Aniakchak

https://www.nps.gov/ania/index.htm https://en.wikipedia.org/wiki/Assateague_Island_National_Seashore Aniakchak National Monument and Preserve is a U.S. National Monument and National Preserve, consisting of the region around the Aniakchak volcano on the Aleutian Range of south-western Alaska. Given its remote location and challenging weather conditions, Aniakchak is one of the most wild and least visited places in the National Park System. This landscape is a vibrant reminder of Alaska's location in the volcanically active "Ring of Fire," as it is home to an impressive six mile (10 km) wide, 2,500 ft (762 m) deep caldera formed during a massive volcanic eruption 3,500 years ago. Located on the Alaska Peninsula, 450 miles southwest of Anchorage, Aniakchak National Monument and Preserve is inaccessible by road. Notoriously bad weather makes access to Aniakchak unpredictable. Drop-offs and/or pick-ups may be significantly delayed. King Salmon Visitor Center Located next door to the King Salmon Airport, the King Salmon Visitor Center provides information on the many federal public lands of Southwest Alaska, particularly those in the Bristol Bay area. A large collection of films is available for viewing and an Alaska Geographic bookstore sells maps, charts, videos, posters, clothing and more. This visitor center is located next to the passenger terminal at the King Salmon Airport. Floating the Gates of Aniakchak A lone raft floats the Aniakchak Wild River as it flows through the "Gates" A lone raft floats the Aniakchak Wild River as it flows through the "Gates" Aniakchak Caldera Aerial shot of Aniakchak Caldera Aerial shot of Aniakchak Caldera Black Nose, Aniakchak Caldera Black Nose, Aniakchak Caldera Black Nose, Aniakchak Caldera Maar Lake, Aniakchak Caldera Maar Lake, Aniakchak Caldera Maar Lake, Aniakchak Caldera The Gates of Aniakchak The Gates of Aniakchak The Gates of Aniakchak 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. Science in Wilderness Marine Reserves ANILCA establishes the largest scientific laboratory...ever! A spawning salmon struggles to get back into the water. Balancing the Benefits and Impacts of Science in Alaska’s Wilderness Achieving consistency in permitting decisions across multiple units of the National Park System remains a constant challenge. When opportunities allow, park managers combine environmental compliance for related projects spanning several units, such as the installation of climate monitoring stations for the Inventory & Monitoring networks. A woman with long, dark hair, lilac shirt and jeans stands next to a climate monitoring station. 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. 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 NPS Geodiversity Atlas—Aniakchak National Monument & Preserve, Alaska Each park-specific page in the NPS Geodiversity Atlas provides basic information on the significant geologic features and processes occurring in the park. Links to products from Baseline Geologic and Soil Resources Inventories provide access to maps and reports. snow covered volcanic caldera Volcanic Hazards in Alaska’s National Parks There are over 100 volcanoes in Alaska, 54 of which are considered historically active, and 14 are found in Alaska national parks, preserves, and monuments. The Alaska Volcano Observatory monitors and conducts research on volcanoes in Alaska in order to better understand volcanic processes and determine the likelihood of future volcanic hazards, with a primary goal of informing the public about volcanic hazards and impending volcanic activity. Alaska Park Science 18(1), 2019. A snow covered volcanic peak. Duck-billed Dinosaurs (Hadrosauridae), Ancient Environments, and Cretaceous Beringia in Alaska’s National Parks This article presents new information from Aniakchak National Monument and Preserve on the Alaska Peninsula, that sheds light on the likely ancient environment that allowed the migration of one group of dinosaurs, the hadrosaurs (duck-billed dinosaurs), across Beringia during the Cretaceous. Alaska Park Science 17(1), 2018. An artists drawing of Hadrosaurs in Aniakchak. 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 POET Newsletter March 2013 Pacific Ocean Education Team (POET) newsletter from March 2013. Articles include: The Japan Tsunami Marine Debris Summary; Restoring "Plastic Beach" Back to Kamilo Point; Coming to a Beach Near You; and An Unexpected Visitor. dock on beach Conserving pinnipeds in Pacific Ocean parks in response to climate change The evolutionary record from previous climate perturbations indicates that marine mammals are highly vulnerable but also remarkably adaptable to climatic change in coastal ecosystems. Consequently, national parks in the Pacific, from Alaska to Hawaii, are faced with potentially dramatic changes in their marine mammal fauna, especially pinnipeds (seals and sea lions). black harbor seal 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 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: 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: 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 Cenozoic Era The Cenozoic Era (66 million years ago [MYA] through today) is the "Age of Mammals." North America’s characteristic landscapes began to develop during the Cenozoic. Birds and mammals rose in prominence after the extinction of giant reptiles. Common Cenozoic fossils include cat-like carnivores and early horses, as well as ice age woolly mammoths. fossils on display at a visitor center 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 18, Issue 1, Understanding and Preparing for Alaska's Geohazards Alaska is the most geologically active part of North America. Much of the awe-inspiring landscapes of Alaska's parks are created by geologic processes. But sometimes, these processes can be hazardous. This issue explores the state of the science to understand geohazards in Alaska national parks. Alaska Park Science 18(1): 2019. A man jumps down a dune of volcanic ash. Series: Alaska Park Science - Volume 17, Issue 1. Migration: On the Move in Alaska Alaska is home to many amazing animal migrations. In this issue, you will read about caribou, salmon, Golden Eagles, Swainson's Thrushes, beluga whales, and more. Human migrations have also occurred here, from ancient Beringia to the Klondike Gold Rush. You can even read about now-extinct species from the Cretaceous and Pleistocene eras. Enjoy this issue of Alaska Park Science and read about migration. Alaska Park Science 17(1), 2018. Caribou swim across a river. Quaternary Period—2.58 MYA to Today Massive ice sheets advanced and retreated across North America during much of the Quaternary, carving landscapes in many parks. Bering Land Bridge National Preserve contains geologic evidence of lower sea level during glacial periods, facilitating the prehistoric peopling of the Americas. The youngest rocks in the NPS include the lava of Hawaii Volcanoes National Park and the travertine at Yellowstone National Park, which can be just a few hours old. fossil bone bed and murals of mammoths Cenozoic Era The Cenozoic Era (66 million years ago [MYA] through today) is the "Age of Mammals." North America’s characteristic landscapes began to develop during the Cenozoic. Birds and mammals rose in prominence after the extinction of giant reptiles. Common Cenozoic fossils include cat-like carnivores and early horses, as well as ice age woolly mammoths. fossils on display in a visitor center 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 Series: Pacific Ocean Education Team (POET) Newsletters From 2009 to 2015, the Pacific Ocean Education Team published a series of short newsletters about the health of the ocean at various National Park Service sites in and around the Pacific Ocean. Topics covered included the 2010 tsunami, marine debris, sea star wasting disease, ocean acidification, and more. Ocean waves wash in from the right onto a forested and rocky shoreline. Fossil Footprints Across Our Parks / Huellas Fósiles a Través de Nuestros Parques Join us on a virtual hike to see fossil footprints across our national parks! As we travel back in time, we’ll discover stories of fantastic pasts and learn that fossil footprints are worthy of protection for the future. <br><br> ¡Únase a nosotros en una caminata para ver huellas fósiles en nuestros parques nacionales! Mientras viajamos a través del tiempo, descubriremos historias de pasados fantásticos y aprenderemos que las huellas fósiles merecen ser conservadas para el futuro. Two primitive tetrapods, looking something like giant lizards walking through desert sand dunes. Volcanic Processes—Lahars Lahars are volcanic mudflows and are among the most destructive of volcanic phenomena. Lahars present significant geohazards since they can travel great distances down river valleys and impact population centers away from the immediate area of a volcano. wide river valley filled with sediment and snowy peaks in the distance Aniakchak Volcano – Shaping the Cultural and Physical Landscape of the Alaska Peninsula The landscape of Aniakchak is a vibrant reminder of Alaska's location in the volcanically active Ring of Fire. In spite of such violent volcanic events, the living world, animal and human, eventually adjusted, recovered, and endured. The history of Aniakchak Caldera exemplifies the destructive force of nature while also demonstrating the resiliency of people. A lake in the middle of a caldera with high walls all around Sub-Plinian Eruptions Sub-Plinian eruptions create high eruption columns that are unsteady. Pyroclastic flows and lahars also form during these eruptions from composite volcanoes. volcanic ash eruption Plinian Eruptions Plinian eruptions are more intense than Sub-Plinean eruptions. Eruption columns may extend into the stratosphere and spread out in an umbrella shape and produce widespread ash deposits. Pyroclastic flows and lahars also occur during these eruptions. black and white photo May 18, 1980 Mount St. Helens eruption Volcanic Craters Craters are present at many volcanic vents. The size and shape of volcanic craters vary a great deal from volcano to volcano, and they even change during the lifespan of an active volcano. Craters can become filled by lava domes or lava flows, and new craters may form during subsequent eruptions. cinder cone crater Crater Lakes Water lakes may exist in craters and calderas (large collapse features) as these depressions can become filled by rainwater or melting snow or ice, or be places where groundwater can accumulate at the surface. Crater lakes can be long-lived or ephemeral, and may contain fresh or acidic waters. crater lake and snowy rim Maars and Tuff Rings Maars and tuff rings are low-standing pyroclastic cones with large craters that usually form from highly-explosive eruptions caused by the interaction of magma with ground or surface waters. Ubehebe Crater in Death Valley National Park is a maar. lakeshore and tundra Fumaroles Fumaroles are places where steam and volcanic gases are emitted. They are present on most active volcanoes. The occurrence of fumaroles and other geothermal features such as hot springs, geysers, and mud pots are important signs that a volcano is active. steam vents on the crater rim Magmatic Eruptions Magmatic eruptions include fresh lava or tephra from a magma source. Magmatic eruptions range from quiet effusions of lava to extremely explosive eruptions that can blow apart mountains and send ash clouds around the globe. volcanic eruption with glowing lava seen at night Composite Volcanoes (Stratovolcanoes) Composite volcanoes are made up of both lava flows and pyroclastic deposits and usually experience multiple eruptions over long periods of time. Mount Rainier is a composite volcano. photo of a snow covered volcanic peak Volcanic Domes Lava domes are steep-sided rounded accumulations of highly viscous silicic lava over a vent. Some domes are part of composite volcanoes, but large ones can make up their own volcanoes. Lassen Peak is a dome. photo of a rounded hill of blocky rock Cinder Cones Cinder cones are typically simple volcanoes that consist of accumulations of ash and cinders around a vent. Sunset Crater Volcano and Capulin Volcano are cinder cones. photo of a dry grassy field with a cinder cone in the distance Series: Volcanic Features Volcanoes vary greatly in size and shape. Volcanoes also may have a variety of other features, which in turn, have a great range in diversity of form, size, shape, and permanence. Many volcanoes have craters at their summits and/or at the location of other vents. Some craters contain water lakes. Lakes of molten or solidified lava may exist on some volcanoes. Fumaroles and other geothermal features are a product of heat from magma reservoirs and volcanic gases. photo of a lava lake in a summit crater 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 Summit Calderas Summit calderas form on preexisting composite volcanoes that experience VEI 6-7 eruptions that cause their summits to collapse. Summit calderas may become filled with precipitation to form steady-stake lakes, although these lakes may also be drained if the caldera rim becomes breached. photo of a snow covered volcanic summit caldera Calderas Calderas are large collapse features that can be many miles in diameter. They form during especially large eruptions when the magma chamber is partially emptied, and the ground above it collapses into the momentary void. Crater Lake and Aniakchak Crater are calderas. photo of oblique aerial view of a volcanic caldera with snow and ice Series: Volcano Types Volcanoes vary in size from small cinder cones that stand only a few hundred feet tall to the most massive mountains on earth. photo of a volcanic mountain with snow and ice Explosive Calderas Explosive calderas result from violent eruptions of great quantities of silicic magmas. These eruptions produce massive eruption columns that extend into the stratosphere, and voluminous pyroclastic flows. Eruptions that produce explosive calderas generally range from 6 (Colossal) on the Volcanic Explosivity Index (VEI) to 8 super eruptions (Apocalyptic). digital oblique aerial image of a volcanic caldera Series: Volcanic Eruption Styles Categories in this traditional classification are based on the eruption styles of particular volcanoes. These magmatic eruption styles are listed in the order of increasing explosivity. volcanic eruption with glowing lava Pyroclastic Flows and Ignimbrites, and Pyroclastic Surges Pyroclastic flows and surges are among the most awesome and most destructive of all volcanic phenomena. Pyroclastic flow deposits are found in at least 21 units of the National Park System. photo of a cloud of ash and dust moving down a mountain side. Volcanic Ash, Tephra Fall, and Fallout Deposits Volcanic ash, pumice, and tephra ejected in volcanic eruptions ultimately falls back to Earth where it covers the ground. These deposits may be the thin dustings or may be many tens of feet (meters) thick near an eruptive vent. Volcanic ash and tephra can present geohazards that are present great distances from the erupting volcano. photo of a bluff with exposed fine-grained volcanic ash and pumice. Series: Volcanic Eruption Types The most fundamental way to characterize a volcanic eruption is whether it is magmatic, phreatic, or phreatomagmatic. volcanic eruption seen at a distance 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 Series: Park Paleontology News - Vol. 15, No. 2, Fall 2023 All across the park system, scientists, rangers, and interpreters are engaged in the important work of studying, protecting, and sharing our rich fossil heritage. <a href="https://www.nps.gov/subjects/fossils/newsletters.htm">Park Paleontology news</a> provides a close up look at the important work of caring for these irreplaceable resources. <ul><li>Contribute to Park Paleontology News by contacting the <a href="https://www.nps.gov/common/utilities/sendmail/sendemail.cfm?o=5D8CD5B898DDBB8387BA1DBBFD02A8AE4FBD489F4FF88B9049&r=/subjects/geoscientistsinparks/photo-galleries.htm">newsletter editor</a></li><li>Learn more about <a href="https://www.nps.gov/subjects/fossils/">Fossils & Paleontology</a> </li><li>Celebrate <a href="https://www.nps.gov/subjects/fossilday/">National Fossil Day</a> with events across the nation</li></ul> Photo of a boulder with a dinosaur track on one side. Tertiary Fossil Floras of Alaskan National Parks The National Park Service units of Alaska have an outstanding fossil record, including fossil plants. Six Alaskan NPS units preserve notable plant fossils of Tertiary age (Paleocene through Pliocene Epochs, 66 to 2.58 million years ago). These fossils were first documented in 1869 and show a major change going from the Eocene to the Oligocene about 34 million years ago. Photo with to fossil leaves. 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. Shrinking Glaciers in Aniakchak National Monument and Preserve Aniakchak National Monument and Preserve is one of nine national parks in Alaska with glaciers. Aniakchak is one of the smallest glaciated parks in the state and has one of the smallest proportions of glacier-covered area (0.1%). Glacier cover in Aniakchak decreased by 14% from the 1950s to the 2000s, and our most recent study found a decrease in area from 1985 to 2020. An historic photo of Aniakchak Caldera. 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.

Park Info National Park Service U.S. Department of the Interior Te Novarupta A trip planning and information guide to Alagnak Wild River Aniakchak National Monument and Preserve Katmai National Park and Preserve PHOTO COURTESY S. GAGE Issue Number 2022 What’s Inside: PHOTO COURTESY L. LAW NATIONAL GEOGRAPHIC SOCIETY NPS PHOTO Brooks Camp ..............6 Katmai Origins...........14 Backcountry Travel ...20 Three National Parks, Many Amazing Experiences National Park Service U.S. Department of the Interior Alagnak Wild River Aniakchak National Monument and Preserve Katmai National Park and Preserve Katmai was declared a National Monument in 1918; Aniakchak in 1978. The Alaska National Interest Lands Conservation Act of 1980 established Alagnak Wild River, while Katmai and Aniakchak were expanded to include national preserve areas. Katmai was also redesignated a national park. Together, these lands encompass nearly fve million acres of unique landscapes managed by the National Park Service. Mailing Address PO Box 7 King Salmon, AK 99613 Park Headquarters Phone: 907-246-3305 Websites Alagnak: www.nps.gov/alag Aniakchak: www.nps.gov/ania Katmai: www.nps.gov/katm NPS Mobile App Download the app and content from entire parks for offine use prior to visiting as there is limited to no service. Welcome to Katmai Country Welcome to Katmai! Katmai National Park and Preserve (Katmai) lies within the ancestral homelands of the Alutiit-Sugpiat (Aleut) people. Human habitation of this region goes back many thousands of years and speaks of thriving communities and perseverance in the face of challenging environments. Today, the Alutiit-Sugpiat people strive to maintain their traditional lifeways even in light of pressure brought on by an ever-changing world. Their connections to these lands are enduring and worthy of our respect. Accordingly, I would like to take a moment to acknowledge our Alaska Native communities—be they Alutiit-Sugpiat, Dena’ina, or Yup’ik—for their enduring legacy as the caretakers of this wonderous land we are fortunate to experience, and today call Katmai. Geographically, Katmai is found on the Alaska Peninsula which encompasses a vast and beautiful landscape where the National Park Service also has the privilege of managing Aniakchak National Monument and Preserve, and the Alagnak Wild River. Regardless of your interests, collectively these diferent park areas ofer a diversity of outstanding Alaskan experiences. The geology of Katmai is both ancient and new. The park’s diverse landscapes comprise expansive mountains, active volcanoes, fowing glaciers and a wild and beautiful seacoast that is frequently fed by sparkling rivers and lakes. The cataclysmic eruption of Novarupta in 1912 took place long ago when compared to a human lifespan but is geologically recent. The resulting ash covered everything for miles and even today life is still recovering from the efects of the eruption. Many dedicated individuals from diverse walks of life have worked tirelessly over the years to ensure that wildlife remains abundant and diverse throughout this region. It is in large part because of these eforts that Katmai today supports world-class fsheries and outstanding wildlife viewing opportunities. To observe an Alaskan brown bear in its natural environment is a testament to the priorities of our nation. We hope that you have the opportunity to experience these special places for yourself. Those that journey here are sure to take back memories that will last a lifetime. Mark Sturm, Superintendent NPS/L. LAW Social Media Contents: Southwest Alaska’s Parklands.................................................2-3 Essential Information..................................................................4 Getting Here, Getting Around ...................................................5 Welcome to Brooks Camp .......................................................6-7 Camping at Brooks Camp ...........................................................8 Brooks Camp Map .......................................................................9 Bear Viewing ........................................................................10-11 Safe Travels in Bear Country ....................................................12 Live Bearcams............................................................................13 2 The Novarupta Katmai and the National Park Idea.....................................14-15 Exploring the Human History of Katmai .................................16 Cycle of the Salmon ..................................................................17 Fishing Information ..................................................................18 Photographing a Wild Heritage & Katmai’s Wildlife ..............19 Backcountry Travel...............................................................20-21 Aniakchak National Monument..........................................22-23 Alagnak Wild River ..........................

Sutwick Island Y P res e r ve b o u nd a e C r eek Cr ee k E k For Cr ee k rt h ee KUJULI K k 2360ft 719m Ri v Cr e ek M e lo y Jaw Mountain er hn so n Cr ee k Pinnacle Mountain A L E U T I A N 2618ft 798m ( Big ) hak Jo Meshik Lake 2295ft 699m Sh akc Ani 2470ft 753m dd Hi Black Nose io Rudy R A N G E re e um en Ri v t 3350ft 1022m ANIAKCHAK CALDERA Half Cone Lava P l en t y Lava Birthday Pass 2050ft 625m 2355ft 718m Bir th y da r pu eek Cr r Ba To Meshik (village) and Port Heiden Airfield Cr e ) ek er) Riv lis h C re k) Re ind r ee th or (N qu e ee na nd k na i Re ee ( Ta Cr Tephra deposits from Aniakchak eruption 3,700 years ago. ab a ar (S ek rv on se lM Surprise Lake 3460ft 1055m Na Vent Mountain 1055ft 322m ek Cre Creek lP na na at 2885ft 879m 4400ft 1341m Ra i nb o w io Aniakchak Peak The Gates N r nal P ent Natio onum al M n io t Na at Creek Mes hik Creek Cub en Wall The Gard 3800ft 1158m N e eserv H i gh ANIAKCHAK NATIONAL MONUMENT ek en Cre Lava C re e k ANIAKCHAK NATIONAL PRESERVE Cr e Creek oe Ci n d e r BAY Fork rth No rt Wiggly My s Elephant Mountain Cr tery River n) Cre ek be go Black Cape Horn 2280ft 695m Villag eC r Al a (Sh CAPE KUMLIK Aniakchak Lagoon No ANIAKCHAK NATIONAL PRESERVE BAY Columbia River Packers Cabin 1481ft 451m Cr R A N G 2430ft 741m Elephant Head Point ANIAKCHAK ek st We ek C re e k re Ray eC mic Pu Cape Ayutka B A Y n Mai 933m Kumlik Island Garden Island A M B E R N o r the a s t A L E U T I A N 3060ft Eagle Island ry O C E A N All offshore islands shown on this map are administered by Alaska Maritime NWR. The Twins 3268ft 996m i arn nt Ya l Na t i o na CAPE KUNMIK 3271ft 997m ek P A C I F I C 1371ft 419m ek ALASKA PENINSULA N AT I O N A L W I L D L I F E R E F U G E Bear Cre ek tio na lP re se f 3030ft 924m Bay ol Cre ni er rv e bo W ALASKA PENINSULA N AT I O N A L W I L D L I F E R E F U G E tar an un da ry 

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 C U H K S I CH BEAUFORT Noatak Noata k Cape Krusenstern 2 r ve River 7 er A IT Kobuk Valley Riv S TR 10 ko Yu uk uk n upi ne Fort Yukon iv e Circle BE RI Koy Bering Land Bridge P o rc Bettles/Evansville C AN AD A AT ES U N IT ED ST NG 12 Kobuk r R i v er 4 Yukon-Charley Rivers Fairbanks Alaska Public Lands Information Center on Tana n iv ver i t na Sus 1 Eagle River Anchorage 1 T LE OK CO Nus ha Dillingham 1 Homer ST O L Yakutat Kenai Fjords Glacier Bay GULF OF ALASKA Juneau Gustavus Katmai Y Sitka Petersburg Hoonah Kodiak Sitka Stra it Port Heiden Skagway Haines DA ES NA TAT CA D S E IT I BR A Klondike Gold Rush Seward King Salmon B Mt. St. Elias 18008ft 5489m Cordova UN SEA K WrangellSaint Elias C ha BERING KO 9 4 tham S KU W Soldotna 1 Valdez McCarthy IN Rive r Y B A Iliamna k ga Chitina er Prince William Sound Kenai Lake Clark Nabesna Gulkana Palmer Bethel IM River Ku sko kw im Glennallen 5 2 1 Slana 3 13 Alaska Public Lands Information Center Tok 8 River 8 5 Ri 4 Mt. McKinley 20320ft 6194m Alaska Public Lands Information Center a 2 McKinley Park Denali R Eagle 2 3 er Yu k 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. 6 2 Nome Copp S IA S S TAT E U R S ED IT UN 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. 6 9 KOTZEBUE SOUND SEA Anaktuvuk Pass Rive r 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 EA R 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