Parashant

https://www.nps.gov/para/index.htm https://en.wikipedia.org/wiki/Grand_Canyon-Parashant_National_Monument Grand Canyon-Parashant National Monument is located on the northern edge of the Grand Canyon in northwest Arizona. The national monument is a very remote and undeveloped place jointly managed by the National Park Service (NPS) and the Bureau of Land Management (BLM). There are no paved roads into the monument and no visitor services. Take a lonely and rocky two-track road in a 4x4 to the edge of the Grand Wash Cliffs. Find a stunning solitary vista deep into the Grand Canyon. Relax in the shade of ponderosas at Mount Trumbull. Touch ancient waters at Pakoon Springs in one of the driest places in the world. Parashant is remote. There are no crowds here. Be equipped to leave pavement, cell service, and the 21st century behind. • The monument is located in the northwest corner of Arizona, bordering Nevada to the west and near the southern border of Utah. The monument has entry roads from Nevada, Utah and Arizona. • There are no paved roads or visitor services within the monument's million-plus acres. • Visitors should be prepared for travel on rugged dirt roads, with an appropriate high-clearance vehicle equipped with all-terrain tires. Spare tires should also be all-terrain rated. Public Lands Information Center This federal interagency office is staffed by employees from the National Park Service, Bureau of Land Management, U.S National Forest Service, and by dedicated volunteers from the local community. The Public Lands Information Center provides recreational information and maps for federal lands managed in southwest Utah, northwest Arizona, and eastern Nevada. From I-15 southbound take Exit 6. Turn left on UT-18/Bluff St and continue for approximately 0.5 miles. Turn left into the parking lot. From I-15 northbound take Exit 6. Turn right on UT-18/Bluff St and continue for approximately 0.4 miles. Turn left into the parking lot. Hudson Point Near a cliff edge the sun sets in the distance. The sun sets behind the Pakoon Basin. Driving the sage flat A UTV drives down a road surrounded on both sides by sage Visitors enjoy exploring the roads on the monument. Camping sunset The sun sets behind a grove of ponderosa trees lighting up an orange tent with a warm glow Campsites on the monument are primitive as there is no designated campground. Waring Ranch Looking across a long narrow stockpond. Green grass slopes towards the water. Areas such as Waring Ranch give a glimpse into ranching operations in the early and mid-20th century Fall sunset The setting sun sits above trees and shrubs adorned with hues of orange, red and green. Sunrise and sunsets hallmark the vast landscapes of the monument. California Condor Species description of the California Condor (Gymnogyps californianus). An adult condor with the wing tag label number 80 stands over a juvenile condor. Partnerships between Resources and Fire Benefit Cultural Landscapes at Parashant National Monument Over the past several years, the fire program for Lake Mead National Recreation Area (LAKE) and Grand Canyon-Parashant National Monument (PARA) has made strides in benefitting cultural and natural resources at both units. Firefighter protects a fence during a prescribed burn Survival of the Southern Paiute The Paiutes have overcome insurmountable challenges and devastation as a people. Their long struggle to preserve the Paiute way and flourish continues. But they will not give up. Instead, they celebrate their achievements, promising that while “[t]he struggle is long and difficult… the Paiute will survive.” Native American man in ceremonial dress with orange cliffs in the background. California Condor Reintroduction & Recovery A tagged California condor flies free. NPS Photo/ Don Sutherland A wing-tagged California condor flying in the blue sky. SW CA Condor Update - 2017-01 (January) From January 2017: An update from Grand Canyon National Park on the California Condor recovery program for the Arizona/ Utah population. A condor flying wild and free. SW CA Condor Update - 2015-11 (November) From November 2015: An update from Grand Canyon National Park on the California Condor recovery program for the Arizona/ Utah population. A condor flying wild and free. SW CA Condor Update - 2015-02 (February) From February 2015: An update from Grand Canyon National Park on the California Condor recovery program for the Arizona/ Utah population. A condor flying wild and free. SW CA Condor Update - 2014-11 (November) From November 2014: An update from Grand Canyon National Park on the California Condor recovery program for the Arizona/ Utah population. A condor flying wild and free. SW CA Condor Update - 2015-07 (July) From July 2015: An update from Grand Canyon National Park on the California Condor recovery program for the Arizona/ Utah population. A condor flying wild and free. SW CA Condor Update - 2016-04 (April) From April 2016: An update from Grand Canyon National Park on the California Condor recovery program for the Arizona/ Utah population. A condor flying wild and free. World CA Condor Update - 2016 Population Status An update on the world California Condor population for 2016. A close up of the pink bald head of a California condor with a ruffle of black feathers. World CA Condor Update - 2017 An update on the world California Condor population for 2017. A close-up of the pink bald head of a California condor with a ruffle of black feathers. Tassi Ranch Cultural Landscape North of the Grand Canyon in the Mojave Desert lies Tassi Ranch, approximately 200 acres of creosote bush ranchland in Grand Canyon-Parashant National Monument. Today, the remnants of the early twentieth century ranch can be found under the shade of an oasis of cottonwood trees, fed by the Tassi Springs near the center of the ranch. The adaptations the ranchers undertook as they worked to establish agriculture in an extreme, remote desert are still visible in the landscape. Tassi Ranch 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 Permian Period—298.9 to 251.9 MYA The massive cliffs of El Capitan in Guadalupe Mountains National Park represent a Permian-age reef along the supercontinent Pangaea. The uppermost rocks of Grand Canyon National Park are also Permian. flat-top mountain Pennsylvanian Period—323.2 to 298.9 MYA Rocks in Cumberland Gap National Historical Park represent vast Pennsylvanian-age swamps. Plant life in those swamps later became coal found in the eastern United States. fossil tracks on sandstone slab 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 Paleontology in Parashant: No Bones About It In late 2020, Geoscientists-in-the-Parks participants Holley Flora and Rose Weeks conducted a paleontological resource inventory in Grand Canyon-Parashant National Monument, Arizona. This monument has notable Paleozoic invertebrate fossils and Quaternary cave fossils. Fieldwork in this large, remote monument is both challenging and rewarding. two people working on a fossil Series: Park Paleontology News - Vol. 13, No. 1, Spring 2021 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> park ranger in uniform Hawaiian Eruptions Fire-fountains and effusive outpourings of very fluid basaltic lavas are the hallmarks of Hawaiian style eruptions. Lava curtain 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 Andrus Canyon Fire – Suppression Success at Grand Canyon-Parashant National Monument In late June 2021, the lightning-ignited Andrus Canyon Fire was discovered burning in a pinyon-juniper dominated woodland with little to no understory on the eastern side of Grand Canyon-Parashant National Monument. Previous relationships with the Bureau of Land Management (BLM), Color County Interagency Fire Center, and other partners allowed NPS fire leadership to quickly mobilize personnel and crews. A row of firefighters looks over the edge of a canyon onto a desert landscape. 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 Changing Patterns of Water Availability May Change Vegetation Composition in US National Parks Across the US, changes in water availability are altering which plants grow where. These changes are evident at a broad scale. But not all areas experience the same climate in the same way, even within the boundaries of a single national park. A new dataset gives park managers a valuable tool for understanding why vegetation has changed and how it might change in the future under different climate-change scenarios. Green, orange, and dead grey junipers in red soil, mountains in background 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 Volcanic Inverted Topography Inverted topography arises when lava flows that filled valleys at the time of their eruption later hold up mesas because their resistance to erosion is greater than most other rock types. photo of volcanic rock with petroglyphs and a distant mesa 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 Monogenetic Volcanic Fields Monogenetic volcanic fields are areas covered by volcanic rocks where each of the volcanic vents typically only erupt once. Monogenetic volcanic fields typically contain cinder cones, fissure volcanoes, and/or maars and tuff rings. They also usually encompass large areas covered by basaltic lava flows. oblique aerial photo of a lava flow that extended into a body of water 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 Volcanic Necks and Plugs Volcanic necks are the remnants of a volcano’s conduit and plumbing system that remain after most of the rest of the volcano has been eroded away. photo of a riverside rocky spire with mountains in the distance Pillow Basalts Pillow basalts are named for the rounded shapes that form when lava cools rapidly underwater. photo of golden gate bridge Studying the Past and Predicting the Future Using Rat Nests In the western United States, packrat middens are one of the best tools for reconstructing recent environments and climates. These accumulations of plant fragments, small vertebrate remains, rodent droppings, and other fossils can be preserved for more than 50,000 years. Packrat middens have been found in at least 41 National Park Service units. Photo of a wood rat. Series: Park Paleontology News - Vol. 14, No. 2, Fall 2022 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 person sitting while using a laboratory microscope. 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 NPS Establishes NPSage Initiative to Restore Sagebrush-Steppe Ecosystems Artemisia species, commonly known as sagebrush, are far from being the only species on the landscape. The sagebrush biome is composed of a rich mosaic of thousands of diverse plant species, which are largely driven by differences in climate, soil and elevation. These distinct sagebrush plant and animal communities occur in approximately 70 park units across the western U.S— all of which are experiencing significant threats from wildfire and droughts. Two NPS staff knealing next to plants growing in a nursery Bats Are in Danger. Here’s How and Why We’re Helping Them. Bats are amazing animals and a formidable force against insect pests, but a nasty fungal disease is killing them. A coordinated national response brings hope. GIF of a bat with big ears in a gloved hand, rotating its head and opening and closing its mouth. Project Profile: Develop Native Plant Capacity for Sagebrush Parks The National Park Service will establish a native seed collection and plant propagation facility on the Oregon State University (OSU)-Cascades Campus, in partnership with the Bureau of Land Management, U.S. Forest Service, Confederated Tribes of Warm Springs, and private industry. a sagebrush steppe environment adjacent to a yellow aspen grove on a hillside