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Hexagonal Fracture Patterns on Navajo Sandstone Crossbeds at Yellow Knolls, Washington County
Hexagonal Fracture Patterns On Navajo Sandstone Crossbeds At Yellow Knolls, Washington County David B. Loope Earth & Atmospheric Sciences, University of Nebraska Lincoln, NE 68588-0340 [email protected] Utah Geosites 2019 Utah Geological Association Publication 48 M. Milligan, R.F. Biek, P. Inkenbrandt, and P. Nielsen, editors Cover Image: Southward-sloping crossbeds in the Navajo Sandstone at Yellow Knolls. M. Milligan, R.F. Biek, P. Inkenbrandt, and P. Nielsen, editors 2019 Utah Geological Association Publication 48 Presidents Message I have had the pleasure of working with many diff erent geologists from all around the world. As I have traveled around Utah for work and pleasure, many times I have observed vehicles parked alongside the road with many people climbing around an outcrop or walking up a trail in a canyon. Whether these people are from Utah or from another state or country, they all are quick to mention to me how wonderful our geology is here in Utah. Utah Geosites 2019 Utah is at the junction of several diff erent geological provinces. We have the Basin and Range to the west and the Central Utah Utah Geological Association Publication 48 Hingeline and Th rust Belt down the middle. Th e Uinta Mountains M. Milligan, R.F. Biek, P. Inkenbrandt, and P. Nielsen, editors have outcrops of some of the oldest sedimentary rock in Utah. Utah also has its share of young cinder cones and basaltic lava Utah Geosites showcases some of Utah’s spectacular geology, both fl ows, and ancient laccoliths, stratovolcanoes, and plutonic rocks. little-known localities and sites seen by visitors to Utah’s many Th e general public comes to Utah to experience our wonderful national and state parks and monuments. -
Utah Lake Watch Report 2008
Utah Lake Watch Report 2008 Utah State University Water Quality Extension Prepared by: Eric Peterson Introduction Utah Lake Watch (ULW) is a statewide monitoring program which enlists the help of volun teers to ga in ins ig ht on the h ealth of Ut ah’ s l ak es and reservoi rs. Th ese d at a help the Utah Division of Water Quality in their lake protection programs, and provide lake managers with a better picture of the health of their lake. Major objectives of the program include: • acquiring baseline data for Utah’s lakes and reservoirs; • providing education to the citizens of the state on the importance of healthy lakes, how lakes function, and how we monitor lakes; and • demonstrating the effectiveness of citizen monitoring in collecting water quality data which can be used to better manage and protect our lakes and reservoirs. To meet these objectives, Utah Lake Watch participants are trained to measure the transparency of a particular lake or reservoir on a regular basis from May until September. The participants record these readings and weather observations on a data sheet, and return the data to USU Water Quality Extension at the end of the season. USU Water Quality Extension compiles the raw data and delivers it electronically to the Utah Division of Water Quality. In addition, they summarize the results for each lake and return these summaries to the citizen volunteers. All of these results and interpretations are contained in this annual report. Participants measure transparency using a Secchi disk. The measurement itself is very easy; the Secchi disk, which is a white and black weighted disk attached to a line, is lowered into the water until it is no longer visible. -
Vendor List by City
Revised 2/20/14 Vendor List by City Antimony Otter Creek State Park 400 East SR 22 435-624-3268 Beaver Beaver Sport & Pawn 91 N Main 435-438-2100 Blanding Edge of the Cedars/Goosenecks State Parks 660 West 400 North 435-678-2238 Bluffdale Maverik 14416 S Camp Williams Rd 801-446-1180 Boulder Anasazi State Park 46 North Hwy 12 435-335-7308 Brian Head Brian Head Sports Inc 269 South Village Way 435-677-2014 Thunder Mountain Motorsports 539 North Highway 143 435-677-2288 1 Revised 2/20/14 Cannonville Kodachrome State Park 105 South Paria Lane 435-679-8562 Cedar City D&P Performance 110 East Center 435-586-5172 Frontier Homestead State Park 635 North Main 435-586-9290 Maverik 809 W 200 N 435-586-4737 Maverik 204 S Main 435-586-4717 Maverik 444 W Hwy 91 435-867-1187 Maverik 220 N Airport Road 435-867-8715 Ron’s Sporting Goods 138 S Main 435-586-9901 Triple S 151 S Main 435-865-0100 Clifton CO Maverik 3249 F Road 970-434-3887 2 Revised 2/20/14 Cortez CO Mesa Verde Motorsports 2120 S Broadway 970-565-9322 Delta Maverik 44 N US Hwy 6 Dolores Colorado Lone Mesa State Park 1321 Railroad Ave 970-882-2213 Duchesne Starvation State Park Old Hwy 40 435-738-2326 Duck Creek Loose Wheels Service Inc. 55 Movie Ranch Road 435-682-2526 Eden AMP Recreation 2429 N Hwy 158 801-614-0500 Maverik 5100 E 2500 N 801-745-3800 Ephraim Maverik 89 N Main 435-283-6057 3 Revised 2/20/14 Escalante Escalante State Park 710 North Reservoir Road 435-826-4466 Evanston Maverik 350 Front Street 307-789-1342 Maverik 535 County Rd 307-789-7182 Morgan Valley Polaris 1624 Harrison -
Milebymile.Com Personal Road Trip Guide Utah Byway Highway # "Flaming Gorge-Uintas Scenic Byway"
MileByMile.com Personal Road Trip Guide Utah Byway Highway # "Flaming Gorge-Uintas Scenic Byway" Miles ITEM SUMMARY 0.0 End of Byway Manila, Utah, a town located in Daggett County, Utah, close to the border of Utah with Wyoming. This is where the Flaming Gorge-Uintas Scenic Byway ends. 3.2 Valley Ranch A Valley Ranch south of Manila, Utah 6.0 State Route #218 State Route #218, Sheep Creek Drive, Sheep Creek Canyon, located in Ashley National Forest, Utah 8.1 Road to Flaming Gorge Road to Flaming Gorge, Sheep Creek, 11.3 State Route #93 State Route #93, Green Lake, 14.0 Flaming Gorge National Flaming Gorge National Recreation Area, State Route #218 / 221, Recreation Area Sheep Creek Canyon, located within Ashley National Forest, Utah 16.5 State Route #539 State Route #539, Ashley National Forest, Utah 24.5 Road Access Road Access to Flaming Gorge Lake, Green Lakes, Canyon Rim Campground, in Flaming Gorge National Recreation Area, within the Ashley National Forest, Utah 27.1 Flaming Gorge National Road to Flaming Gorge National Recreation Area / Flaming Gorge Recreation Area Reservoir, Utah 28.0 Junction Junction of United States Highway #191 with State Highway #44, 44.8 Border of Utah with Border of Utah with Wyoming/End of Part of Byway Flaming Wyoming/End of Part of Gorge-Uintas Scenic Byway, Utah This is where the part of the byway Byway that runs on United States Highway #191 ends, while the byway extends Northwest on Utah Highway #44 till Manila, Utah, a small town located in Daeggett County, Utah 45.4 Flaming Gorge National Flaming -
Sheeting Joints and Polygonal Patterns in the Navajo Sandstone, Southern Utah: Controlled by Rock Fabric, Tectonic Joints, Buckling, and Gullying David B
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Papers in the Earth and Atmospheric Sciences Earth and Atmospheric Sciences, Department of 2018 Sheeting joints and polygonal patterns in the Navajo Sandstone, southern Utah: Controlled by rock fabric, tectonic joints, buckling, and gullying David B. Loope University of Nebraska, Lincoln, [email protected] Caroline M. Burberry University of Nebraska - Lincoln, [email protected] Follow this and additional works at: http://digitalcommons.unl.edu/geosciencefacpub Part of the Earth Sciences Commons Loope, David B. and Burberry, Caroline M., "Sheeting joints and polygonal patterns in the Navajo Sandstone, southern Utah: Controlled by rock fabric, tectonic joints, buckling, and gullying" (2018). Papers in the Earth and Atmospheric Sciences. 519. http://digitalcommons.unl.edu/geosciencefacpub/519 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Papers in the Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Research Paper GEOSPHERE Sheeting joints and polygonal patterns in the Navajo Sandstone, southern Utah: Controlled by rock fabric, tectonic joints, buckling, GEOSPHERE, v. 14, no. 4 and gullying https://doi.org/10.1130/GES01614.1 David B. Loope and Caroline M. Burberry 14 figures; 1 table Department of Earth and Atmospheric Sciences, University of Nebraska, -
Zion National Park Tour from Las Vegas (Zion)
ZION NATIONAL PARK TOUR FROM LAS VEGAS (ZION) Zion National Park, just 163 miles from Las Vegas is located near Springdale, Utah, covers 229 square miles (590 km2) at the junction of the Colorado Plateau, Great Basin, and Mojave Desert regions, the park's unique geography and variety of life zones allow for unusual plant and animal diversity. The primary feature of the park is Zion Canyon, which is 15 miles (24 km) long and up to half a mile (800 m) deep cut through the sandstone by the North Fork of the Virgin River. Common daytime animals include mule deer, rock squirrels, pinyon jays, as well as whiptail and collared lizards. Desert cottontails, jackrabbits, and Merriam's kangaroo rats come out at night. Cougars, coyotes, gray foxes, and ring-tail cats are the top predators. The park is home to 289 bird, 79 mammal, 28 reptile, 7 fish, and 6 amphibian species. Golden eagles, red-tailed hawks, peregrine falcons, and white- throated swifts can be seen in the area. California condors and bighorn sheep were reintroduced in the 1990s. Nineteen species of bat also live in the area. Notable geographical features of the park which leave visitors in awe include the Virgin River Narrows, Emerald Pools, Hidden Canyon, Angels Landing, The Great White Throne, Checkerboard Mesa, The Three Patriarchs, and Kolob Arch. The geology of the Zion and Kolob canyons area includes nine formations that together represent 150 million years of mostly Mesozoic-aged sedimentation. This entire area was truly created by the hand of God. ZION NATIONAL PARK TOUR FROM LAS VEGAS Artists and photographers have been drawn to Zion for decades in an effort to capture its infinite variety of moods. -
Hexagonal Fracture Patterns on Navajo Sandstone Crossbeds at Yellow Knolls, Washington County
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Earth and Atmospheric Sciences, Department Papers in the Earth and Atmospheric Sciences of 2019 Hexagonal Fracture Patterns On Navajo Sandstone Crossbeds At Yellow Knolls, Washington County David Loope Follow this and additional works at: https://digitalcommons.unl.edu/geosciencefacpub Part of the Earth Sciences Commons This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Papers in the Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Hexagonal Fracture Patterns On Navajo Sandstone Crossbeds At Yellow Knolls, Washington County David B. Loope Earth & Atmospheric Sciences, University of Nebraska Lincoln, NE 68588-0340 [email protected] Utah Geosites 2019 Utah Geological Association Publication 48 M. Milligan, R.F. Biek, P. Inkenbrandt, and P. Nielsen, editors Cover Image: Southward-sloping crossbeds in the Navajo Sandstone at Yellow Knolls. M. Milligan, R.F. Biek, P. Inkenbrandt, and P. Nielsen, editors 2019 Utah Geological Association Publication 48 Presidents Message I have had the pleasure of working with many diff erent geologists from all around the world. As I have traveled around Utah for work and pleasure, many times I have observed vehicles parked alongside the road with many people climbing around an outcrop or walking up a trail in a canyon. Whether these people are from Utah or from another state or country, they all are quick to mention to me how wonderful our geology is here in Utah. -
Utah State Parks Are Open Every Day Except for Thanksgiving and Christmas
PLAN YOUR TRIP Utah State Parks are open every day except for Thanksgiving and Christmas. For individual park hours visit our website stateparks.utah.gov. Full UTAH STATE PARK LOCATIONS / PARK RESERVATIONS 1 Anasazi AMENITIES Secure a campsite, pavilion, group area, or boat slip in advance by 2 Antelope Island calling 800-322-3770 8 a.m.–5 p.m. Monday through Friday, or visit 3 Bear Lake stateparks.utah.gov. # Center Visitor / Req. Fee Camping / Group Camping RV Sites Water Hookups—Partial Picnicking / Showers Restrooms Teepees / Yurts / Cabins / Fishing Boating / Biking Hiking Vehicles Off-Highway Golf / Zipline / Archery 84 Cache 3 State Parks 4 Camp Floyd Logan 1. Anasazi F-V R Reservations are always recommended. Individual campsite reservations 23 State Capitol Rivers 5 Coral Pink Sand Dunes Golden Spike Randolph N.H.S. Lakes 2. Antelope Island F-V C-G R-S B H-B may be made up to four months in advance and no fewer than two days Cities Box Elder Wasatch-Cashe N.F. 6 Dead Horse Point G Brigham City Rich 3. Bear Lake F-V C-G P-F R-S C B-F H-B before desired arrival date. Up to three individual campsite reservations per r e Interstate Highway 7 Deer Creek a 4. Camp Floyd Stagecoach Inn Museum F R t customer are permitted at most state parks. 43 U.S. Highway North S 8 East Canyon a 5. Coral Pink Sand Dunes F-V C-G P R-S H l Weber Morgan State Highway t PARK PASSES Ogden 9 Echo L 6. -
Erosion, Weathering, and Change Activity Guide
National Park Service U.S. Department of the Interior Zion National Park Weathering, Erosion, and Change Geologic Events in Zion PHOTO CREDIT Contents Introduction 2 Core Connections 2 Background 2 Activities Earth’s Power Punches 4 Rock On, Zion 5 It Happened Here! 6 Glossary 8 References 9 Introduction This guide contains background information about how weathering, erosion, and other geologic processes such as volcanoes continually shape the landscape, and directions for three activities that will help students better understand how these processes are at work in Utah. This guide is specifically designed for fifth grade classrooms, but the activities can be NPS modified for students at other levels. Theme of deposition (sedimentation), lithification, The Earth’s surface is a dynamic system that is uplift, weathering, erosion, tectonics, and constantly changing due to weathering, volcanic activity make the park a showcase for erosion, floods, earthquakes, volcanoes, and changing landscapes. other geologic events. Deposition (Sedimentation) Focus Zion National Park was a relatively flat basin The activities focus on relationship between near sea level 275 million years ago, near the NPS/MARC NEIDIG geologic processes such as weathering and coast of Pangaea, the land area believed to erosion and changes on the Earth’s surface. have once connected nearly all of the earth’s landmasses together. As sands, gravels, and Activities muds eroded from surrounding mountains, Earth’s Power Punches streams carried these materials into the Students view a presentation of digital im- basin and deposited them in layers. The sheer ages showing the forces that shape the Earth’s weight of these accumulated layers caused surface. -
Utah Scenic Byways Guide
Utah is the place where prehistory intersects with the enduring spirit of the Old West. Wild, adventure-rich places cradle vibrant urban centers. With interstates and airplanes, the world can feel pretty small. On Utah’s designated scenic byways, the world feels grand; its horizons seem infinite. As you drive through Utah, you’ll inevitably encounter many of the state’s scenic byways. In total, Utah’s distinct topography provides the surface for 27 scenic byways, which add up to hundreds of miles of vivid travel experiences wherein the road trip is as memorable as the destination. Utah’s All-American Road: Scenic Byway 12 headlines the network of top roads thanks to landscapes and heritage unlike anywhere else in the nation. All of Utah’s scenic byways are explorative journeys filled with trailheads, scenic overlooks, museums, local flavors and vibrant communities where you can stop for the night or hook up your RV. Not sure where to start? In the following pages, you’ll discover monumental upheavals of exposed rock strata among multiple national and state parks along the All-American Road (pg. 4); dense concentrations of fossils along Dinosaur Diamond (pg. 8); and the blazing red cliffs and deep blue waters of Flaming Gorge–Uintas (pg. 12) — and that’s just in the first three highlighted byways. Your journey continues down two dozen additional byways, arranged north to south. Best of all, these byways access an outdoor adventureland you can hike, fish, bike, raft, climb and explore from sunup to sundown — then stay up to welcome the return of the Milky Way. -
The Colorado Plateau
The Colorado Plateau An OUGS Severnside Field Trip 2015 The Colorado Plateau 2015 Introduction This was to be another Severnside trip, but one with a new organiser! Janet Hiscott and Tom Sharpe had devised the idea for this trip when talking about what he would do in his retirement from the Museum of Wales. The large group of 27 members that collected in Denver at the end of September 2015 were the beneficiaries of this chat. We were all eager to explore the Colorado Plateau with Janet and Tom to guide us. The Colorado Plateau is an area between the Rockies and the Basin and Range Province and extends through parts of 4 states, Utah, Colorado, New Mexico and Arizona. (Fig. 1) It contains some of the most famous and most visited National Parks of the USA and we were here for 17 days to be introduced to the geology, paleontology and human interaction with and exploitation of the region. The Rockies have been through several cycles of uplift and erosion since the Precambrian, the most recent period of uplift started 5Ma ago and the area has seen a change in elevation of 5000ft. There was associated volcanic activity, building volcanoes and causing a redistribution of metals by heated fluids. The latter having been exploited by man in the Colorado Mineral Belt. The debris eroded from the Rockies during these successive periods of upift was deposited in the plains surrounding them. These sediments, and marine deposits from a period of inundation by an inland sea, form the level beds that comprise the Colorado plateau. -
Changing Landscapes Fifth Grade Pre- and Post-Visit Activity Guide
National Park Service U.S. Department of the Interior Zion National Park Utah Changing Landscapes Fifth Grade Pre- and Post-Visit Activity Guide NPS/MARC NEIDIG Changing Landscapes Fifth Grade Pre- and Post-Visit Activity Guide Zion National Park Springdale, Utah 84767 Contents Introduction 1 Core Connections 1 Background 1 Pre-Visit Activities 3 Earth’s Power Punches 3 Rock On Zion! 4 Then and Now 6 Post-Visit Activities 8 Map Minds 8 It Happened Here! 9 Future Forecasters 11 Glossary 12 References 14 Introduction Background Theme Zion National Park is located along the edge The Earth’s surface is a dynamic system that is of a region called the Colorado Plateau. Uplift, constantly changing due to weathering, tilting, and the erosion of rock layers formed erosion, earthquakes, volcanoes, and uplift. a feature called the Grand Staircase, a series of colorful cliffs stretching between Bryce Focus Canyon, Zion, and the Grand Canyon. The activities focus on relationship between NPS PHOTO geologic processes and changes on the Earth’s Zion has spectacular geology. The arid climate surface. and sparse vegetation expose bare rock and reveal the park’s geologic history. Evidence Pre-Visit Activities of deposition (sedimentation), lithification, 1. Earth’s Power Punches – Students view a uplift, weathering, erosion, tectonics, and presentation of digital images showing the volcanic activity make the park a showcase for forces that shape the Earth’s surface. Then changing landscapes. students view images from Zion and deter- mine which geologic forces have contributed Deposition (Sedimentation) to the landscapes shown. Finally, students Zion National Park was a relatively flat basin discuss which landscapes were formed slowly near sea level 275 million years ago, near the NPS PHOTO and which were formed quickly.