"This bundle of intertwining, twisting cave formations were probably formed by capillary action. The mineral calcite is very pure white in these formations." by U.S. National Park Service , public domain

Timpanogos Cave

National Monument - Utah

Timpanogos Cave National Monument protects the Timpanogos Cave Historic District and a cave system on Mount Timpanogos in the Wasatch Mountains in American Fork Canyon near American Fork, Utah.

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Map of the U.S. National Park System. Published by the National Park Service (NPS).National Park System - National Park Units

Map of the U.S. National Park System. Published by the National Park Service (NPS).

Map of the U.S. National Park System with Unified Regions. Published by the National Park Service (NPS).National Park System - National Park Units and Regions

Map of the U.S. National Park System with Unified Regions. Published by the National Park Service (NPS).

Map of the U.S. National Heritage Areas. Published by the National Park Service (NPS).National Park System - National Heritage Areas

Map of the U.S. National Heritage Areas. Published by the National Park Service (NPS).

https://www.nps.gov/tica/index.htm https://en.wikipedia.org/wiki/Timpanogos_Cave_National_Monument Timpanogos Cave National Monument protects the Timpanogos Cave Historic District and a cave system on Mount Timpanogos in the Wasatch Mountains in American Fork Canyon near American Fork, Utah. Hike your way past stunning vistas to explore a hidden underground world. Taste the thrill of caving as you twist and bend to enter beautifully decorated rooms. Learn the science behind formations and hear stories of cave exploration and preservation. Experience and discover as you go – geologic mysteries await. From I-15: Take Exit 284 (Alpine-Highland exit), turn east on State Highway 92 and proceed ten miles (16km) to the monument. UT 40 or U.S. 189: Travel UT 189 through Provo Canyon, west on Orem 800 North (UT 52). After 2.4 miles turn right on State Street UT- 89. After 3.8 miles, turn onto Pleasant Grove 100 East (UT 146). Stay on this road for almost five miles, as it turns in Canyon Road and takes you to the mouth of American Fork Canyon. Turn right up American Fork Canyon to visitor center. Timpanogos Cave Visitor Center The Timpanogos Cave Visitor Center is located in American Fork Canyon on UT-92. It sits at the base of the cave trail that leads to Timpanogos Cave. The visitor center is generally closed when the cave tours are closed. See https://www.nps.gov/tica/planyourvisit/hours.htm for the most up-to-date information. From I-15: take Exit 284 (Alpine-Highland exit), turn east on UT-92, drive 10 miles (16km) to the monument. From UT 40: from Heber or Provo Canyon travel on UT40 through Provo Canyon, turning west onto Orem 800 North (UT 52), then after 2.4 miles turn right onto State Street (Hwy 89). After 3.8 miles, turn onto Pleasant Grove 100 East (UT 146). Stay on this road for five miles, as it turns into Canyon Rd and takes you to the mouth of American Fork Canyon. When Canyon Rd ends, turn right into the canyon. Helictites in Timpanogos Cave Twisty helictites growing off a stalactite Timpanogos Cave is filled with twisting helictites and other beautiful formations Timpanogos Cave's "Chimes Chamber" Visitors gaze at delicate cave formations in Timpanogos Cave's Chimes Chamber Timpanogos Cave's beautiful Chimes Chamber is filled with delicate cave formations Hansen Cave-Introduction to Caving Tour Two cavers look at large formations in Hansen Cave Cavers on the Introduction to Caving Tour admire magnificent formations. View from the Timpanogos Cave Trail Utah Valley beyond the steep cliffs and fir trees of American Fork Canyon The scenic view from the trail to the caves is one people often remember. Along the Trail to the Caves White-orange quartzite surrounded by greenery stands against a blue sky The trail to the cave leads the hiker past layer after layer of geologic time 2011 NPS Environmental Achievement Awards Recipients of the 2011 NPS Environmental Achievement Awards Arches National Park’s Free-Flowing Waters Visitors to Arches National Park experience natural free-flowing waters and have water to quench their thirst, thanks to an agreement between the National Park Service and the State of Utah. The sun sits just below the horizon behind Delicate Arch. Contaminants of Emerging Concern in Northern Colorado Plateau Park Waters Pesticides, antibiotics, and personal care products are all being found in streams and rivers. But would you expect to find them in a national park? On the northern Colorado Plateau, scientists found that even in isolated areas, these "contaminants of emerging concern" are not uncommon. Find out what we found where--and how you can help. Ripples in cave water About The Southern Paiute “Paa” ute means water ute, and explains the Southern Paiute preference for living near water sources. The Spanish explorer Escalante kept detailed journals of his travels in the Southwest and made notes concerning Southern Paiute horticulture, writing in 1776, that there were “well dug irrigation ditches” being used to water small fields of corn, pumpkins, squash, and sunflowers. Southern Paiute boy by wickiup shelter. Bats in Caves Bats and caves go together in people's minds. National Parks are home to many important bat caves. But, bats are particular. Many caves only contain a few bats. Some bats like certain caves for raising their young and other caves for winter hibernation. Other bats avoid caves entirely and sleep and raise their young in protected locations in trees and rocks outside. a group of bats hanging on a cave ceiling NPS Geodiversity Atlas—Timpanogos Cave National Monument, Utah 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. [Site Under Development] canyon and cliffs Cave Research Activities and Documented Vandalism Core samples were taken from two stalagmites and some flowstone in the Timpanogos Cave System to determine stable isotope geochemistry in an effect to assess whether Lake Bonneville produced lake-effect snow on the glaciers found within the Wasatch Range. Additionally, an attempted break-in damaged one of the entrance doors to the cave. cave formation with hole drilled What We’re Learning and Why it Matters: Long-Term Monitoring on the Northern Colorado Plateau Knowing which key natural resources are found in the national parks, and whether they're stable or changing, helps decisionmakers make sound choices. The Northern Colorado Plateau Network is building that knowledge. After more than ten years of monitoring, we've learned a lot about park ecosystems, how they're changing, and what they may look like in the days to come. Find out what we’ve learned and how it’s being used to help managers plan for the future. Man stands in a stream, looking down at a handheld gauge. Trends in Water Quality of Cave Pools at Timpanogos Cave National Monument, 2008–2018 At Timpanogos Cave National Monument, water quality is monitored in two cave pools perched within a steep mountainside. Yet a recent analysis of measurements collected over a ten-year period revealed some surprising results about the influence of human activities on park waters. The findings will help park managers make decisions that protect park resources for enjoyment by future generations. Green pool surrounded by cave formations. Water Quality in the Northern Colorado Plateau Network: Water Years 2016–2018 Once a month, ecologists collect water samples at dozens of monitoring sites in and near ten National Park Service units across Utah and Colorado. This consistent, long-term monitoring helps alert managers to existing and potential problems. Find out the results for 2016-2018 in this brief from the Northern Colorado Plateau Network. A monitoring crew of three samples a clear river flowing over brown rock and sand Series: Inside Earth – NPS Cave & Karst News – Summer 2017 This newsletter is produced as a forum for information and idea exchanges between National Park Service units that contain caves and karst landscapes. It also provides a historical overview and keeps partners and other interested folks aware of cave and karst management activities. 4 rangers walk through shoe cleaning station 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: National Park Service Geodiversity Atlas The servicewide Geodiversity Atlas provides information on <a href="https://www.nps.gov/subjects/geology/geoheritage-conservation.htm">geoheritage</a> and <a href="https://www.nps.gov/subjects/geology/geodiversity.htm">geodiversity</a> resources and values all across the National Park System to support science-based management and education. The <a href="https://www.nps.gov/orgs/1088/index.htm">NPS Geologic Resources Division</a> and many parks work with National and International <a href="https://www.nps.gov/subjects/geology/park-geology.htm">geoconservation</a> communities to ensure that NPS abiotic resources are managed using the highest standards and best practices available. park scene mountains Series: NPS Environmental Achievement Awards Since 2002, the National Park Service (NPS) has awarded Environmental Achievement (EA) Awards to recognize staff and partners in the area of environmental preservation, protection and stewardship. A vehicle charges at an Electric Vehicle charging station at Thomas Edison National Historical Park Series: Cave Week—Featured Articles More than 20 parks across the US are participating in Cave Week via social media posts, cave tours, exhibits, school events, web pages and much more. The theme for Cave Week 2020 is, “Why do we go into caves?” This articles shares a few stories about why people (and bats) enter caves. person standing by underground lake in a cave 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 Blanket Cave National Youth Park—Activity Enjoy a fun activity and learn about caves even when you can't get out to a park. In this activity you will build your own cave and learn how to make it like a "real" natural cave. Find out about cave formations and wildlife, and how to be safe and care for caves. New "Blanket Cave National Youth Parks" are springing up all across America! Join the fun! cartoon drawing of a childs and a park ranger exploring a cave Monitoring From Space: Using Satellite Imagery to Measure Landscape Conditions on the Ground Scientists from the Northern Colorado Plateau Network travel thousands of miles each year to collect data on plants, soils, and water across network parks. But it would be impossible to cover every square inch of the Northern Colorado Plateau with boots on the ground. Instead, we simultaneously monitor the parks with boots in space—satellite data that provide information at a much broader scale. Satellite and Earth in space

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