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Scoping Report: Grand Staircase-Escalante National
CONTENTS 1 Introduction .............................................................................................................................................. 1 2 Scoping Process ....................................................................................................................................... 3 2.1 Purpose of Scoping ........................................................................................................................... 3 2.2 Scoping Outreach .............................................................................................................................. 3 2.2.1 Publication of the Notice of Intent ....................................................................................... 3 2.2.2 Other Outreach Methods ....................................................................................................... 3 2.3 Opportunities for Public Comment ................................................................................................ 3 2.4 Public Scoping Meetings .................................................................................................................. 4 2.5 Cooperating Agency Involvement ................................................................................................... 4 2.6 National Historic Preservation Act and Tribal Consultation ....................................................... 5 3 Submission Processing and Comment Coding .................................................................................... 5 -
Geologic Map of the Frisco Quadrangle, Summit County, Colorado
Geologic Map of the Frisco Quadrangle, Summit County, Colorado By Karl S. Kellogg, Paul J. Bartos, and Cindy L. Williams Pamphlet to accompany MISCELLANEOUS FIELD STUDIES MAP MF-2340 2002 U.S. Department of the Interior U.S. Geological Survey Geologic Map of the Frisco Quadrangle, Summit County, Colorado By Karl S. Kellogg, Paul J. Bartos, and Cindy L. Williams DESCRIPTION OF MAP UNITS af Artificial fill (recent)—Compacted and uncompacted rock fragments and finer material underlying roadbed and embankments along and adjacent to Interstate 70. Also includes material comprising Dillon Dam dt Dredge tailings (recent)—Unconsolidated, clast-supported deposits containing mostly well- rounded to subrounded, cobble- to boulder-size clasts derived from dredging of alluvium for gold along the Blue and Swan Rivers; similar dredge tailings along Gold Run Gulch are too small to show on map. Dredge tailings were mapped from 1974 air photos; most tailings have now been redistributed and leveled for commercial development Qal Alluvium (Holocene)—Unconsolidated clast-supported deposits containing silt- to boulder-size, moderately sorted to well-sorted clasts in modern floodplains; includes overbank deposits. Clasts are as long as 1 m in Blue River channel; clasts are larger in some side-stream channels. Larger clasts are moderately rounded to well rounded. Includes some wetland deposits in and adjacent to beaver ponds along Ryan Gulch. Maximum thickness unknown, but greater than 10 m in Blue River channel Qw Wetland deposits (Holocene)—Dark-brown to black, organic-rich sediment underlying wetland areas, commonly containing standing water and dense willow stands. Maximum thickness estimated to be about 15 m Qav Avalanche deposits (Holocene)—Unsorted, unstratified hummocky deposits at the distal ends of avalanche-prone hillside in Sec. -
Terrestrial Vertebrate Fauna of the Kaiparowits Basin
Great Basin Naturalist Volume 40 Number 4 Article 2 12-31-1980 Terrestrial vertebrate fauna of the Kaiparowits Basin N. Duane Atwood U.S. Forest Service, Provo, Utah Clyde L. Pritchett Brigham Young University Richard D. Porter U.S. Fish and Wildlife Service, Provo, Utah Benjamin W. Wood Brigham Young University Follow this and additional works at: https://scholarsarchive.byu.edu/gbn Recommended Citation Atwood, N. Duane; Pritchett, Clyde L.; Porter, Richard D.; and Wood, Benjamin W. (1980) "Terrestrial vertebrate fauna of the Kaiparowits Basin," Great Basin Naturalist: Vol. 40 : No. 4 , Article 2. Available at: https://scholarsarchive.byu.edu/gbn/vol40/iss4/2 This Article is brought to you for free and open access by the Western North American Naturalist Publications at BYU ScholarsArchive. It has been accepted for inclusion in Great Basin Naturalist by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. TERRESTRIAL VERTEBRATE FAUNA OF THE KAIPAROWITS BASIN N. Diiane Atwood', Clyde L. Pritchctt', Richard D. Porter', and Benjamin W. Wood' .\bstr^ct.- This report inehides data collected during an investigation by Brighani Young University personnel to 1976, as well as a literature from 1971 review. The fauna of the Kaiparowits Basin is represented by 7 species of salamander, toads, mnphihians (1 5 and 1 tree frog), 29 species of reptiles (1 turtle, 16 lizards, and 12 snakes), 183 species of birds (plus 2 hypothetical), and 74 species of mammals. Geographic distribution of the various species within the basin are discussed. Birds are categorized according to their population and seasonal status. -
The Science Behind Volcanoes
The Science Behind Volcanoes A volcano is an opening, or rupture, in a planet's surface or crust, which allows hot magma, volcanic ash and gases to escape from the magma chamber below the surface. Volcanoes are generally found where tectonic plates are diverging or converging. A mid-oceanic ridge, for example the Mid-Atlantic Ridge, has examples of volcanoes caused by divergent tectonic plates pulling apart; the Pacific Ring of Fire has examples of volcanoes caused by convergent tectonic plates coming together. By contrast, volcanoes are usually not created where two tectonic plates slide past one another. Volcanoes can also form where there is stretching and thinning of the Earth's crust in the interiors of plates, e.g., in the East African Rift, the Wells Gray-Clearwater volcanic field and the Rio Grande Rift in North America. This type of volcanism falls under the umbrella of "Plate hypothesis" volcanism. Volcanism away from plate boundaries has also been explained as mantle plumes. These so- called "hotspots", for example Hawaii, are postulated to arise from upwelling diapirs with magma from the core–mantle boundary, 3,000 km deep in the Earth. Erupting volcanoes can pose many hazards, not only in the immediate vicinity of the eruption. Volcanic ash can be a threat to aircraft, in particular those with jet engines where ash particles can be melted by the high operating temperature. Large eruptions can affect temperature as ash and droplets of sulfuric acid obscure the sun and cool the Earth's lower atmosphere or troposphere; however, they also absorb heat radiated up from the Earth, thereby warming the stratosphere. -
The High Deccan Duricrusts of India and Their Significance for the 'Laterite
The High Deccan duricrusts of India and their significance for the ‘laterite’ issue Cliff D Ollier1 and Hetu C Sheth2,∗ 1School of Earth and Geographical Sciences, The University of Western Australia, Nedlands, W.A. 6009, Australia. 2Department of Earth Sciences, Indian Institute of Technology (IIT) Bombay, Powai, Mumbai 400 076, India. ∗e-mail: [email protected] In the Deccan region of western India ferricrete duricrusts, usually described as laterites, cap some basalt summits east of the Western Ghats escarpment, basalts of the low-lying Konkan Plain to its west, as well as some sizeable isolated basalt plateaus rising from the Plain. The duricrusts are iron-cemented saprolite with vermiform hollows, but apart from that have little in common with the common descriptions of laterite. The classical laterite profile is not present. In particular there are no pisolitic concretions, no or minimal development of con- cretionary crust, and the pallid zone, commonly assumed to be typical of laterites, is absent. A relatively thin, non-indurated saprolite usually lies between the duricrust and fresh basalt. The duricrust resembles the classical laterite of Angadippuram in Kerala (southwestern India), but is much harder. The High Deccan duricrusts capping the basalt summits in the Western Ghats have been interpreted as residuals from a continuous (but now largely destroyed) laterite blan- ket that represents in situ transformation of the uppermost lavas, and thereby as marking the original top of the lava pile. But the unusual pattern of the duricrusts on the map and other evidence suggest instead that the duricrusts formed along a palaeoriver system, and are now in inverted relief. -
Halls Crossing
National Park Service Glen Canyon National Recreation Area U.S. Department of the Interior Rainbow Bridge National Monument Vol. 10, No. 1, 2014 The official newspaper PHOTO: Bob Moffitt Discover Glen Canyon Welcome! only 13% of Glen Canyon National Recreation overlooks. For spectacular views of the canyon Area. The impounded waters offer unparalleled country, those with 4-wheel drive vehicles Glen Canyon National Recreation Area’s varied water-based recreational opportunities where can visit less accessible areas of the park like expanses of land and water offer more than you can boat, swim, fish, water ski, camp or Alstrom Point or the Burr Trail, which begins you may think. As a unit of the National Park take a boat tour to Rainbow Bridge or Antelope in Glen Canyon and continues into Capitol Reef Service, Glen Canyon preserves and protects Canyon. National Park. over 1.2 million acres for scenic, scientific, and recreational values. Glen Canyon’s vast acreage You may be surprised to know that almost half With such recreational diversity and so many can be divided into three prominent land and of the park is managed as a proposed wilderness places to discover, visitors are often inspired to water areas, each of which offers distinct types area, meaning there is minimal development and return for further exploration. Whether it’s by of experiences for visitors from around the visitors can enjoy a more remote experience. boat, car, or foot, we invite you to experience all globe. that Glen Canyon National Recreation Area has The remainder of the park offers areas that to offer. -
Documented by Mcdonald and Harbaugh (1988) Was Used for This Sirrulation
srATE OF UTAH DEPAR'IMENI' OF NATURAL RESCURCES Tedmical Publication lb. 102 GROUND-WATER HYrROLCGY OF THE UPPER SE.VIER RIVER BASIN, SClJIH-cENrnAL UTAH, AID SIMULATION OF GROUND-WATER F'I.(W IN THE VALLEY-FILL AlJJIFER IN PAN:lliI'ICH VALLEY By Susan A. 'Ihiros am William C. Brothers Prepared by the Uni ted States Geological Survey in cooperation with the Utah Departnent of Natural Resources Division of water Rights 1993 Page Abstract 1 Introduction ••••••• I Purp:>se arrl soope 3 Methods of investigation . 3 Ackoowledgnents 3 Numberi~ system for hydrologic-data sites •••••••••••••• 3 Description of the study area ................................... 4 Geologic setti~ ........................................... 6 Climate .................................................... 8 vegetation . 9 Iarrluse ................................................... 10 Surface-water hydrology .................................... 10 Ground-water hydrology of oonsolidated rocks 11 Ground-water hydrology of the valley-fill aquifer in Panguitch Valley 13 Recharge 14 seepage fran streams 14 seepage fran caIla.1s ••••••••••••••••••••••••••••••••••••••••• 15 seepage fran unconsuned irrigation water ••••••••••••••••• 16 Infiltration of precipitation •••••••••••••••••••••••• 22 seepage fran consolidated rock ....................... 22 Movanent 22 Discharge 23 seepage to the Sevier River and canals ••••••••••••••••••• 23 E.Va]?CJtraIlSpiration . 24 Springs 25 wells 25 Slll:::surfare outfl~ •••••••••..•.••••••.•••••••••••••••••.••• 26 Water-level fluctuations 26 -
Factors Affecting Cottonwood Recruitment in Zion National Park
Factors Affecting Cottonwood Recruitment in Zion National Park Final Report to National Park Service CPCESU, Project number OSU 3 and OSU 4 Cooperative Agreement CA# H1200040002 By William J. Ripple1 and Robert L. Beschta College of Forestry Oregon State University, Corvallis, OR 97331 E-mail: [email protected] Phone: (541) 737-3956 Fax: (541) 737-3049 January 29, 2007 1 Corresponding author 1 Factors Affecting Cottonwood Recruitment in Zion National Park Abstract The strength of top-down forces in terrestrial food webs is highly debated as there are few examples illustrating the role of large mammalian carnivores in structuring biotic and abiotic systems. Based on the results of this study we hypothesize that an increase in human visitation within Zion Canyon of Zion National Park ultimately resulted in a catastrophic regime shift through pathways involving trophic cascades and abiotic environmental changes. Increases in human visitors in Zion canyon apparently reduced cougar (Puma concolor) densities, which subsequently led to higher mule deer (Odocoileus hemionus) densities, higher browsing intensities and reduced recruitment of riparian cottonwood trees (Populus fremontii), increased bank erosion, and reductions in both terrestrial and aquatic species abundance. These results may have broad implications with regard to our understanding of alternative ecosystem states where large carnivores have been removed or are being recovered. Key Words: predator, cottonwood, deer, stream, biodiversity, Leopold 2 Introduction Humans can have a major role in food web dynamics by displacing or extirpating top predators. Over a half century ago, the iconoclast Aldo Leopold was among the first to argue that elimination of large mammalian predators had strong top-down influences on ecosystems (Leopold et al., 1947). -
On the Glaciology of Edgegya and Barentsgya, Svalbard
On the glaciology of Edgegya and Barentsgya, Svalbard JULIAN A. DOWDESWELL and JONATHAN L. BAMBER Dowdeswell J. A. & Bamber. J. L. 1995: On the glaciology of Edgeoya and Barentsoya, Svalbard. Polar Research 14(2). 105-122. The ice masses on Edgeoya and Barentsdya are the least well known in Svalbard. The islands are 42-47% ice covered with the largest ice cap, Edge0yjokulen. 1365 km2 in area. The tidewater ice cliffs of eastern Edgedya are over 80 km long and produce small tabular icebergs. Several of the ice-cap outlet glaciers on Edgeoya and Barentsoya are known to surge, and different drainage basins within the ice caps behave as dynamically separate units. Terminus advances during surging have punctuated more general retreat from Little Ice Age moraines, probably linked to Twentieth Century climate warming and mass balance change. Airborne radio-echo sounding at 60 MHz along 340 km of flight track over the ice masses of Edgeoya and Barentsldya has provided ice thickness and elevation data. Ice is grounded below sea level to about 20 km inland from the tidewater terminus of Stonebreen. Ice thickens from <lo0 rn close to the margins, to about 250 m in the interior of Edgeeiyj~kulen.The maximum ice thickness measured on Barentsjokulen was 270111. Landsat MSS images of the two islands, calibrated to in-band reflectance values, allow synoptic examination of snowline position in late July/early August. Snow and bare glacier ice were identified. and images were digitally stretched and enhanced. The snowline was at about 300111 on the east side of Edgeoyjbkulen, and 50-100 m higher to the west. -
Energy and Mineral Resources, Grand Staircase
Circular 93 Utah Geological Survey Illustration Captions View figure: Circular 93 1., 2., 3., 4., 5., 6., 7., 8., 9., 10., 11., 12., 13., 14., 15. A Preliminary Assessment of Energy and Table of Contents 1.Preface Mineral Resources within the Grand 2.Summary 3.Introduction Staircase - Escalante National Monument 4.Geology 5.Kaiparowits Plateau coal Compiled by M. Lee Allison, State Geologist field 6.Oil and Gas Potential Contributors: 7.Tar-sand Resources Robert E. Blackett, Editor 8.Non-fuel Minerals and Thomas C. Chidsey Jr., Oil and Gas Mining David E. Tabet, Coal and Coal-Bed Gas 9.Acknowledgments Robert W. Gloyn, Minerals 10.References Charles E. Bishop, Tar-Sands January 1997 UTAH GEOLOGICAL SURVEY a division of UTAH DEPARTMENT OF NATURAL RESOURCES CONTENTS PREFACE SUMMARY INTRODUCTION Background Purpose and Scope GEOLOGY Regional Structure Permian through Jurassic Stratigraphy Cretaceous and Tertiary Stratigraphy THE KAIPAROWITS PLATEAU COAL FIELD History of Mining and Exploration Coal Resources Coal Resources on School and Institutional Trust Lands Sulfur Content of Kaiparowits Coal Coal-bed Gas Resources Further Coal Resource Assessments Needed OIL AND GAS POTENTIAL Source Rocks Potential Reservoirs Trapping Mechanisms Exploration and Development Carbon Dioxide Further Oil and Gas Resource Assessments Needed TAR-SAND RESOURCES OF THE CIRCLE CLIFFS AREA NON-FUEL MINERALS AND MINING Manganese Uranium-Vanadium Zirconium-Titanium Gold Copper, Lead and Zinc Industrial and Construction Materials Mining Activity Further Non-Fuel Mineral Resource Assessments Needed ACKNOWLEDGMENTS REFERENCES APPENDIX A: Presidential proclamation APPENDIX B: Summary of the coal resource of Kaiparowits Plateau and its value APPENDIX C: Summary of coal resources on School and Institutional Trust Lands APPENDIX D: Authorized Federal Oil and Gas Leases in the monument ILLUSTRATIONS Figure 1. -
Glen Canyon Unit, CRSP, Arizona and Utah
Contents Glen Canyon Unit ............................................................................................................................2 Project Location...................................................................................................................3 Historic Setting ....................................................................................................................4 Project Authorization .........................................................................................................8 Pre-Construction ................................................................................................................14 Construction.......................................................................................................................21 Project Benefits and Uses of Project Water.......................................................................31 Conclusion .........................................................................................................................36 Notes ..................................................................................................................................39 Bibliography ......................................................................................................................46 Index ..................................................................................................................................52 Glen Canyon Unit The Glen Canyon Unit, located along the Colorado River in north central -
From Decades to Epochs: Spanning the Gap Between Geodesy and Structural Geology of Active Mountain Belts
Journal of Structural Geology 31 (2009) 1409–1422 Contents lists available at ScienceDirect Journal of Structural Geology journal homepage: www.elsevier.com/locate/jsg From decades to epochs: Spanning the gap between geodesy and structural geology of active mountain belts Richard W. Allmendinger a,*, John P. Loveless b, Matthew E. Pritchard a, Brendan Meade b a Department of Earth & Atmospheric Sciences Cornell University, Ithaca, NY 14853-1504, United States b Department of Earth & Planetary Sciences, Harvard University, Cambridge, MA, United States article info abstract Article history: Geodetic data from the Global Navigation Satellite System (GNSS), and from satellite interferometric Received 25 March 2009 radar (InSAR) are revolutionizing how we look at instantaneous tectonic deformation, but the signifi- Received in revised form cance for long-term finite strain in orogenic belts is less clear. We review two different ways of analyzing 31 July 2009 geodetic data: velocity gradient fields from which one can extract strain, dilatation, and rotation rate, and Accepted 9 August 2009 elastic block modeling, which assumes that deformation is not continuous but occurs primarily on Available online 14 August 2009 networks of interconnected faults separating quasi-rigid blocks. These methods are complementary: velocity gradients are purely kinematic and yield information about regional deformation; the calcula- Keywords: Geodesy tion does not take into account either faults or rigid blocks but, where GNSS data are dense enough, GPS active fault zones and stable blocks emerge naturally in the solution. Block modeling integrates known Active tectonics structural geometry with idealized earthquake cycle models to predict slip rates on active faults. Future technological advances should overcome many of today’s uncertainties and provide rich new data to mine by providing denser, more uniform, and temporally continuous observations.