Geology and Ground-Water Resources of the Snake River Plain in Southeastern Idaho
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Teton - 17040204 Idaho 8 Digit Hydrologic Unit Profile February 2008
Dec Teton - 17040204 Idaho 8 Digit Hydrologic Unit Profile February 2008 Introduction The Teton 8-Digit Hydrologic Unit Code (HUC) subbasin contains 700,960 acres. Forty percent of the subbasin is in Teton County, twenty-seven percent is in Madison County and seven percent is in Fremont County, Idaho. Twenty-seven percent is in Teton County, Wyoming. Fifty-four percent of the basin is privately owned and forty-six percent is publicly owned. Forty-one percent of the basin is in shrub, rangeland, grass, pasture or hayland, thirty-five percent of the basin is in forest, water, wetlands, developed or barren, and twenty-four percent is cropland. Elevations range from 11,005 feet in the eastern part of the HUC to 4,814 feet at the basin outlet on the west. Conservation assistance is provided by one Conservation District in Wyoming, two Soil Conservation Districts and one Soil and Water Conservation District in Idaho, and one Resource Conservation and Development office. Profile Contents Introduction Progress/Status Physical Description Resource Concerns Landuse Map & Precipitation Map Census and Social Data Common Resource Area Footnotes/Bibliography Resource Settings Future Conservation Needs The United States Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, sex, religion, age, disability, political beliefs, sexual orientation, and marital or family status. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA’s TARGET Center at 202- 720-2600 (voice and TDD). -
Geologic Map of the Newdale Quadrangle, Fremont and Madison Counties, Idaho
IDAHO GEOLOGICAL SURVEY DIGITAL WEB MAP 122 MOSCOW-BOISE-POCATELLO WWW.IDAHOGEOLOGY.ORG EMBREE, PHILLIPS, AND WELHAN CORRELATION OF MAP UNITS EOLOGIC AP OF THE EWDALE UADRANGLE, REMONT AND ADISON OUNTIES, DAHO INTRODUCTION G M N Q F M C I Artificial Unit Alluvial Units Eolian Units Mass Wasting Volcanic The Newdale quadrangle lies on a dissected plateau locally known as the Units Units 1 2 3 Rexburg Bench. Geologic features of the Rexburg Bench are closely associ- Glenn F. Embree , William M. Phillips , and John A. Welhan Basalt Flows Rhyolitic Rock ated with water and agricultural resources. Near-surface geology of the m Qtfb Qtfg Qtfs Qtff Qls bench consists of the Huckleberry Ridge Tuff and three basalt units. The HOLOCENE 2011 Huckleberry Ridge is a highly permeable and jointed ash flow tuff. Most Qa Qc Qes high production irrigation water wells in the region draw from the Huckle- 10.0 ka berry Ridge aquifer. A dam constructed by the US Bureau of Reclamation in Qgh late the Teton River canyon failed catastrophically in 1976, largely due to Qel PLEISTOCENE Qbc Qbm Qgh uncontrolled seepage of reservoir water through joints and shear zones in Qbsp Qa the Huckleberry Ridge Tuff. Bedrock outcrops are rare in the Newdale ? Qa 1 Qgh quadrangle outside of the Teton River canyon because of widespread loess ~15 - 140 ka 126 ka Qa cover. The loess is the parent material for the rich soils of the region. QUATERNARY Qgh Qgh Qgh Qgh middle Qes Qbc PLEISTOCENE Qyh GEOLOGIC HISTORY Qel/Qbc Qyh 256 +/- 14 ka3 Qgh Qbsp Qel/Qbsp 780 ka The Huckleberry Ridge Tuff was erupted from the Henrys Fork caldera of the early Qyh Qyh Yellowstone Plateau at 2.059 Ma (Lanpere and others, 2002; Christiansen, Qbsp Qbm ? PLEISTOCENE Qel/Qyh 2001). -
TRAVERTINE-MARL DEPOSITS of the VALLEY and RIDGE PROVINCE of VIRGINIA - a PRELIMINARY REPORT David A
- Vol. 31 February 1985 No. 1 TRAVERTINE-MARL DEPOSITS OF THE VALLEY AND RIDGE PROVINCE OF VIRGINIA - A PRELIMINARY REPORT David A. Hubbard, Jr.1, William F. Gianninil and Michelle M. Lorah2 The travertine and marl deposits of Virginia's Valley and Ridge province are the result of precipitation of calcium carbonate from fresh water streams and springs. Travertine is white to light yellowish brown and has a massive or concretionary structure. Buildups of this material tend to form cascades or waterfalls along streams (Figure 1). Marl refers to white to dark yellowish brown, loose, earthy deposits of calcium carbonate (Figure 2). Deposits of these carbonate materials are related and have formed during the Quaternary period. This preliminary report is a compilation of some litei-ature and observations of these materials. A depositional model is proposed. These deposits have long been visited by man. Projectile points, pottery fragments, and firepits record the visitation of American Indians to Frederick and Augusta county sites. Thomas Jefferson (1825) wrote an account of the Falling Spring Falls from a visit prior to 1781. Aesthetic and economic considerations eontinue to attract interest in these deposits. 'Virginia Division of Mineral Resources, Charlot- Figure 1. Travertine waterfall and cascade series tesville, VA on Falling Springs Creek, Alleghany County, 2Department of Environmental Sciences, Univer- Virginia. Note man standing in center of left sity of Virginia, Charlottesville, VA margin. 2 VIRGINIA DIVISION OF MINERAL RESOURCES Vol. 31 Figure 2. An extensive marl deposit located in Figure 3. Rimstone dam form resulting from Frederick County, Virginia. Stream, in fore- precipitation of calcium carbonate in Mill Creek, ground, has incised and drained the deposit. -
Geologic Map of the Twin Falls 30 X 60 Minute Quadrangle, Idaho
Geologic Map of the Twin Falls 30 x 60 Minute Quadrangle, Idaho Compiled and Mapped by Kurt L. Othberg, John D. Kauffman, Virginia S. Gillerman, and Dean L. Garwood 2012 Idaho Geological Survey Third Floor, Morrill Hall University of Idaho Geologic Map 49 Moscow, Idaho 83843-3014 2012 Geologic Map of the Twin Falls 30 x 60 Minute Quadrangle, Idaho Compiled and Mapped by Kurt L. Othberg, John D. Kauffman, Virginia S. Gillerman, and Dean L. Garwood INTRODUCTION 43˚ 115˚ The geology in the 1:100,000-scale Twin Falls 30 x 23 13 18 7 8 25 60 minute quadrangle is based on field work conduct- ed by the authors from 2002 through 2005, previous 24 17 14 16 19 20 26 1:24,000-scale maps published by the Idaho Geological Survey, mapping by other researchers, and compilation 11 10 from previous work. Mapping sources are identified 9 15 12 6 in Figures 1 and 2. The geologic mapping was funded in part by the STATEMAP and EDMAP components 5 1 2 22 21 of the U.S. Geological Survey’s National Cooperative 4 3 42˚ 30' Geologic Mapping Program (Figure 1). We recognize 114˚ that small map units in the Snake River Canyon are dif- 1. Bonnichsen and Godchaux, 1995a 15. Kauffman and Othberg, 2005a ficult to identify at this map scale and we direct readers 2. Bonnichsen and Godchaux, 16. Kauffman and Othberg, 2005b to the 1:24,000-scale geologic maps shown in Figure 1. 1995b; Othberg and others, 2005 17. Kauffman and others, 2005a 3. -
STEEL BRIDGES of EASTERN IDAHO ITD Key #12479/Project #A012(479)
STEEL BRIDGES OF EASTERN IDAHO ITD Key #12479/Project #A012(479) Prepared for IDAHO TRANSPORTATION DEPARTMENT By PRESERVATION SOLUTIONS LLC May 2018 TABLE OF CONTENTS Acknowledgements ....................................................................................................................................... 1 Introduction & Certification of Results ........................................................................................................... 2 Project Description ........................................................................................................................................ 3 Methodology .................................................................................................................................................. 6 Glossary ........................................................................................................................................................ 9 Survey Findings .......................................................................................................................................... 11 Historic Contexts ......................................................................................................................................... 22 Selected Bibliography ................................................................................................................................. 58 Appendix A: NRHP Evaluation Criteria ...................................................................................................... -
Upper Snake Region Idaho Fishing & Boating Access Guide
UPPER SNAKE REGION IDAHO FISHING & BOATING ACCESS GUIDE 30 X r e v i Sand Creek Ponds X R P m Panhandle Small r a W k FREMONT Horseshoe P! e In-State Dubois re Lake RQ22 C s Jump Off Canyon Clearwater a Location m a Ashton Reservoir kC e P!X re C XX X Warm River Warm River ADA as Ora Bridge Salmon m RQ47 a C er CLARK S Ashton Riv a Lemon P! P Falls Stone Bridge Upper Snake Fall River n X d Lake Marysville C r X e e Magic Southwest South ¨¦§15 k Chester Wetland R Vernon Bridge Valley d XX -east P! Drummond Mud Lake WMA P P Camas Red Road Bridge Chester Dam Chester - North Ramp X PLamont RQ32 Egin P! Parker P! Fun Farm Bridge Lakes Saint Anthony Warm Slough Quayles Hamer X er P! Lake iv ton Riv R Te er n MONTANA Beaver Dick Teto ! Teton X P P! RQ33 P Felt X P Sugar City Newdale X Cartier Slough WMA 6000 W ¤£20 Terreton Rexburg Nature Park P! P 33 X Harrops Bridge X P! Tetonia RQ P !P X 33 Mud Lake Sage Junction Gem State WHA X RQ Rexburg Moody Creek W 400 N Erickson Dugway Rd MADISON Cache Bridge X Mud Lake WMA Market X TETON Lake X E 3500 Rd S X X - South Ramp P Thornton Horseshoe Bridge X X XW Buxton Rd P! Driggs P Menan Buttes Rd Menan Lorenzo tes Market Lake WMA P! Ba P! Dry Bed Rainey Bridge Roberts Dry X Bed P! Lewisville Twin Bridges RQ33 J EFFERSON X Bates Bridge P! X X RQ48 XX Rigby W 600 S P Byington Jim Moore Pond S Ririe Heise n P! Teton Creek ak X P! e Victor R ek S i e F v P! Cr S Fox Creek West e Ucon w llow n r ill o Wi Cr ake X X W eek R iv e West River Road RQ43 ¤£26 r Fox Creek East ¤£ 20 Ririe ¤£26 P! Iona Reservoir Trail Creek Pond P Lincoln RQ31 ¤£20 Conant Valley Idaho X Upper P !P P! ! Ammon th R Falls 49 d S Swan Valley Palisades ¨¦§15 49th Rd S d BONNEVILLE Lake R X E e Su n n o nys i B de P! R Irwin X d X Clowards Crossing Gem State ¤£26 Palisades Creek Grays Lake Outl P! Shelley Kepps Crossing X X k k BINGHAM e e ¤£ e e 91 r r C C Palisades Res. -
Caribou - Targhee National Forest 1405 Hollipark Drive Idaho Falls, Idaho 83401 Caribou - Targhee National Forest Forest Plan Monitoring and Evaluation Report
Targhee Monitoring Report: 1997-2004 May 2006 USDA Forest Service Intermountain Region Caribou - Targhee National Forest 1405 Hollipark Drive Idaho Falls, Idaho 83401 Caribou - Targhee National Forest Forest Plan Monitoring and Evaluation Report Section 2--Accomplishment of Goals and Objectives i Targhee Monitoring Report: 1997-2004 May 2006 Accomplishment of Objectives—Summary Table Table 1: Summary of the percent of each objective that the Targhee has accomplished. Details of how each objective has been met follow in the section “Accomplishment of Goals and Objectives”. % Accomplished as of January 2005 Resource Area Objective 25 50 75 100 PFC By 2000, complete a PFC assessment within a selected subsection. 100% By 2007, develop at least one fire management plan for a priority area within each of the seven 100% subsections. Fire By 2005, initiate a program to burn a minimum 2,000 acres annually for habitat improvement, fuels 100% management, and forest health, consistent with approved fire management plans. 0% Lands Remove utility facilities located in avoidance or exclusion areas as it becomes practical to do so. This will be amended to be a guideline By 2007, complete watershed improvement needs backlog in the Lemhi/Medicine Lodge, Big Hole 25% Mountains, and Caribou Range Mountains Subsections. By 2007, verify watershed improvement needs identified in the Teton Basin Study. 50% Fish, Water, and By 2007, inventory watershed improvement needs on the Centennial Mountains, Madison-Pitchstone 50% Riparian Plateaus, and Teton Range Subsections. By 1999, coordinate with ID & WY to reassess the health of native cutthroat trout populations within the Lemhi/Medicine Lodge, Centennial Mountains, Island Park, Madison-Pitchstone Plateaus, and Teton 100% Range Subsections. -
Case Study #2
Case Study #2 Teton Regional Land Trust: Protecting and Restoring Priority Habitats Project Summary: Protect and restore key habitats, including 27,000 acres of diverse and productive wetlands for water birds and other wildlife in the rapidly developing Teton River Basin. The land trust has protected nearly 9,000 acres of land through cooperative efforts with private landowners and has begun restoration efforts on over 4,000 acres in the upper Teton River watershed. Regional Setting: The Teton River, flanked by the Teton Range to the east and the Big Hole Mountains to the west, is a tributary of the Henrys Fork of the Snake River in eastern Idaho. Part of the Greater Yellowstone Ecosystem, the Teton River Basin encompasses an irreplaceable landscape that provides migratory corridors, breeding habitat and over-wintering lands for upon this wetland/upland complex, including a number of thousands of waterbirds. Development pressure driven by waterfowl and shorebirds identified as priorities in national demand for second homes in this spectacularly scenic area bird conservation plans. The wetlands and nearby grain fields threatens traditional land uses that have sustained high quality provide essential staging habitat for the migratory Rocky wetlands along with local ranching and agricultural communities. Mountain population of greater sandhill cranes. The river corridor provides regionally significant wintering habitat for hundreds of Land Trust Mission: The Teton Regional Land Trust conserves trumpeter swans. Nesting long-billed curlews are found here in agricultural and natural lands and encourages land stewardship greater density than anywhere else in their range. The river itself in the Upper Snake River valley for the benefit of today's is home to a self-sustaining population of the sensitive communities and as a legacy for future generations. -
County Comprehensive Plan
JEROME COUNTY COMPREHENSIVE PLAN TABLE OF CONTENTS Revised 11/13/2015 Section Page I. Introduction ...................................................................................................................................1 A. Setting ................................................................................................................................1 B. Purpose and Scope .............................................................................................................2 C. Private Property Rights ......................................................................................................4 D. Plan Structure ....................................................................................................................6 E. Plan Adoption and Review ................................................................................................8 II. Population ....................................................................................................................................9 A. Existing Conditions ...........................................................................................................9 1. 1990 Census Characteristics ...................................................................................10 a. Geographic Distribution ..............................................................................10 b. Age ..............................................................................................................10 c. Race and Hispanic Origin ...........................................................................12 -
The Settlement of Teton Valley, Idaho-Wyoming
Brigham Young University BYU ScholarsArchive Theses and Dissertations 1974 The Settlement of Teton Valley, Idaho-Wyoming David Brooks Green Brigham Young University - Provo Follow this and additional works at: https://scholarsarchive.byu.edu/etd Part of the History Commons, Mormon Studies Commons, and the Sociology Commons BYU ScholarsArchive Citation Green, David Brooks, "The Settlement of Teton Valley, Idaho-Wyoming" (1974). Theses and Dissertations. 4727. https://scholarsarchive.byu.edu/etd/4727 This Thesis is brought to you for free and open access by BYU ScholarsArchive. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. THE sfttiinhsettlementT OF TETtemonTETONON VALLEY IDAHO WYOMING A thesis presented to the department of geography brighamB r ighambigham young university in partial fulfillmentfulfillynent of the requirements for the degree master of science by D brooks green this thesis by D brooks green is accepted in its present form by the department of geography of brigham young university as satisfying the thesis requirement for the degree of master of science 1 1 L waw& eiaelaLIA X 1 1 X y richardurfaH jackson cammicommiconmiiuteewae3e chairman 1 L AAAy L 1 1 i yuj alan H grey committecommittee meermepioer te aa7aaa roberi 1 lilILL a on depai6twnt rronaron 11 TABLE OF CONTENTS page PREFACE 0 0 0 0 0 0 viii LIST OF TABLES v LIST OF illustrations vi chapter I1 introduction -
Old West Meets New West BOARD of DIRECTORS from Our President Kim Keeley, President Chuck Iossi, Vice President I Learned to Fish from My Grandmother
water linesSPRING/SUMMER 2012 Old West Meets New West BOARD OF DIRECTORS From Our President Kim Keeley, President Chuck Iossi, Vice President I learned to fish from my grandmother. She taught me to cast and tie Geordie Gillett, Treasurer knots, but the real learning came from tagging along with her when she Richard Berg, Secretary fished. The only rule was no talking. So I learned to observe. I watched my Jon Fenn grandmother, watched the creek, watched fish, found snakes, made little Kristie Grigg boats out of rosehips, and sometimes I just watched the inside of my Derek Hutton eyelids. It wasn’t until years later that I realized all the skills I had learned David Jennings on those too few fishing outings: observation, Tim Mason respect, creativity, and appreciation. Mitch Prissel Crucial to our River stewardship is very similar. Over the past KEY PARTNERS success has been twelve years FTR has methodically assessed the Bonneville Environmental Foundation health of our watershed using cutting edge technol- willing participation Idaho Department of Fish and Game ogy as well as anecdotal evidence imparted to us by from landowners, Idaho Department of Environmental longtime residents. We gather information and Quality donors, and Wyoming Game and Fish create solutions to the issues we encounter, guided volunteers, and the U.S. Forest Service, Caribou-Targhee by both scientific reason and social evidence. Crucial National Forest to our success has been willing participation from gift of perspective landowners, donors, and volunteers, and the gift of from the old timers. STAFF perspective from the old timers. Quincy Liby, Outreach Coordinator Mike Lien, Restoration Director We have a myriad of challenges ahead of us. -
Stromatolites of the Belt Series in Glacier National Park and Vicinity, Montana
Stromatolites of the Belt Series in Glacier National Park and Vicinity, Montana By RICHARD REZAK SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 294-D Descriptions of eight zones of Precambrian stromatolites, including two new forms, based on a revised method of classification UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1957 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. CONTENTS Page Abstract 127 S tratigraphy—Continued Introduction 127 Stromatolite zones—Continued Previous investigations 127 Ravalli group—Continued Page Present investigation 127 Grinnell argillite 136 Area of investigation 128 Collenia undosa zone 1 136 Acknowledgments 129 Piegan group 137 Classification of stromatolites 129 Siyeh limestone 137 General 129 Collenia symmetrica zone 1 137 Previous classifications 130 Conophyton zone 1 138 Pres* ent classification 131 Collenia multiflabella zone 138 Generic distinction 131 Missoula group 139 Specific characteristics 131 Collenia undosa zone 2 139 Gross form of colony 131 zone 2 139 Nature of the laminae 132 Collenia symmetrica Size of colony 132 Conophyton zone 2 140 Types 132 Ecology 141 Key to the identification of stromatolites in the Belt Modern environments 141 series 132 Origin of stromatolites 146 Descriptions of genera and species 132 Paleoecology 147 Genus Cryptozoon Hall 132 Collenia frequens zone 147 Genus Collenia Walcott 133 Newlandia lamellosa 147 Genus Newlandia Walcott 134 Collenia undosa zones 147 Genus Conophyton Maslov 135 Collenia symmetrica zones 148 Stratigraphy 135 zones 148 General 135 Conophyton Stromatolite zones 136 Collenia multiflabella zone 148 Ravalli group 136 Conclusions 149 Altyn limestone 136 Selected bibliography 149 Collenia frequens zone 136 Index 153 ILLUSTRATIONS [Plates 19-24 follow page 154] Page PLATE 18.