on a fire to members of the public.
Aurora Borealis: A Brief Overview
A brief overview of how Northern Lights occur.
two ribbons of greenish light in a dark blue sky, over a very dark forest
Hunting and Subsistence Use of Dall Sheep
Learn about the two ways humans harvest sheep - for subsistence use and in sport hunting.
a male sheep
Alaska's Northern Parks: The Wonder of the Arctic
The Arctic is a region characterized by extremes and adaptation. It is rich in natural and cultural history. The articles in this edition of Alaska Park Science highlight the many facets of life in the Arctic.
stone outcrop in the Arctic tundra
Small Mammals as Indicators of Climate, Biodiversity, and Ecosystem Change
This is a time of rapid environmental changes in Alaska. Species that have evolved within tundra habitats over multiple glacial cycles are not only best adapted to high-latitude and high-elevation environments, but may also respond more slowly to change. Studies of small mammal communities could provide valuable insights to larger ecosystem changes.
two marmots perched atop a large boulder
Declining Sheep Populations in Alaska’s Arctic Parks
Dall’s sheep are an important subsistence species for local residents, particularly when caribou are scarce, and they are highly valued by sport hunters and wildlife enthusiasts. Their populations may be at an all-time low, however, in Noatak National Preserve and Gates of the Arctic National Park and Preserve due to weather conditions and other factors.
a woman kneeling in snow, collecting sheep shit
2013 Microgrant Recipients
The Murie Science and Learning Center (MSLC) funds numerous outreach projects through the Microgrant program. These grants help MSLC partner parks pay for science education outreach projects. Funding for the Microgrant program is provided by Alaska Geographic. Read about the 2013 Microgrant recipients and their outreach projects.
A Ranger stands with two junior rangers
2014 Microgrant Recipients
The Murie Science and Learning Center (MSLC) funds numerous outreach projects through the Microgrant program. These grants help MSLC partner parks pay for science education outreach projects. Funding for the Microgrant program is provided by Alaska Geographic. Read about the 2014 Microgrant recipients and their outreach projects.
Two students kneel in grassy field taking notes while looking at pink flagged marked locations
Wolverines
Wolverine. The name alone stirs up visions of northern wilderness. Wolverines belong to the mustelidae family along with weasels, mink, marten, and otters. The family mustelidae makes up most of the order Carnivora (carnivores).
a wolverine on a snow-covered river digging at something partially buried
2019 Science Education Grants
The Murie Science and Learning Center (MSLC) funds numerous outreach projects through the Science Education Grant program. These grants help MSLC partner parks pay for science education outreach projects. Funding for the Science Education grant program is provided by Alaska Geographic. Read about the 2019 Science Education Grant recipients and their outreach projects.
a park ranger and kids standing in shallow lake water
Snowshoe hare use of mineral licks
Read the abstract and link to the recently published article in Ecology on hare geophagy: Kielland, K., D. DiFolco, and C. Montgomerie. 2018. Dining dangerously: Geophagy by snowshoe hares. Ecology DOI:10.1002/ecy.2555
A hare eats mineral soil.
North for Science! Learns About Fire Ecology in Alaska
This summer's North for Science! Program included a lesson in wildland fire ecology in Alaska. The funding for the fire ecology portion was made possible by the National Park Service Fire Communication and Education Grant Program. Students were provided an incredible opportunity to learn about the role of wildland fire in boreal and arctic ecosystems.
A group of eight students sit atop the Arctic Interagency Visitor Center's welcome sign.
Caribou: Did You Know?
Did you know facts and life history about the Western Arctic Caribou Herd of northwest Alaska
Bull caribou in the Brooks Range mountains of Alaska
Fire in the Range of Western Arctic Caribou Herd
Wildland fire may have a significant impact on lichen-dependent caribou within the tundra ecosystem.
A caribou carrying heavy antlers walks slowly though green tundra on a hazy, grey day.
2018 Science Education Grants
The Murie Science and Learning Center (MSLC) funds numerous outreach projects through the Science Education Grant program. These grants help MSLC partner parks pay for science education outreach projects. Funding for the Science Education grant program is provided by Alaska Geographic. Read about the 2018 Science Education Grant recipients and their outreach projects.
an instructor and a camper work on a carving
The Fate of Permafrost
At present, permafrost is continuous in Arctic parks and discontinuous in Denali and Wrangell St.-Elias national parks and preserves. We expect the distribution of permafrost will still be continuous in Arctic parks by the 2050s; however, it is very likely that the distribution of permafrost in Denali and Wrangell-St. Elias will become sporadic by then.
a person standing next to an eroded hillside
Artists Spotlight Alaskan Wilderness
Voices of the Wilderness Traveling Art Exhibit is a collection of paintings, photographs, sculptures, poetry, and other works inspired by Alaska’s wilderness.
quilt of two white birch trees
Caribou: Nomads of the North
Caribou are an iconic Arctic species that are highly adaptable both physiologically and behaviorally. Yet, caribou populations face many challenges, such as climate change and industrial development, and are in decline in many portions of their range.
two bull caribou swimming through a river
2015 Microgrant Recipients
The Murie Science and Learning Center (MSLC) funds numerous outreach projects through the Microgrant program. These grants help MSLC partner parks pay for science education outreach projects. Funding for the Microgrant program is provided by Alaska Geographic. Read about the 2015 Microgrant recipients and their outreach projects.
Students kneel in a wetland and examine a net
Jillian Richie - Archaeologist
Jillian Richie is an archaeologist for Gates of the Arctic National Park and Preserve and Yukon-Charley Rivers National Preserve, Alaska.
Jillian in the field, preparing an archaeological field site.
Amy Larsen - Aquatic Ecologist/Pilot
Amy Larsen is an aquatic ecologist and pilot for Gates of the Arctic National Park and Preserve and Yukon-Charley Rivers National Preserve in Alaska.
Amy Larsen collecting field data on shallow lakes.
Caribou Migration Linked to Climate Cycles and Insect Pests
Read the abstract and get the link to an article published in Ecosphere on climate and insect drivers for caribou migration: : Gurarie, E., M. Hebblewhite, K. Joly, A. P. Kelly, J. Adamczewski, S. C. Davidson, T. Davison, A. Gunn, M. J. Suitor, W. F. Fagan, and N. Boelman. 2019. Tactical departures and strategic arrivals: Divergent effects of climate and weather on caribou spring migrations. Ecosphere 10(12):e02971. 10.1002/ecs2.2971
Caribou migrate across snow-covered tundra.
Larger Brown Bear Sows are More Successful in Rearing Cubs
Read the abstract and get the link to a new article looking at Alaska brown bear cub recruitment across four populations: Hilderbrand, G. V., D. D. Gustine, K. Joly, B. Mangipane, W. Leacock, M. D. Cameron, M. S. Sorum, L. S. Mangipane, and J. A. Erlenbach. 2019. Influence of maternal body size, condition, and age on recruitment of four brown bear populations. Ursus 29(2): 111-118.
A brown bear sow and four cubs.
Brown Bear Den Sites
Read the abstract and get the link to a new article on bear den site characteristics in the Brooks Range: Sorum, M. S., K. Joly, A. G. Wells, M. D. Cameron, G. V. Hilderbrand, and D. D. Gustine. 2019. Den-site characteristics and selection by brown bears (Ursus arctos) in the central Brooks Range of Alaska. Ecosphere 10(8): e02822. 10.1002/ecs2.2822
A close up of bear paws and claws.
Donna DiFolco - Biological Technician
Donna DiFolco is a biological technician for Gates of the Arctic National Park and Preserve and Yukon-Charley Rivers National Preserve, Alaska.
Donna releasing a hare during field work.
Caribou Resource Brief for the Arctic Network
The Western Arctic Caribou Herd is one of the most critical subsistence resources in northwest Alaska. Monitoring the herd helps develop subsistence and sport hunting regulations that conserve the resource, protect critical habitat, and reduce conflicts among user groups. Since 2009, over 300 GPS collars have been deployed on caribou that have collected over 800,000 caribou locations.
Caribou swim across the Kobuk River at Onion Portage in Kobuk Valley National Park
Collared Pika
Collared pikas are small mammals within the same order as rabbits and hares, and they resemble small rabbits with very short ears and small limbs. Adapted to thrive at high elevations in Alaska, their habitat is at risk -- climate change may drastically change the fragile environment in which they live.
tiny gray rabbit-like creature sitting on a rock
Arctic Ground Squirrel
The largest of the North American ground squirrels, arctic ground squirrels are burrowing rodents that resemble prairie dogs, with small ears, a flat tail, and a white-spotted back. They are very common throughout much of Denali and live mainly in the alpine tundra.
two ground squirrels
Dall Sheep
Dall sheep are unmistakable, looking like pure-white bighorn sheep. Like bighorn sheep, they have large, curled horns, but Dall sheep horns are longer and skinnier than their southern counterparts. They inhabit mountain ranges in Alaska and Canada and are often visible from quite far away.
Close up of sheep face and horns
The Surprising Diets of Brooks Range Brown Bears
Read the abstract and get the link to a paper on brown bear diets in the interior Arctic of the Brooks Range: Mangipane, L. S., D. J. R. Lafferty, K. Joly, M. S. Sorum, M. D. Cameron, J. L. Belant, G. V. Hilderbrand, and D. D. Gustine. 2020. Dietary plasticity and the importance of salmon to brown bear (Ursus arctos) body size and condition in a low Arctic ecosystem. Polar Biology.
A bear fishes a small stream.
Salmon Sleuths: GPS-collared Bears Lead Researchers to Unknown Salmon Streams in Interior Alaska
Movement data from GPS-collared bears provides valuable information to improve conservation efforts not only for bears, but also for salmon. This study describes the discovery of an unexpected relationship between bears and salmon in the Arctic Interior and the out-sized role salmon have on diet and movement patterns of grizzly bears living in a nutrient-limited system. Alaska Park Science 19(1):2020
A bear sow and 2 cubs fishing in an Arctic stream.
Fish Inventories of the Upper Kobuk and Koyukuk River Basins
Fish inventories in the Brooks Range added hundreds of new miles to the Anadromous Waters Catalog, improving overall knowledge of fish species assemblage, distribution, and abundance in the region. This information will help guide management actions on the proposed Ambler Road and future studies of aquatic resources. Alaska Park Science 19(1):2020
A helicopter landed on a small stream bank.
Fall 2019 Weather Summary for Arctic Parks
What was the weather like in Arctic Parks in 2019? Check out this weather summary for Fall 2019 for Bering Land Bridge NP, Gates of the Arctic NPP, and Western Arctic Parklands.
Climate scientists repair climate station. Mountains in the backdrop.
Hoary Marmot
Hoary marmots are large rodents that live mainly in alpine areas. Their loud, clear warning calls are a common sound in mountainous regions.
closeup of a marmot baby
Magnetic Detection of Archaeological Hearths in Alaska
Read the abstract and link to a recent article on archaeological research using magnetic detection of hearths: Urban, Thomas M., Jeffrey T. Rasic, Claire Alix, Douglas D. Anderson, Linda Chisholm, Robert W. Jacob, Sturt W. Manning, Owen K.Mason, Andrew H. Tremayne, Dale Vinson (2019). Magnetic detection of archaeological hearths in Alaska: A tool for investigating the full span of human presence at the gateway to North America. Quaternary Science Reviews 211: 73-92.
An archaeologist searches for hearths using a magetometer
Arctic Perennial Snowfields are Shrinking
Read the abstract and get the link to an article on changes in perennial snowfields in the Brooks Range. Tedesche, M. E., E. D. Trochim, S. R. Fassnacht, and G. J. Wolken. 2019. Extent Changes in the Perennial Snowfields of Gates of the Arctic National Park and Preserve, Alaska. Hydrology 6, 53.
A researcher records measurements on a snowfield high in the Brooks Range.
Moose: Did You Know?
Did You Know factoids about moose in Interior Alaska National Parks
Bull moose bedded in vegetation
Refining the Analysis of Hair Samples
Read the abstract and get the link to a published paper on how bear hair is used to determine diet and how the method of using hair to determine diet is refined to detect seasonal variation. Rogers, M. C., G. V. Hilderbrand, D. D. Gustine, K. Joly, W. B. Lealock, B. A. Mangipane, and J. M. Welker. 2020. Splitting hairs: Dietary niche breadth modelling using stable isotope analysis of a sequentially grown tissue. Isotopes in Environmental and Health Studies.
A close look at bear fur.
Predicting Seasonal Distributions and Migratory Routes of Western Arctic Herd Caribou
Read the abstract and get the link for an article on caribou migration patterns published in Movement Ecology: Baltensperger, A. P., and K. Joly. 2019. Using seasonal landscape models to predict space use and migratory patterns of an arctic ungulate. Movement Ecology 7 (18). DOI: 10.1186/s40462-019-0162-8.
The western arctic caribou herd along the Kobuk River.
Weather Impacts on Dall's Sheep
Read the abstract and link to a recent paper in Ecosphere on Dall's sheep population impacts from weather events: Rattenbury, K. L., J. H. Schmidt, D. K. Swanson, B. L. Borg, B. A. Mangipane, and P. J. Sousanes. 2018. Delayed spring onset drives declines in abundance and recruitment in a mountain ungulate. Ecosphere 9(11):e02513. 10.1002/ecs2.2513
Dalls sheep lambs and ewes on a rock cliff.
Permafrost Landforms as Indicators of Climate Change in Parks Across the Arctic
Permafrost, ground so cold that it stays frozen for multiple years, develops certain landforms when it thaws, and thereby provides a way for scientists to recognize and monitor our changing climate.
treeless hillside partially collapsed into a river at its base
Research Fellowship Recipients (2015)
Learn about 2015 Research Fellowship recipients
a man sitting in a forest
Research Fellowship Recipients: 2008
Learn about 2008 fellowship recipients
Research Fellowship Recipients: 2009
Learn about 2009 research fellowship recipients
The Social Structure of Dall Sheep
Dall sheep employ a sophisticated social structure.
A ewe and two lambs stand on a rocky cliff
Monitoring Dall Sheep
Discovery how and why scientists monitor Dall sheep in national parks throughout Alaska.
A group of three dall sheep walk down a dirt road
Dall Sheep and Climate Change
How might climate change impact the world's northernmost wild sheep population?
ewe and lamb on a rocky outcropping
Birds of the Arctic
Simon Paneak, a Nunamiut hunter, spent most of his adult life living in Anaktuvuk Pass in the Brooks Range. Simon was a fountain of traditional ecological knowledge, as were other adults within his community. However, Simon spoke, read, and wrote English, which facilitated his long collegial relationships with a variety of researchers interested in Arctic cultural and biological ecosystems.
landscape of spruce forests and mountains
Landbirds Resource Brief for the Arctic Network
Approximately 147 resident and migratory bird species are expected to occur in the five National Parks of the Arctic Network. Among the songbirds breeding above treeline, White-crowned Sparrow, American Tree Sparrow, Savannah Sparrow, and Wilson’s Warbler are ubiquitous and abundant. This resource brief summarizes long-term monitoring of landbirds in the Arctic Network.
A Bluethroat perched in a willow in the golden light of the Arctic.
What Future for the Wildness of Wilderness in the Anthropocene?
Visionary as it was, the Wilderness Act did not anticipate today’s human-driven, global-scale changes. The idea of preserving wild lands challenges us with the irony that such places, untouched by humans, will only continue through our will to keep them that way. A resolute human purpose is needed to maintain the decision to have areas that are free of human purpose.
aerial view of wolves moving single-file through a snowy forest
Using Ethics Arguments to Preserve Naturalness: A Case Study of Wildlife Harvest Practices on NPS Lands in Alaska
The NPS responsibility to maintain natural wildlife populations is inherently challenging. For example, many animals migrate out of parks either seasonally or long-term. Typically, we collect and analyze data, and then publish our work. However, the answer rarely, if ever, lies solely in the data. Often the question is not even one of biology, but one of values. In these cases, nonscientific tools such as rigorous and transparent argument analyses are appropriate.
bear eating a fish in shallow water
The Economic and Cultural Benefits of Northwest Alaska Wilderness
Northwest Alaska, from Kotzebue Sound to the headwaters of the Kobuk River, is approximately the size of Indiana. It is mostly roadless wild lands, dotted by eleven villages that are located on the coast or major rivers. The formal designation of wilderness areas in northwest Alaska contributes to sustaining an ecosystem that is predicated on an expansive area of natural habitat that is not fragmented by human development.
four caribou swimming in neck-deep water
Research Fellowship Recipients: 2012
Learn about 2012 Research Fellowship recipients
woman in a red shirt and white hat
Research Fellowship Recipients | 2014
Learn about 2014 Research Fellowship recipients.
woman kneeling in water
Monitoring Dall Sheep in Alaska's Arctic Parklands
In an area the size of New Jersey, scientists study Dall's sheep. They are one of 28 vital signs monitored by the Arctic Network Inventory and Monitoring Program (ARCN I&M) because of their importance to the public and in assessing the overall health of the regional ecosystem.
group of white colored sheep on a mountainside
Alaska brown bears exposure to bacterial, viral, and parasitic pathogens
Read the abstract and get the link to a new article on pathogens found in Alaska brown bears published in the Journal of Wildlife Disease: Ramey, A. M., C. A. Cleveland, G. V. Hilderbrand, K. Joly, D. D. Gustine, B. Mangipane, W. B. Leacock, A. P. Crupi, D. E. Hill, J. P. Dubey, and M. J. Yabsley. In press. Exposure of Alaska brown bears (Ursus arctos) to bacterial, viral, and parasitic agents varies spatiotemporally and may be influenced by age.
A bear perched on a rock outcrop
National Park Getaway: Gates of the Arctic National Park & Preserve
North of the Arctic Circle lies a wild land barely changed from time immemorial, a park whose name invites adventure and exploration—Gates of the Arctic National Park and Preserve. Even amidst the grand landscapes of Alaska, the 8-million acre Gates of the Arctic remains a treasured destination for wilderness exploration.
Is the Arctic too hot for moose?
Read the abstract and get the link to a science article on how moose in the Arctic are impacted by climate change: Jennewein, J. S., M. Hebblewhite, P. Mahoney, S. Gilbert, A. J. H. Meddens, N. T. Boelman, K. Joly, K. Jones, K. A. Kellie, S. Brainerd, L. A. Vierling, and J. U. H. Eitel. 2020. Behavioral modifications by a large, northern herbivore to mitigate warming conditions. Movement Ecology 8(39).
A moose gets some shade under spruce trees.
Alaska Aviation Safety
In Alaska, small planes are often the best way to get around but flying has its risks. Aviation safety requires more than just a pilot’s skill–it takes all of us. Learn more about aviation to increase the safety of your next park flight.
An NPS pilot in a plane cockpit flying over a turquoise lake
Matthew Cameron - Wildlife Biologist
Matthew Cameron is a wildlife biologist at Gates of the Arctic National Park and Preserve and Yukon-Charley Rivers National Preserve.
Matt Cameron portrait.
Perennial Snowfields of the Central Brooks Range: Valuable Park Resources
The nature of change in perennial snowfields in the central Brooks Range is one of rapid decline, and these changes are of increased significance to the high alpine hydrology and ecology of Gates of the Arctic. Results of research will help archaeologists continue to target field survey areas, as well as address the impacts that these changes are having on park natural resources.
a large patch of snow near the top of a rocky mountain
Lichens of the Arctic
Because certain lichen species are both abundant and sensitive to changes in the environment, they can serve as useful indicators of ecosystem health. When exposed to even low levels of certain pollutants, particularly sensitive species will decline or die, making lichen community composition a good indicator.
closeup of green colored lichen
Adam Freeburg - Archaeologist
Adam Freeburg is an archaeologist for Gates of the Arctic National Park and Preserve and Yukon-Charley Rivers National Preserve.
An archaeologist hikes a ridgeline to a survey site in the Yukon-Tanana uplands.
Kyle Joly - Wildlife Biologist
Kyle Joly is a wildlife biologist in Alaska. He works with the Arctic Inventory and Monitoring Network, Gates of the Arctic National Park and Preserve, and Yukon-Charley Rivers National Preserve.
Wildlife biologist Kyle Joly with a young caribou.
Mathew Sorum - Wildlife Biologist
Mathew Sorum is a wildlife biologist for Gates of the Arctic National Park and Preserve and Yukon-Charley Rivers National Preserve.
Mat rows a raft across an Arctic lake.
The 19th Amendment, Elizabeth Peratrovich, and the Ongoing Fight for Equal Rights
In Alaska, women's suffrage passed in 1913—seven years prior to the 19th Amendment—and antidiscrimination legislation passed nearly 20 years prior to the major national civil rights bills of the 1960s. In the 1940s, Elizabeth Peratrovich—a Tlingit woman who was Grand President of the Alaska Native Sisterhood—led the charge to end discrimination against Alaska Natives.
gold coin of a raven, a woman's face, and words elizabeth peratrovich anti-discrimination law
Series: Alaska Park Science - Volume 16 Issue: Science in Alaska's Arctic Parks
The National Park Service manages five parks that fall partially or entirely within the Arctic tundra biome. These five parks encompass 19.3 million acres of land and constitute approximately 25% of the land area managed by the National Park Service nationwide. These are undeveloped places, with free-flowing rivers and wilderness at a massive scale.
a group of muskox running across a field
Series: Dall Sheep in Alaska's National Parks
Discover the importance of Dall Sheep in Alaska's National Parks
Two sheep rest on a snowy mountain
Series: Alaska Park Science - Volume 12 Issue 2: Climate Change in Alaska's National Parks
In this issue: * Status and Trends of Alaska National Park Glaciers * Tracking Glacial Landscapes: High School Science Gets Real * Climate Change Scenario Planning Lessons from Alaska
a hillside overlooking a wide valley filled by a glacier, surrounded by steep mountains
Series: Alaska Park Science - Volume 13 Issue 2: Mineral and Energy Development
There’s no denying that energy and mineral extraction have been and will continue to be important across the North for a long time. Mining and energy-related industries provide direct and indirect employment for thousands of people, taxes and other revenues. Our need is for science, engineering, and scholarly research; to develop safe, effective, and affordable technologies; to protect, preserve, and restore the natural and human environment; and to record and communicate our history.
aerial view of buildings and a pier sticking out into the ocean
Series: Alaska Park Science - Volume 13 Issue 1: Wilderness in Alaska
This issue includes: * Economics of Wilderness * Using Ethics Arguments to Preserve Naturalness * Busing Through the Wilderness: "Near-Wilderness" Experiences in Denali ... and more!
mountains reflecting into a calm lake, the words 'alaska park science'
Series: The Legacy of ANILCA
The Alaska National Interest Lands Conservation Act impacts the National Park Service in many ways. ANILCA stipulates the designation of wilderness, subsistence management, transportation in and across parklands, use of cabins, mining, archaeological sites, scientific research studies and more.
Two men drag a harvest seal from icy blue waters across frozen ice.
Series: Geologic Time Periods in the Paleozoic Era
During the Paleozoic Era (541 to 252 million years ago), fish diversified and marine organisms were very abundant. In North America, the Paleozoic is characterized by multiple advances and retreats of shallow seas and repeated continental collisions that formed the Appalachian Mountains. Common Paleozoic fossils include trilobites and cephalopods such as squid, as well as insects and ferns. The greatest mass extinction in Earth's history ended this era.
fossil corals in a rock matrix
Series: Copper River Basin Symposium - Wrangell-St Elias National Park and Preserve
February 2020: With a theme of Tradition, Science, and Stewardship, the two-day symposium included keynote speakers, 26 short presentations, and a poster session. A panel discussion delved into opportunities in working with indigenous communities. Ahtna elders provided wisdom in daily welcomes, and there was a presentation by Copper River Stewardship Youth. Topics ranged widely from fisheries to archaeology to geology. As well as sharing knowledge, participants shared meals, stories, and ideas.
Copper River Basin Symposium logo by Lindsay and Elvie
Series: Alaska Park Science - Volume 19, Issue 1 - Below the Surface: Fish and Our Changing Underwater World
Alaska has over three million lakes, 12,000 rivers, and an estimated 6,640 miles of ocean coastline. Below the surface swim some of the world’s most abundant, healthy, all-wild fish, including salmon, halibut, and eulachon. Fish sustained Alaska Natives for millennia and continue to represent food and economic security for many people. Alaska Park Science 19(1): 2020
Red-colored salmon swim in turquoise water.
Series: Alaska Park Science - Volume 14 Issue 2: Birds of Alaska's National Parks
This issue includes articles exploring birds throughout national parks in Alaska. Particular emphasis is on the changing ways to study birds, and the increasing importance not just on the summer homes of birds in Alaska, but the routes between their wintering and summer breeding grounds.
a great horned own and two large owlets in a nest
Series: Alaska Park Science - Volume 9 Issue 1: Monitoring the "Vital Signs" of Healthy Park Ecosystems
This issue explores the "vital signs" of parks. The National Park Service's Inventory and Monitoring (I&M) Network studies broad ecological trends throughout parks, and uses those trends, or vital signs, to gauge the health of a park's ecosystem.
man standing in a shallow creek
Series: Alaska Park Science- Volume 8 Issue 1: Connections to Natural and Cultural Resource Studies in Alaska's National Parks
This issue of Alaska Park Science explores natural and cultural studies in Alaska's National Parks. Theses studies cover a variety of topics including wildlife management, archaeology, permafrost, sustainable energy, and interviews with two researchers from the Cooperative Park Studies Unit.
Aurora over Klondike Gold Rush National Historical Park and Skagway, Alaska.
Brown bear population size and harvest in Northwest Alaska
Read a summary and get the link to a paper published in the Journal of Wildlife Management on brown bear population trends in northwest Alaska: Schmidt, J. H., H. L. Robison, L. S. Parrett, T. S. Gorn, and B. S. Shults. 2021. Brown bear density and estimated harvest rates in northwestern Alaska. The Journal of Wildlife Management 85(2): 202-214.
Aerial view of brown bears crossing a snow field in the Brooks Range.
Mississippian Period—358.9 to 323.2 MYA
The extensive caves of Mammoth Cave and Wind Cave national parks developed in limestone deposited during the Mississippian. Warm, shallow seas covered much of North America, which was close to the equator.
fossil crinoid
Devonian Period—419.2 to 358.9 MYA
The Devonian is part of the “Age of Fishes.” Fish fossils from Death Valley National Park shed light on the early evolution of fish in North America. Tilted Devonian rocks in Chesapeake & Ohio Canal National Historical Park attest to continued Appalachian Mountain formation.
fossil brachiopod
Paleozoic Era
During the Paleozoic Era (541 to 252 million years ago), fish diversified and marine organisms were very abundant. In North America, the Paleozoic is characterized by multiple advances and retreats of shallow seas and repeated continental collisions that formed the Appalachian Mountains. Common Paleozoic fossils include trilobites and cephalopods such as squid, as well as insects and ferns. The greatest mass extinction in Earth's history ended this era.
fossil corals in a rock matrix
Fire Extent and Frequency Resource Brief for the Arctic Network
Fire affects all 5 parks within the Arctic Network. The first fires in the network were officially recorded in 1956, although the history of fire in these parks, based on charcoal records dates back to at least 6,000 years ago. Since 1956, 574 fires have occurred in Arctic Network parks, burning nearly 1.1 million acres, an area almost twice the size of Cape Krusenstern National Monument. The vast majority of these fires (97%) were started by lightning.
Fire ecologist measures depth of soil consumption in tussocks 1 year after a recent fire in Noatak.
Fire in Ecosystems: Boreal Forest
The boreal forest, also called taiga, is the largest forested habitat in the world, making up one third of the earth’s total forested area. In North America, the boreal forest spreads from Alaska, across Canada, and into the Great Lakes region of the United States. Boreal forests have burned naturally for thousands of years creating a variety of landscapes, or mosaic, with young and old trees living on the landscape.
Aerial view of flaming front in coniferous trees putting off a lot of smoke.
Repeat Photography: A Visually Compelling Tool for Documenting Natural Resource Change
Repeat photography is an effective method to qualitatively and quantitatively assess landscape change over time. From shrinking glaciers to changing vegetation to changes in the built environment, comparing historical and contemporary photos can help us identify specific features or processes that may require more intensive monitoring and research and can serve as a valuable tool for education, outreach, and resource management. Alaska Park Science 20(1), 2021
A historic photo overlaid on a modern image.
Series: Alaska Park Science Volume 20 Issue 1 - Parks as Proving Grounds
Parks in Alaska pose special challenges to researchers: they are large, remote, and less is known about them. This makes it all the more important that tools and techniques we use here are practical, effective, and impactful. While researchers often focus on sharing the findings from their work, here we shine a light on the devices and approaches used by researchers with attention to the innovation needed to work in Alaska. Alaska Park Science 20 (1), 2021
A scientist uses a probe on the top of a mountain.
Dall's Sheep Resource Brief for the Arctic Network
Dall’s sheep are an alpine adapted species at their northernmost extent in the Brooks Range of Alaska. GAAR and NOAT encompass most of the available habitat in the central and western Brooks Range and were estimated in the 1980’s to contain 13-15% of the world’s Dall’s sheep. Dall’s sheep are an important subsistence species for local residents and highly valued where sport hunting is permitted in preserves.
A Dall's sheep ram close up image
Brown Bear Resource Brief for the Arctic Network
Alaska has more than 50% of the remaining North American brown bears and the second largest population worldwide. Parks in the Arctic Inventory and Monitoring Network may ultimately provide a refuge for brown bears in northwest Alaska that are adapted to life in the Arctic, but strong monitoring programs are needed to understand whether these bear populations can remain healthy in a rapidly changing Arctic.
A brown bear sits in a tundra wetland.
Bumble Bees of Alaska: A Field Guide
This field guide to bumble bees will help you identify these abundant and conspicuous pollinators, which are found across most of Alaska. They are well-adapted to cold, harsh climates and live in every habitat where there are flowers offering up pollen and nectar, including forests, shrublands, tundra, wetlands, riparian areas, beaches, and gardens.
a bumble bee perched on tiny pink flowers
The Long Walk: The Origins of Anaktuvuk Pass
The time is early summer 1949, at Sulupaat, a camp near the mouth of April Creek in the Killik River valley. There, the families of Maptigaq Morry, Inualuuraq Hugo, Homer Mekiana, and their children and grandchildren are prepared to set out on The Long Walk. It would be more than a two week long overland dog-packing trek, as the Killik families made their way eastward to join another small group of families at Tulugaq Lake, nearly a hundred miles distant.
Justus Mekiana walking with a group of dogs wearing dog-packs
Nunamiut Caribou Skin Clothing and Tents
Inland mountain Eskimos experience one of the world’s most extreme winter climates—temperatures of 55 degrees below zero or colder, often with gale force winds and blinding snow. Despite these daunting conditions, Eskimo people carry on with their daily life of hunting, fishing, gathering firewood, traveling, and camping. The key to their success and survival—above all else—is warm, effective, brilliantly designed and expertly made clothing.
Nunamiut ice fisherman wearing caribou skin parka, pants, and boots
Nunamiut: The Caribou People
In Northern Alaska, people and caribou have lived in a close, intricate relationship for at least 11,000 years. Caribou have been vitally important for the survival of all native people whose homelands are now partially encompassed by Gates of the Arctic National Park and Preserve. For some tribes, caribou is just part of a diet which also includes other game, fish and marine mammals. But for the Nunamiut Eskimos, caribou is by far the single most important food source.
1967 Simon Paneak drawing of a hunter in a qayaq spearing caribou as they cross a river
What a mammoth's tusk can tell us about its life
Where did woolly mammoths roam when they lived in Beringia? What can learning about their movements tell us about their lives and their extinction? Read more here: Wooller, M. J., C. Bataille, P. Druckenmiller, G. M. Erickson, P. Groves, N. Haubenstock, T. Howe, J. Irrgeher, D. Mann, K. Moon, B. A. Potter, T. Prohaska, J. Rasic, J. Reuther, B. Shapiro, K. J. Spaleta, and A. D. Willis. 2021. Lifetime mobility of an Arctic woolly mammoth. Science 373(6556): 806-808.
Two woolly mammoths walk across Beringia.
Stream Communities & Ecosystems Resource Brief for the Arctic Network
Stream flow has changed in recent decades at monitoring sites near the Arctic Network. The timing of peak discharge during spring snowmelt now occurs nearly 10 days earlier than it did 30 years ago. The Kobuk River is now re-freezing later in fall than it did in the 1980s. In headwater streams of the Arctic Network, permafrost thaw is changing watershed hydrology, causing streams to cool and discharge to decline during summer months.
Aerial image of a Braided river in Alaska’s Arctic Network with mountains in background
How do caribou decide when to migrate in the fall?
Read a summary and link to a published paper that describes the factors that determine caribou fall migration. Cameron, M. D., J. M. Eisaguirre, G. A. Breed, K. Joly, and K. Kielland. 2021. Mechanistic movement models identify continuously updated autumn migration cues in Arctic caribou. Movement Ecology 9(54): 12 pp.
Caribou running through tundra in the fall.
A Wilderness Treasure Hunt Unlocks Caribou Secrets
Two rangers retrieve a GPS collar from an animal in the backcountry, helping biologists learn about the animal’s movements.
Backcountry ranger Taylor Bracher holds up GPS collar
Arctic Summers are Getting Longer
Read a summary and get the link to an article that describes how the Arctic is getting greener: Swanson, D. K. 2021. Start of the green season and normalized difference vegetation index in Alaska's Arctic national parks. Remote Sensing 13(13): 2554.
A muskox naps in the tundra.
Terrestrial Landscape Dynamics Resource Brief for the Arctic Network
Landscape dynamics are the “big picture” of changes in the growing season, vegetation, and surface water. The timing of the start and end of the growing season and snow-free season varies by about a month from year-to-year. The area of lakes and ponds has declined in the northern coastal plain of Bering Land Bridge NP, from about 8.5% of the land surface area in 2000 to less less than 7% by 2019. Tall shrubs are expanding their range and getting denser in some areas.
Muskox lying on tundra with a mountain in the background under overcast sky
Terrestrial Vegetation and Soils Resource Brief for the Arctic Network
Vegetation is the basis for ecosystem productivity and wildlife habitat. Arctic vegetation is very sensitive to climate change and disturbance such as fire, herbivory, and traffic. Research has documented an increase in shrubs and, to a lesser extent, trees in the arctic over recent decades, probably related to climate change. Major changes in vegetation structure such as these have a cascading effect on other ecosystem attributes.
scientists measure the cover of plants on the tundra along a tape measure
What we can learn from a bear's stomach
Read the abstract and get the link to an article that looks at the diversity of bear gut microbiomes and how they differ across Alaska. Trujillo, S. M., E. A. McKenney, G. V. Hilderbrand, L. S. Mangipane, M. C. Rogers, K. Joly, D. D. Gustine, J. A. Erlenbach, B. A. Mangipane, and D. J. R. Lafferty. 2022. Intrinsic and extrinsic factors influence on an omnivore's gut microbiome. PLOS ONE 17(4): e0266698.
A bear eating sedges.
Plan Like a Park Ranger - 10 Tips for Visiting Alaska's National Parks
Planning a visit to the National Parks of Alaska? Check out our top 10 tips and plan like a park ranger.
two people camp next to a glacier
Series: Commemorating ANILCA at 40
Forty years after ANILCA was passed, the Alaska Region of the National Park Service is reflecting on the impact, legacy, and future of this unique legislation. Many Alaskans experience ANILCA as both a blessing and a burden. While tremendous hurdles have been overcome, there are many yet to be faced. This issue of Alaska Park Science provides a range of perspectives on ANILCA that we hope strikes a balance and reflects over four decades of varied experiences.
The Charley River.
The Harvest and Use of Wild Resources by Communities Within or Near Northern Alaska Parklands
Customary and traditional harvests of wild resources provide for the nutritional, economic, spiritual, and cultural well-being of communities throughout Alaska. The National Park Service has the authority and responsibility to manage these uses on parklands. Comprehensive surveys reveal harvest and use patterns, providing information to maintain these critical resources and manage for the continuation of subsistence required under ANILCA. Alaska Park Science 21(1), 2022
A pile of frozen northern pike from ice fishing.
How much space does a brown bear in the Brooks Range use?
Read the abstract and get a link to a published article on brown bear home ranges in the Brooks Range of Alaska: Joly, K., M. D. Cameron, M. S. Sorum, D. D. Gustine, W. Deacy, and G. V. Hilderbrand. 2022. Factors influencing Arctic brown bear annual home range sizes and limitations of home range analyses. Ursus (33e11): 1-12.
A bear fishing and one on the bank.
Weather and Climate Resource Brief for the Arctic Network
Climate is the most important broad-scale factor influencing ecosystems. Temperatures across Alaska are rising much faster than at lower latitudes. Trends in Arctic Alaska’s average annual air temperatures from 1950 to 2021, our longest consistent record, show a significant temperature increase of >2.6°C in the communities in and around Alaska’s Arctic national parks.
A helicopter standbys while two people work on a climate station station.
Gates of The Arctic National Park and Preserve/Bettles Weather Summary Fall 2021, Winter 2021-2022, and Spring 2022
The weather station in Bettles, AK has been recording temperature and precipitation data for over seventy years. December brought extreme precipitation and rain-on-snow along the West Coast of Alaska and into Interior Alaska. Heavy snowfall, freezing rain, and rain brought record amounts of precipitation to many communities. It was the wettest December on record! 3.61 inches of precipitation was recorded in December (melted snow, sleet, rain), which is 345% of normal.
Two people work on maintaining a climate station against the backdrop of a wide tundra valley.
Wilderness Character Mapping
The condition of wilderness character varies across a wilderness based on the intensity and distribution of human influences that degrade it. Just as variation in other landscape features can be depicted spatially, so too can the condition of wilderness character. Wilderness character mapping was used to model potentially impacting future scenarios. Specifically, maps include potential impacts of two proposed industrial road routes through the preserve.
A view of the Kobuk River.
What's the Difference: Reindeer vs. Caribou
Caribou and reindeer are the same species and share the same scientific name, Rangifer tarandus. Caribou are what the species is called in North America and reindeer are what they are called in Eurasia.
Graphic illustration of a caribou and reindeer,
Pile burning protects remote structure in Gates of the Arctic National Park and Preserve
More than half of NPS structures in Alaska are farther than one mile from a road. But these structures are crucial to those who visit remote parts of the state to recreate, subsistence hunt and fish, and work. Often, they provide the only shelter for miles. Difficulty accessing these structures makes them extra vulnerable in the event of wildfire and makes it important to conduct fuels treatments prior to any threats.
A cabin blanketed in snow with evergreen trees and mountains in the background.
Taking the Pulse of U.S. National Parks
How do we know if parks are healthy? We measure their vital signs, of course! Across the country, there are 32 inventory and monitoring networks that measure the status and trends of all kinds of park resources. We're learning a lot after years of collecting data. Check out these articles written for kids and reviewed by kids in partnership with the international online journal Frontiers for Young Minds.
A cartoon of a ranger taking the pulse of the Earth.
Series: Geologic Time—Major Divisions and NPS Fossils
The National Park System contains a magnificent record of geologic time because rocks from each period of the geologic time scale are preserved in park landscapes. The geologic time scale is divided into four large periods of time—the Cenozoic Era, Mesozoic Era, Paleozoic Era, and The Precambrian.
photo of desert landscape with a petrified wood log on the surface
When are newly collared caribou representative of the herd?
Read the abstract and get the link to a paper published in the Wildlife Bulletin about representativeness among collared animals in a population: Prichard, A. K., K. Joly, L. S. Parrett, M. D. Cameron, D. A. Hansen, and B. T. Person. 2022. Achieving a representative sample of marked animals: A spatial approach to evaluating post-capture randomization. Wildlife Society Bulletin e1398.
A collared caribou bounds away.
Landslide Risks Along Park Roads Increase in a Warming Climate
Read the abstract and get the link to an article on how climate change is impacting park roads in Alaska: Lader, R., P. Sousanes, U. S. Bhatt, J. E. Walsh, and P. A. Bieniek. 2023. Climate indicators of landslide risks on Alaska national park road corridors. Atmosphere 14(1): 34.
A grade displacement on park road.
A surprising number of bears congregate at Arctic salmon streams
Read a summary and get the link to a peer-reviewed journal article that quantifies the number of bears using an Arctic salmon stream. Surprisingly, it is as densely fished as coastal streams with moderate fish runs. Sorum, M. S., M. D. Cameron, A. Crupi, G. K. Sage, S. L. Talbot, G. V. Hilderbrand, and K. Joly. 2023. Pronounced brown bear aggregation along anadromous streams in interior Alaska. Wildlife Biology e01057.
A bear hair snare.
Parasites in Alaska Brown Bears
Read a summary and link to a journal article on the parasites found in Alaska brown bears: Haynes, E., S. Coker, M. J. Yabsley, K. D. Niedrighaus, A. M. Ramey, G. G. Verocai, G. V. Hilderbrand, K. Joly, D. D. Gustine, B. Mangipane, W. B. Leacock, A. P. Crupi, and C. A. Cleveland. 2023. Survey for selected parasites in Alaska brown bears (Ursus arctos). Journal of Wildlife Diseases 59 (1): 186-191. DOI: 10.7589/JWD-D-22-00070.
An Alaskan brown bear.
Arctic and Subarctic Bears' Exposure to Toxins
Read a summary of findings and get the link to an article looking at contaminants in brown bears: Fuchs, B., K. Joly, G. V. Hilderbrand, A. L. Evans, I. Rodushkin, L. S. Mangipane, B. A. Mangipane, D. D. Gustine, A. Zedrosser, L. Brown, and J. M. Arnemo. 2023.Toxic elements in arctic and sub-arctic brown bears: Blood concentrations of As, Cd, Hg and Pb in relation to diet, age, and human footprint. Environmental Research 229: 115952.
A bear eating salmon in the river
Seasonal Changes Across Alaska Parks
Featured here are a series of videos made from a year-long series of images from remote cameras (phenocams) at climate stations in Alaska national parks. We use this information to compare seasonal events such as when snow persists on the ground, when snow is completely melted, the timing of vegetation green-up and senescence, and more.
A scientist at a climate monitoring station
Some bears ride the green wave
Read the abstract and get the link to an article that looks at whether or not brown bears (grizzly bears) follow the "green wave" of green up: Bowersock, N. R., L. M. Ciarniello, W. W. Deacy, D. C. Heard, K. Joly, C. T. Lamb, W. B. Leacock, B. N. McLellan, G. Mowat, M. S. Sorum, F. T. van Manen, and J. A. Merkle. 2023. A test of the green wave hypothesis in omnivorous brown bears across North America. Ecography :e06549.
Two Alaska brown bears in the grass.
Shaping the System Under President Jimmy Carter
President Jimmy Carter oversaw one of the largest growths in the National Park System. Explore some of the parks that are part of the legacy of the presidency of Jimmy Carter, who served as the 39th president of the United States from January 20, 1977, to January 20, 1981.
Historic photo of Jimmy Carter walking through a crowd at Harpers Ferry
Alaska's Shrinking Glaciers
Alaska is one of the most heavily glaciated areas in the world outside of the polar regions. Approximately 23,000 square miles of the state are covered in glaciers—an area nearly the size of West Virginia. Glaciers have shaped much of Alaska’s landscape and continue to influence its lands, waters, and ecosystems. Because of their importance, National Park Service scientists measure glacier change. They found that glaciers are shrinking in area and volume across the state.
A close up of the surface of a glacier with ice and rocky morraine.
Nutuvukti Lake and Fen
Nutuvukti Lake is a unique and interesting place in Gates of the Arctic National Park and Preserve. The lake lies in a trough between two mountain ridges covered with dwarf subarctic spruce forest and alpine tundra. Six miles long, Nutuvukti Lake is smaller than its more famous neighbor, Walker Lake, but is still one of the largest lakes in northern Alaska and home to lake trout, arctic grayling, arctic char, northern pike, and whitefish.
A large lake with a mountain and reflection.
Rusting of Wild and Scenic Rivers in Alaska Arctic National Parks
Over the past few years, scientists have observed a new phenomenon related to thawing soils: streams which have turned a vibrant orange color across Alaska’s Arctic. Of particular concern is the recent discoloration of the Salmon Wild & Scenic River in Kobuk Valley National Park.
a river with orange rusty water
Permafrost Thaw Slumps in the Noatak Valley
Retrogressive thaw slumps, small landslides caused by thaw and subsidence of permafrost, are dramatic features on the Arctic landscape. They can impact water quality in streams and lakes. Resource brief, 2023
An enhanced aerial map of thaw slumps over time.
Fire in Ecosystems: Arctic Tundra
Fires in the tundra happen less often than in the boreal forest. Fires can be sporadic and widely distributed. The years between fire events, called fire return intervals, vary widely from 30 years to over 1,000 years in the tundra.
White flowers dot an open plain that give way in the distance to gray mountains.
Updated Species Database Will Help Boost Amphibian Conservation Across the National Park Service
To steward amphibians effectively, managers need basic information about which species live in parks. But species lists need constant maintenance to remain accurate. Due to recent efforts, the National Park Service now has an up-to-date amphibian species checklist for almost 300 parks. This information can serve as the basis for innumerable conservation efforts across the nation.
A toad sits on red sand, looking into the camera.
Metals released from thawing permafrost are rusting Arctic streams
Read the abstract and get the link to a published paper on how permafrost thaw is releasing metals into streams and turning them orange: O'Donnell, J. A., M. P. Carey, J. C. Koch, C. Baughman, K. Hill, C. E. Zimmerman, P. F. Sullivan, R. Dial, T. Lyons, D. J. Cooper, and B. A. Poulin. 2024. Metal mobilization from thawing permafrost to aquatic ecosystems is driving rusting of Arctic streams. Communications Earth & Environment 5: 268.
An orange stream joins a blue-water stream.
Preventing Elodea Colonization of Salmon Habitat
Alaska has one of the most productive salmon fisheries in the world but an invasive plant threatens the quality of lakes for salmon spawning. Funds from the Bipartisan Infrastructure Law (BIL) have energized early detection efforts to find and prevent the spread of non-native Elodea to freshwater salmon habitat.
A thick mat of elodea.
Improving Salmon Resilience to a Warming Climate
Salmon are the lifeblood of much of Alaska. Extensive river and lake systems protected in Alaska national parks provide significant habitat for all five species of Pacific salmon. As the climate warms, rising temperatures may threaten these important salmon resources. This project, funded by the Bipartisan Infrastructure Law (BIL), will describe reference conditions and potential targets for ecosystem recovery due to climate change, wildfires, oil spills, and other events.
Salmon swimming in blue-green water.
Alaska’s Endangered Heritage: Climate Change and Cultural Preservation
The rugged beauty of Alaska has been the homelands of Alaska Native people for thousands of generations. Today the relentless march of climate change threatens a range of cultural resources from archeological sites to historic cemeteries. Now the National Park Service is in a race to document heritage across the parklands in Alaska.
View of a snow-covered mountain from across a lake.
Project Profile: Mitigate Climate Change Impacts & Improve Subsistence Food Security Via Co-Stewardship Arrangements
The National Park Service will enhance climate change resilience and food security in rural Alaskan communities. The project prioritizes goals of building Tribal-NPS co-stewardship relationships that support Tribes’ ability to adapt to changing environmental conditions and associated food security challenges. Activities include improving harvest reporting strategies and conducting community harvest assessments. This project has additional goals to develop adaptive approaches.
Dried fish hanging overlooking a campsite in a forest clearing near a lake.
National Park Service
U.S. Department of the Interior
Gates of the Arctic National Park and Preserve
Photo by Andrew Ackerman
Arrigetch Peaks National Natural Landmark
The 40-square miles encompassing Arrigetch Peaks National Natural Landmark includes a wide spectrum of
ecologies: mountain terrain, alpine glaciers, tundra, high altitude rock desert and boreal forest.
Our Natural Heritage
National Natural Landmarks are sites that possess exceptional value in illustrating the natural heritage of our nation and present an unspoiled example of
natural history. The 40-square-mile area encompassing Arrigetch Peaks, considered to be of outstanding national importance, was declared a National Natural
Landmark many years before Gates of the Arctic National Park and Preserve
came into being around it.
The Arrigetch Peaks
The Arrigetch Peaks became a National
Natural Landmark in 1968, six years after
it was initially suggested by a geologist
doing studies in the central Brooks Range.
Considered an exceptional example of geologic formations, processes and history, and
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including multiple ecological communities,
it was also recognized for its spectacular
scenic attributes. Under the Bureau of Land
Management at the time, it eventually became
one of the iconic landmarks of Gates of the
Arctic National Park and Preserve.
National Park Service
U.S. Department of the Interior
Gates of the Arctic National Park and Preserve
Photo by Joe Wilkins
Made of solid bronze and weighing
in at over 25 pounds, a new plaque
commemorating Arrigetch Peaks
National Natural Landmark within
Gates of the Arctic National Park
and Preserve finally replaces the
original bronze plaque that had been
in the old ranger station in Bettles,
which was melted by the fire that
demolished the station in 2004.
The area encompasses a wide spectrum of
ecologies in a 40-square-mile area: mountain
terrain, alpine glaciers, tundra, high altitude
rock desert and boreal forest. Formed by glacial ice and running water, which lowered the
surrounding uplands, the Arrigetch Peaks are
an excellent example of alpine glacier activity.
Some of the oldest spruce trees in Alaska have
been found here, in isolated sites untouched
by wildfire.
“The Fingers of the Hand
Outstretched”
Long before early geologists came to survey
the area, the inland Nunamuit Eskimos called
the place Arrigetch, meaning “the fingers of
the hand outstretched.” They told a story of a
mighty hunter who taught them to survive in
the harsh arctic landscape. He showed them
the best animals to hunt and which plants to
use. Before he left he threw down his gloves
and transformed them into the towering granite spires of the Arrigetch, so that the people
would always remember him.
Still Inspiring Visitors
Today the area is still inspiring awe in visitors. The two day trek into the peaks from the
Alatna River presents the hiker with one scenic
vista after another, increasing in grandeur with
the altitude. Boreal forest becomes tundra,
the tundra changes to rock desert, and granite
rock faces rise as much as 4,000 feet above the
adjacent valleys. The jagged peaks and sheer
rock walls of this area are some of the most
spectacular in northern Alaska. It is truly a
natural national treasure.
For more information about the Arrigetch Peaks
National Natural Landmark within Gates of the
Arctic National Park and Preserve, please contact our
Interpretive Park Ranger in Bettles, DaleLynn Gardner,
at (907) 692-6100, or email her at
DaleLynn_Gardner@nps.gov.
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National Park Service
U.S. Department of the Interior
Gates of the Arctic National Park and Preserve
Photo by Andy Greenblatt
Keeping Tabs on Caribou and Moose Populations
Ten additional GPS-satellite radio-collars were
deployed on Western Arctic Herd (WAH) caribou. The collars provide biologists with the
locations of these caribou every 8 hours, 365
days a year—over 170,000 locations so far—
enabling biologists to track the migration and
distribution of caribou throughout the year.
Moose Project Nearing
Completion
The fieldwork for a multi-agency project
involving NPS, U.S. Fish & Wildlife Service,
Bureau of Land Management and Alaska
Dept. of Fish & Game is complete. About 70
collars were deployed on bull and cow moose
from the southern end of Kanuti National
Wildlife Refuge to Sukakpak Mountain. The
moose were located by aircraft monthly; about
30 moose had GPS collars that recorded their
positions every 8 hours. Most of the collars on
moose in the park have been removed.
The project’s goals are to increase our understanding of the distribution, movements,
A number of new caribou-related projects
have recently been initiated, including an
analysis of potential impacts of the proposed
Ambler Road and the Red Dog Road, investigating summer range quality and quantity, a
traditional ecological knowledge survey, and
a sport hunter survey. Check out the WAH
Working Group’s webpage at:
www.westernarcticcaribou.org
Photo by Jimmy Fox
Caribou Monitoring
Continues
habitat usage, and survival and twinning rates
of this population. We are currently analyzing
the data and hope to report results next year.
Gates of the Arctic National Park & Preserve
For more information about the caribou or moose
projects, contact Wildlife Biologist Kyle Joly at (907)
455-0626 or email him at Kyle_Joly@nps.gov.
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National Park Service
U.S. Department of the Interior
Gates of the Arctic National Park and Preserve
Eskimo Hunting Bow
These fragments of an Eskimo
hunting bow were a rare find
near the Nigu River in Gates
of the Arctic National Park
and Preserve. Most wooden
artifacts decay rapidly and
are rarely available to help
archeologists learn about early
lifeways of Eskimo peoples.
The hunting bow
was a fixture in most
prehistoric cultures
worldwide.
During the summer of 2008, National Park Service
archeologists Chris Ciancibelli and Dael Devenport
conducted a field survey in a high mountain valley
along the upper reaches of the Nigu, Alatna, and
Killik Rivers in the northwestern corner of Gates
of the Arctic National Park and Preserve. As part of
ongoing efforts to study the cultural resources within
the park’s boundaries, they documented artifacts,
campsites, and other indicators of the historic and
prehistoric presence of people on the landscape.
While walking over a gravelly, tundra-covered
lakeside terrace at the headwaters of the Nigu River
(see map), the researchers noticed a small scatter of
sticks. As they approached, they could confirm that
the driftwood-like weathered sticks on the ground
were actually pieces of a wooden hunting bow.
Finding this bow is remarkable because organic
artifacts, such as wood, skin, or bone, are usually
found only when preserved in permafrost, even
though archeological relics such as stone tools,
tent rings, and rock cairns are relatively common
finds throughout the Brooks Range. When organic
materials are lacking, archeologists can only gain
insight into the material culture of a people by way
of its stone technologies, losing the information-rich
associations of the organic components of hunting
weapons and other objects.
Analysis of the wooden bow
When reassembled from six fragments, the bow
measures about 127 cm (50 inches) in length. This
bow is the most complete specimen recovered to
date from the Brooks Range, as only small fragments
had been identified previously. Radiocarbon analysis
of a small sample from the bow dates the wood to the
late 1800s or early 1900s.
After comparing the bow to different known cultural
styles, Dr. Claire Alix (a specialist in wooden
artifacts at the University of Paris-Sorbonne, France)
classified the Nigu River bow as a reflexed Western
Arctic type bow. Reflexed refers to the shape of a bow,
which, when unstrung, forms a “C” that opens away
from the hunter. The reflexed Western Arctic type
of bow was first described by ethnographer John
Murdoch as one commonly used by Eskimo cultures
of northern Alaska and the Bering Strait. Murdoch
documented their material culture in the late 1800s
before the shift toward more modern technologies.
Looking at a piece of the wooden bow under
a microscope to identify wood characteristics
diagnostic to tree species, Alix concluded that the
Eskimos constructed the bow from either spruce
or tamarack. Neither species is readily available in
the Arctic tundra environment north of the Brooks
Range, but both are found along the southern edge of
the Range and as driftwood along the Arctic coastline.
The Eskimo hunting bow
The hunting bow was a fixture in most prehistoric
cultures worldwide. Each culture adapted the bow
to the local function and environment where the
weapon was used. Eskimo hunters migrating from
Siberia eastward across the Arctic are believed to
have introduced the bow to North America.
Many variations of the bow exist in Eskimo cultures,
as the bow has been used to hunt sea mammals, fish,
and a variety of terrestrial animals. Construction
techniques were equally diverse. Some bows were
composite, meaning they were made from multiple
parts and material types. For example, the handle
was often made of a stronger material such as bone,
which would add strength to the bow and allow for
the use of two separate lengths of wood.
the Nigu River artifacts, including the bow, were
made and used before Euro-American contact was
established.
Although Eskimo people are commonly thought
of as strictly coastal inhabitants, the archeological
record indicates their presence in the Brooks Range
for around 5,000 years. The Nunamiut are an inland
group of Iñupiaq Eskimos that have inhabited the
Gates of the Arctic region for the last 400-500 years.
Prior to settling in Anaktuvuk Pass in the 1940s, the
Nunamiut were nomadic hunters who relied on the
spring and fall migrations of the caribou through the
mountains. The Nigu bow is likely a remnant from
the nomadic period of the Numamiut people.
The wooden bow was found
at the headwaters of the Nigu
River (circled in map at top).
Eskimos using the Nigu River
site hunted in this landscape.
Dr. Claire Alix measures the
bow to determine its style and
material type.
Did Eskimos launch this stone
arrowhead also found at Nigu
River (bottom photo) with the
wooden bow?
Other artifacts at Nigu River
On searching the Nigu River site near the hunting
bow, park archeologists found ot
National Park Service
U.S. Department of the Interior
Gates of the Arctic National Park and Preserve
Paleo-Eskimo Culture at Matcharak Lake
Thousands of bones and
artifacts, well-preserved
within the permafrost layer,
were found at Matcharak
Lake. The 2008 excavations
have already confirmed many
assumptions about Denbigh
people 4000 years ago—the
extensive use of bone and
antler as tools, and that these
earliest of Paleo-Eskimos were
skilled artisans.
As archaeologists,
we realize that the
record will always be
incomplete; therefore,
we must work with
the information we
have.
Paleo-Eskimos are the ancient ancestors of modern
Eskimos, as recognized through archaeological
studies throughout Alaska, Canada, and Greenland.
In Alaska, the earliest members of this group are
known from a distinctive stone tool technology
known as the Denbigh Flint Complex (say DEN-bee).
When archaeologists talk about Denbigh, they are not
only referring to their material culture, i.e. the stone
tools, but also to the people who made them. More
broadly, Denbigh people are part of the Arctic Small
Tool tradition, who were the first humans to colonize
most of Arctic North America 5000 years ago.
The importance of bone
It is believed that Denbigh Paleo-Eskimos, after
processing animals for consumption, would often
discard the unusable remains in camp, away from
where people were working and sleeping. Rarely are
the bones of this type of midden (prehistoric trash
dump) discovered at ancient archaeology sites in the
Arctic.
Although 75 to 100 Denbigh sites are known in
Alaska, only a handful (literally) of bone fragments
are known from all of these sites. Without bones,
questions about diet, seasonal mobility, and hunting
strategies are unanswerable, although archaeologists
have proposed numerous hypotheses about Denbigh
life-ways.
However, at a recently-discovered site near
Matcharak Lake, in Gates of the Arctic National Park
and Preserve, the conditions of shallow permafrost
and the ongoing formation of peat were just right
to preserve the discarded remains of numerous
Denbigh meals—perfectly preserved until excavation
in 2008. With the discovery of a frozen bone midden
at Matcharak Lake, archaeologists can now begin to
reconstruct the behavior of these Native Alaskans.
Archeological discovery
The Matcharak Lake site perches on a 15-meter (45
foot) terrace between Matcharak Lake (see photo)
and the Noatak River. It was discovered through
routine archaeological survey of the upper Noatak
River drainage in 2007 by Andrew Tremayne and
Cody Strathe, both student archaeologists for the
National Park Service. Prior to this discovery, no
prehistoric sites were known in the area.
Recognizing the potential for recovering organics
(e.g., bone, antler, teeth, and plants) associated
with Denbigh Flint Complex tools, National Park
Service archeologist Jeff Rasic arranged for a team
of archeologists, including Tremayne, to excavate a
portion of the site in 2008.
Excavation at Matcharak Lake
To access this site, a crew consisting of Tremayne
and four other archeologists were flown by float
plane directly to the area of excavation. Technical
equipment was flown in,
including a total station
(surveying instrument) for
recording the exact location of
artifacts and bone, and screens for
sifting dirt to capture very small
artifacts. For three weeks, the
crew worked patiently and slowly,
waiting for the permafrost to melt
enough to actually dig in the soil.
Learning about Denbigh
At the Matcharak site, Tremayne
and the others recovered
thousands of bones of various
kinds (caribou, fish, and
migratory birds), along with tools
and incised-bone art work. Now,
the work of archeologists can
unfold further as they begin to
address some of the questions
that have puzzled them for years.
For his part, Tremayne has
chosen (for his Master’s thesis at
the University of Wyoming), to
analyze the site’s animal remains,
focusing on what the bones
reveal about the diet and hunting
strategies of site occupants.
However, as Tremayne explains,
because Matcharak Lake is a
localized, small-scale mountain
camp, he can only really talk
about how these Paleo-Eskimos
behaved while at that camp.
The discovery of unrivaled
preservation of bone,
including the articulated
caribou thorax (top), at
Matcharak Lake, makes this a
very important Denbigh site.
Incised bone artwork (middle)
and designed bone tools (L &
R, lower). The tool at right
is associated with a caribou
mandible and bone fragments.
Testing hypotheses about Paleo-Eskimo life-ways
Some researchers have suggested there is evidence
that Denbigh people spent their winters in the
mountains and the summer on the coast, but the
presence of at least one caribou fetal bone, fish, and
migratory birds at Matcharak Lake supports the
hypothesis that, at some point, Denbigh occupied
Matcharak Lake in early summer or spring.
If Denbigh hunters were specialized caribou hunters,
the expectation would be to find mostly caribou
bones. So,
National Park Service
U.S. Department of the Interior
Gates of the Arctic National Park and Preserve
NPS photo by Joe Keeney
Uncovering Prehistory at Lake Matcharak
Archaeologists at work on the Matcharak Peninsula Site, August 2013. This photo was taken about a week after
excavations began. The string grid helps to guide the archaeologists on where to excavate and is used to map
the exact location of each artifact that is found.
Human Occupations 7,000
Years Ago
From July 29 to August 17, 2013, NPS archaeologists Joe Keeney, Jillian Richie,
and Caroline Ketron, along with volunteer archaeologists Sam Hutchins and
Ryan Nordstrom, visited Lake Matcharak, a site along the Upper Noatak River in
Gates of the Arctic National Preserve, to expand on subsurface tests from previous years. The Matcharak Peninsula Site (AMR-196) is located on a south-facing
terrace, centered on a small peninsula along the southeast shore of the lake.
Keeney, a graduate student in the University
of Alaska Fairbanks department of anthropology, led the team with the goal to collect data
about the cultural materials buried beneath the
surface and how the overlying sediments were
deposited. The site is the focus of Keeney’s
master’s thesis research, and the data will
hopefully illustrate details about the people
inhabiting the site in prehistory. Radiocarbon
dates that are associated with stone tools
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and well-preserved bone recovered from the
site reflect human occupations to as early as
around 7,000 years ago, making it significant
as the largest collection of well-preserved
faunal remains from this time period and the
associated Northern Archaic technological
tradition. Analysis of the artifacts from this site
should shed light on life ways of these Arctic
hunter-gatherers, how they subsisted at Lake
Matcharak, when, and at what time of year.
National Park Service
U.S. Department of the Interior
Gates of the Arctic National Park and Preserve
During fieldwork, the archaeologists carefully
Meticulous Sifting and
Documenting Yields Results and systematically dug through approximately
microblades, and utilized flake tools. All sediments were backfilled upon completion of the
project to leave as little trace of the fieldwork
as possible.
7 m3 of surface sediments. They precisely
mapped over 500 bones, bone fragments,
stone tools, and flakes (the waste material
from manufacturing stone tools) using a total
station, a laser-based surveying instrument.
All dirt was sifted with a fine mesh to locate
artifacts too small to be seen during excavation and each artifact was then carefully
collected for later analysis. The first formal
tools recovered from the site were found this
summer, including the base of a side-notched
point (a tool indicative of Northern Archaic
technology), a microblade core, numerous
Photo courtesy of Brooks Range Aviation
NPS photo by Joe Keeney
The first formal tools
recovered from the site
were found this summer,
including the base of a
side-notched point (a tool
indicative of Northern
Archaic technology), a
microblade core, numerous
microblades, and utilized
flake tools.
The Matcharak Peninsula Site (AMR-196) was
originally identified in 2009 when NPS archaeologists discovered a 5,000 year-old caribou
bone and evidence of stone tools. The site was
then revisited in 2010 and 2011 for extended
testing, resulting in over 600 bones, bone
fragments, and stone tool flakes being recovered from approximately 6 m3 of excavated
sediments.
A conical microblade core discovered during
excavations at the Matcharak Peninsula Site in 2013.
The 2013 archaeology crew at Lake Matcharak.
From left are Ryan Nordstrom, Caroline Ketron, Sam
Hutchins, Jillian Richie, and Joe Keeney.
Gates of the Arctic National Park & Preserve
For more information about the work being done at
the Matcharak Peninsula Site, contact Archaeologist
Joe Keeney at (907) 455-0634, or email him at
Joseph_Keeney@nps.gov.
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National Park Service
U.S. Department of the Interior
Gates of the Arctic National Park and Preserve
Yukon-Charley National Preserve
Prehistoric Networking:
Obsidian in Gates of the Arctic National Park and Preserve
Long before the boundaries of the Gates of
the Arctic National Park were on the map,
people used the volcanic glass known as
obsidian to fashion projectile points, hide
scrapers and other tools. Archaeologists today are especially interested in these obsidian artifacts because they can tell presicely
where each piece of obsidian was collected
and how far a person, thousands of years
ago, carried their tools. Tracing obsidian
also allows archaeologists to make connections between archaeological sites.
This research is possible because each
obsidian source has a unique chemical
signature. Several methods can be used to
identify this signature and the geographic
source of the material. So far, close to 200
obsidian artifacts from Gates of the Arctic
have been analyzed. The obsidian entered
the central Brooks Range almost exclusively from the Batza Tena source on the
Koyukuk River, more than 200 km (125 mi)
south of the park.
Obsidian is found at over 200 archaeological sites in the Gates of the Arctic National Park and Preserve.
the XRF technology have brought about
portable instruments that make it possible
to analyze artifacts within the museums
rather than sending samples away for
analysis.
An obsidian flake from Itkillik Lake sourced to
Group P. The source for this obsidian has not yet
been discovered.
Formation of Obsidian
Obsidian is a volcanic glass that lacks a
crystal lattice structure because it formed
from a magma or lava that cooled very
rapidly. This geological characteristic makes
obsidian a perfect raw material for manufacturing stone tools because it flakes easily.
When this liquid rock cools, it traps the elements present in the molten liquid. These
trace elements occur in volcanic glass in
variable amounts, thereby creating a unique
chemical signature for any particular volcanic flow.
Obsidian Sourcing
The most reliable method of obsidian
sourcing involves using X-ray fluorescence
(XRF) or Inductively Coupled PlasmaMass Spectrometry (ICP-MS) to detect
the combination and proportions of trace
elements. The advantage of XRF spectrometers is that they do not destroy any part
of the artifact during the analysis; ICP-MS
leaves a scar barely visible with the naked
eye. In addition, recent developments in
Alaskan obsidian sources can be differentiated from one another by measuring levels
of iron, rubidium, strontium, zirconium,
and yttrium. Researchers have developed
databases that keep records of all sourced
obsidian. In all of Alaska, five obsidian
sources are known and more than 20
sources are represented by archaeological
samples from unknown geological sources.
By finding more samples from unknown
sources in archaeological sites researchers hope to determine an area where the
source is likely to be located.
Results of Obsidian Sourcing
Obsidian occurs in 211 (16%) of the 1300
known archaeological sites in the Gates of
the Arctic. So far, archaeologists have been
able to source obsidian from 25 sites in
several valleys, including the Killik, Alatna,
Nigu, Itkillik, North Fork of the Koyukuk,
and Hunt Fork of John River. Obsidian for
this analysis was also obtained from sites on
the shores of several lakes: Kurupa, Kipmik
and Agiak.
Most obsidian has been found on high
knolls where soil accumulation is marginal
and organic materials that can be dated (by
radiocarbon methods, for example) are
practically non-existent. However, based
on characteristic stone tool forms and the
few dated archaeological sites present in
the park, archaeologists have determined
that obsidian was used the entire time that
people have occupied the valleys of the
park, starting approximately 10,000 years
ago.
Nearly all obsidian found in the park
came from the Batza Tena source. Artifacts from this source are found across the
state (excluding the Aleutian Islands and
Southeast Alaska) and in all time periods.
The shortest distance that the obsidian had
to travel to the Gates of the Arctic from this
source is 175 km (110 mi), the longest is
340 km (210 mi). It is no surprise that this
obsidian is so common in the Gates of the
Arctic, since the source is relatively close
to the park and the Koyukuk River Valley
connects the two.
Only two obsidian artifacts found in the
Gates of the Arctic cannot be attributed to
the Batza Tena source. These came from
two different groups. A group designation
singifies that artifacts with a particular
chemical signature consistently appear at
archaeological sites, however the physical
source of that obsidian has not yet been
discovered. One of these samples, found
at Kurupa Lake, came from a source that is
referred to as Group G. Group G obsidian
is also found in archaeological sites in the
western Brooks Range. Another artifact
was attributed to Group P was found in the
National Park Service
U.S. Department of the Interior
Gates of the Arctic National Park and Preserve
Snowshoe Hare Project
A volunteer carefully searches a
plot for snowshoe hare pellets.
Each plot is 2 inches wide by 10 feet
long, delineated by an elastic band
wrapped around plastic stakes at each
end.
The fact that snowshoe hare populations cycle dramatically from very low to very
high densities over a 10 year period is fairly common knowledge. What is not as
well understood is what causes this cycling and what controls the amplitude of
hare population peaks. Some hare populations in and around Gates of the Arctic
National Park consume mineral soils when their populations become more dense.
Hare populations in these areas seem to reach higher densities than hare populations
that do not consume such minerals. Questions about how hare populations in “mineral” vs. “non-mineral” areas differ are a primary focus of this project.
7th Annual Pellet Count
During the 7th annual pellet count in 2013, a
total of 221 pellets were counted in 408 plots
at six sites. This continues the downward
trend from the mini-peak a few years ago
in the non-mineral sites of Rosie Creek and
Snowshoe Hare Annual Pellet Counts
Cathedral Mountain south of Coldfoot. At
Slate Creek, also a mineral site, and at the
mineral sites (Wiseman Creek, Jennie Creek
and Gold Creek), which did not experience
pronounced increases, the trend of low
numbers of hares
continues (Figure 1).
6.00
Figure 1. Number of snowshoe hare
pellets/plot deposited annually at six
study sites in the snowshoe hare study
area in and near Gates of the Arctic
National Park near Wiseman, Alaska.
# Pellets/Plot
5.00
Cathedral
Rosie
4.00
Slate
3.00
Wiseman
Jennie
2.00
Gold
1.00
0.00
2007
2008
2009
2010
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2011
2012
2013
The last major peak in
hare densities in our
area was in 1998-2001,
which we documented
in the park (our current
“Wiseman” site) using
winter track counts that
began in 1997.
National Park Service
U.S. Department of the Interior
Gates of the Arctic National Park and Preserve
Establishment of New Site
This grid may eventually replace
the nearby Jennie grid.
This large bluff lies across the
Hammond River from the Jennie
Creek pellet plot grid. During the
last major peak in snowshoe hare
densities, hares purportedly risked
exposure to predators to visit this
bluff and consume its soils.
In addition to checking the established pellet plots, we cleared pellets from 47 plots in
the new Hammond grid,
established in 2012. This
grid may eventually replace
the nearby Jennie grid if
the miner there bulldozes
his entire claim (on which
the Jennie grid lays). The
new site is as close to the
large Jennie Creek bluff
as we could put it (where
we believe hares consume
soil during extreme peak
population densities) while
being outside the mining claim area. With the
grid cleared of all old pellets, we will be ready
to conduct the first annual count at Hammond
in 2014.
Absolute Tree Densities at Jennie and Hammond Sites
In August, we made a second trip to the
snowshoe hare study area, mainly to collect
vegetation data from the
new Hammond site. We
recorded tree and shrub
densities and vegetation
strata from 50% of the
plots on the Hammond
grid. Density data show
that the Hammond site
has an even lower density of trees than Jennie
(Jennie already having the
lowest tree density of the
other six sites) (Figure
2). However, shrub density at Hammond is
greater than at Jennie (Figure 3), which has the
second greatest density of shrubs of all study sites.
Absolute Shrub Densities at Jennie and Hammond Sites
70,000
600
Picea glauca
Ribes triste
60,000
500
Vaccinium uliginosum
no trees (open)
400
Salix bebbiana
Betula papyrifera
300
50,000
Rosa acicularis
Juniperus communis
40,000
Potentilla fruticosa
Alnus crispa
Populus balsamifera
200
Populus balsamifera
30,000
Betula glandulosa
Picea glauca
Ledum palustre
20,000
100
0
Alnus crispa
Shepherdia canadensis
10,000
Jennie
Hammond
Salix spp.
0
Figure 2. Comparison of absolute tree densities on the
Jennie Creek grid and neighboring Hammond River
grid in the snowshoe hare study area near Wiseman,
Alaska. Tree density here is relatively low. The
Hammond site may need to replace Jennie if mining
operations in the area continue to spread.
Jennie
Hammond
Figure 3. Comparison of absolute shrub densities on
the Jennie Creek grid and neighboring Hammond
River grid in the snowshoe hare study area near
Wiseman, Alaska. The Hammond site has the second
greatest shrub density (after Cathedral Mountain) of
all seven sites in the snowshoe hare study area.
Gates of the Arctic National Park & Preserve
For more information on Gates of the Arctic National
Park and Preserve’s snowshoe hare project, contact
Donna DiFolco at (907) 455-0625 or email her at
Donna_DiFolco@nps.gov.
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National Park Service
U.S. Department of the Interior
Gates of the Arctic National Park and Preserve
Photo courtesy of Anchorage Museum
Subsistence Management in Gates of the Arctic
Protecting Subsistence
Rights
Anaktuvuk Pass residents hunting
caribou in 1962.
Subsistence Resource
Commissions
In 1980, Congress recognized the uniqueness and importance of a subsistence
way of life to rural residents by identifying it as one of the purposes of the Alaska
National Interest Lands Conservation Act (ANILCA). Through Title VIII of
ANILCA, Congress established a policy that rural residents engaged in a subsistence way of life be provided the opportunity to continue to do so, consistent
with sound management principles and the conservation of healthy fish and
wildlife populations; that the utilization of public lands in Alaska is to cause
the least adverse impact possible on rural residents who depend upon subsistence resources; that the non-wasteful subsistence uses of fish and wildlife be
the priority consumptive use; and that in managing subsistence activities, the
federal land managing agencies shall cooperate with adjacent landowners and
land managers, including tribal governments, Native corporations, and state and
federal agencies.
To achieve this complex synthesis of protection and use, Congress felt it was important
to formally involve those who have a personal knowledge of traditional subsistence
activities and resources on federal lands. For
national parks and monuments where subsistence uses were traditional, Subsistence
Resource Commissions were established to
make recommendations to the park superintendents, Secretary of Interior, and Governor
of Alaska on a hunting program for the park
areas.
The Gates of the Arctic National Park Subsistence
Resource Commission (SRC) was established
in 1982, and has been formally meeting with
National Park Service
U.S. Department of the Interior
Gates of the Arctic National Park and Preserve
Resident Zone Communities the NPS since 1984 to provide a sounding
Photo by Jack Reakoff
Wolverine pelts (right) and wolf hides (reversed) dry
outside a home in Wiseman, one of Gates of the
Arctic’s 11 resident zone communities.
Sleds are used to haul a harvested moose home from
the field.
Gates of the Arctic National Park & Preserve
For more information on Gates of the Arctic National
Park and Preserve’s Subsistence program, contact
Marcy Okada at (907) 455-0639 or email her at
Marcy_Okada@nps.gov.
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Photo by Heidi Schoppenhorst
The SRC is comprised of nine members
representing different geographical, cultural,
and user diversity for the Gates of the Arctic
region. Three members are appointed by the
Secretary of Interior, three appointed by the
Governor of Alaska, and three appointed by
Federal Regional Advisory Councils. The
Commission meets at least twice a year to
review regulatory wildlife and fisheries proposals and make recommendations which
may address major topics such as eligibility,
access, harvest monitoring, methods and
means of taking, research needs, use of cabins
and shelters, trapline management, and timber
management.
board for local concerns and develop a subsistence management program specific to Gates
of the Arctic. It was the intent of Congress to
limit eligibility for subsistence activities within
Gates of the Arctic National Park to local rural
residents who have a personal or family history
of use of park resources. Hence, 11 communities near Gates of the Arctic National Park
were designated as subsistence resident zone
communities for the park. Alatna, Allakaket,
Ambler, Anaktuvuk Pass, Bettles, Evansville,
Hughes, Kobuk, Nuiqsut, Shungnak, and
Wiseman were identified as communities with
a significant concentration of subsistence users
who have customarily and traditionally used
park resources and lands.
National Park Service
U.S. Department of the Interior
Gates of the Arctic National Park and Preserve
NPS photo by Chris Ciancibelli
Walker Lake
Archaeological
Survey
NPS Archaeologists record a site near
Walker Lake. Jillian Richie maps the
boundary of the site while Joe Keeney
documents and photographs each
artifact.
Located at the headwaters of the Kobuk River in Gates of the Arctic National
Park, Walker Lake was the focus for a National Park Service archaeological survey
in July 2013. A crew of four archaeologists evaluated the condition of known prehistoric sites, expanded survey coverage, and identified new archaeological sites.
Past surveys in the area documented small lithic scatters indicative of short-term
prehistoric hunting locations; results of the 2013 survey follow this tendency.
Discoveries of Ancient Sites Fourteen known archaeological sites were
revisited during the 2013 field season, and 16
Continue
new sites were discovered. The majority of
investigated sites are lithic scatters—remains
of chert, obsidian, and other stone material
discarded during ancient tool production. A
typical site contains one or more lithic scatters,
small in both number of artifacts and extent,
and is usually located on one of the many
elevated landforms near the lake (e.g. bedrock
knolls, beach ridges, and glacial moraines).
A small number of tools are present in some
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scatters, and include unifacial scrapers, expedient flake tools, microblades, biface preforms
and side-notched projectile points. Test pits
dug near lithic scatters have also revealed
prehistoric campfires, or hearths. Hearths are
particularly interesting to archaeologists for
their ability to preserve organic material like
charcoal or bone, which can indicate when
the fire last burned using radiocarbon dating.
Samples of bone and charcoal collected from
hearths at Walker Lake during the 2013 field
season date as old as 4,320 years ago.
National Park Service
U.S. Department of the Interior
Gates of the Arctic National Park and Preserve
NPS photo by Jillian Richie
NPS photo by Jillian Richie
These arctic huntergatherers used stone tools
to hunt and process a kill,
typically caribou, and
the elevated landforms
on which the tools were
discovered at Walker Lake
were likely used as lookouts.
A side-notched point discovered in 2013 during the
archaeological survey at Walker Lake. The notches
near the base allow the point to be securely fastened
to a shaft.
One of two sub-surface hearths found at Walker Lake
in 2013, evidenced by oxidized soil, bone fragments,
and flecks of charcoal.
Early Hunter-Gatherers at
Walker Lake
Information gained during the 2013 field
season is preliminary in nature, but the
archaeological sites dated in 2013 are most
likely associated with the Northern Archaic
tradition, a cultural and technological tradition
associated with hunter-gatherers across Alaska
and northwest Canada. These arctic huntergatherers used stone tools to hunt and process
a kill, typically caribou, and the elevated
landforms on which the tools were discovered
at Walker Lake were likely used as lookouts.
Additionally, the ephemeral nature of sites at
Walker Lake, along with artifact assemblages
that include end scrapers and bone fragments,
appears to reflect temporary hunting localities.
Cultural Resources at Risk
Cultural materials at Walker Lake are at a risk
of being disturbed by human collection, animal trampling, and other natural forces such
as fire and erosion. Despite this risk, the vast
majority of sites evaluated in 2013 are stable
and in good condition, with only minimal
impacts by human or natural disturbances.
Anyone can help maintain these, and other,
archaeological sites by leaving archaeological materials in their natural setting. If
you encounter a site or artifact, report it to
National Park Service staff with photographs
and detailed location information.
Gates of the Arctic National Park & Preserve
For more information on Gates of the Arctic’s
archaeological survey at Walker Lake, please contact
Jillian Richie at (907) 455-0630, or email her at
Jillian_D_Richie@nps.gov.
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National Parks in Alaska
Alaska National Parks
Alaska
National Park Service
U.S. Department of the Interior
Upper Noatak Valley, Gates of the Arctic National Park and Preserve
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GULF OF ALASKA
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NORTON SOUND
Alaska’s immense size can make travel to and through the
state challenging. Some planning is necessary. Just getting to
Alaska can be an adventure involving travel by air, highway, and
sea. Commercial airlines serve Anchorage, Fairbanks, Juneau,
and other towns, while cruise ships ply Alaska’s southeastern
waters through the Inside Passage. The Alaska Marine Highway
transports people and vehicles on ferries from the Lower 48 to
towns in Southeast Alaska and between points in Southcentral
Alaska. The Alaska Highway, paved in Alaska and most of Canada,
is open and maintained year-round. It extends 1500 miles from
Dawson Creek, British Columbia, to Fairbanks, Alaska, and
provides a land link with roads to the south.
Subsistence hunting, fshing and gathering by rural
Alaskans continues on many park lands here. These
customary and traditional uses of wild renewable
resources are for direct personal or family
consumption. Local residency and customary reliance
on these uses determines eligibility for continued
subsistence uses on national park lands.
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Uses of Park Lands: Many national park lands in
Alaska are designated as national preserves.This
designation allows for uses not typical in national
parks or national monuments in the continental
United States. Within these preserves, sport hunting
and trapping are permitted subject to state fsh and
game laws, seasons, and bag limits; and to federal
laws and regulations.
Gates of the Arctic
11
Kotzebue
Private Lands: Privately owned lands are located
within and next to park boundaries throughout Alaska.
These private lands are not open to public use or travel
without permission from the owners. Check with park
staff to determine the location of private lands and
public easements. Unauthorized use or travel across
private lands could be deemed criminal trespass.
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Travel Tips
Once in Alaska, you may have several options for travel to the
park lands. Unlike most National Park Service areas in the Lower
48, most in Alaska are not accessible by road. Scheduled air service
to towns and villages will put you within air-taxi distance of most
of these hard-to-reach parks. Experiencing Alaska’s more remote
treasures can require signifcant time, effort, and money and may
involve air or boat charters, rafts, kayaks, and hiking. See the back
of this brochure for access information for individual parks.
Inupiat Heritage Center
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For information about individual parks, contact them directly
(see back of this brochure) or visit the National Park Service
website at www.nps.gov/akso/index.cfm. For information
about national parks or other public lands in Alaska, visit or
contact the Alaska Public Lands Information Centers in
Anchorage, Fairbanks, Ketchikan, and Tok, or visit their
homepage at www.AlaskaCenters.gov.
• Anchorage: 605 West Fourth Avenue, Anchorage, AK 995012248, 907-644-3661 or 866-869-6887
• Fairbanks: Morris Thompson Cultural and Visitors Center,
101 Dunkel Street, Suite 110, Fairbanks, AK 99701-4848,
907-459-3730 or 866-869-6887
• Ketchikan: Southeast Alaska Discovery Center,
50 Main Street, Ketchikan, AK 99901-6659, 907-228-6220
• Tok: P.O. Box 359, Tok, AK 99780-0359, 907-883-5667
or 888-256-6784.
Tourist information is available from the Department of
Commerce, Community and Economic Development,
P.O. Box 110804, Juneau, AK 99811-0804,
www.travelalaska.com. For information about ferry or railroad
travel in Alaska, contact:
• Alaska Marine Highw
National Parks in Alaska Map
National Park Service
U.S. Department of the Interior