DOCSLIB.ORG

Geologic Map of the Newdale Quadrangle, Fremont and Madison Counties, Idaho

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
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). Well logs show that the tuff flowed over irregular topography ? Qyh 909 +/- 13 ka3 Qbsp Qbc containing at least one large lake, west-flowing streams, basaltic lava flows, 2 Qyh ? 2.059 +/- 0.004 Ma 2.60 Ma and rhyolitic rocks. Large scale gravity sliding and deformation occurred Qyh Qyh Tb Qbsp Qbc within the lake and stream deposits shortly after the Huckleberry Ridge Ts PLIOCENE TERTIARY Qyh ? Qbc Qyh ignimbrite flowed over them (Geissman and others, 2010; Embree and ? Qyh Hoggan, 1999). A minimum of 1 km (0.6 mi) of horizontal movement Qbsp caused significant deformation in the still partially fluid tuff sheet. Unusu- 1 Range of OSL ages, Phillips and others, 2009, Pierce and others, 2003. Qyh ally numerous open joints, shear zones, large scale >150 m (>490 ft) ampli- 2 Sanidine 40Ar/39Ar age, Lanphere and others, 2002. Qbsp Qyh Qyh tude overturned asymmetric antiforms, and a tectonically denuded valley 3 40Ar/39Ar ages, D. Champion, oral communication, 2010. Qyh Qyh (Hog Hollow) were created prior to complete welding and devitrification of Geologic time scale from Walker, J.D. and Geissman, J.W. compilers, 2009, the ignimbrite. Geologic Time Scale: Geological Society of America, doi: Qyh Qyh Qyh Qyh 10.1130/2009. CTS004R2C. Qbsp The basalt of Moody Creek was erupted from a presently obscured vent in Qbsp Qbsp Qyh Qyh the adjacent Moody quadrangle to the south. Following ancestral Moody Qgh Qbc Qyh Creek and flowing around uplands of Huckleberry Ridge Tuff, at least 3 lava Qyh Qel/Qyh flows were emplaced. Pillow basalts at the base of the flows suggest that Qyh they encountered the Teton River, diverting or blocking it temporarily at the Qyh mouth of the Teton Canyon (Jordan and others, 2010b). The basalt of Moody Qa Creek has not been dated. It has reverse magnetic polarity, indicating that it Qtfs is probably older than 780 ka. Sand (Holocene)—Sand and pebbly sand; forms parts of pendant bars in SYMBOLS Qyh Qyh canyon and sheet-like deposits at canyon mouth and farther downstream; Qyh The basalt of Snake River Plain is tentatively correlated with flows erupted downstream deposits derived from scour of sandy road fills, irrigation Contact: dashed where approximately located. Qel/Qbc Qbsp Qyh Qyh from a low shield volcano in the Ashton quadrangle at 909 ka (D. Cham- canals, and terrace scarps; canyon deposits as thick as 3 m (10 m); deposits Qyh pion, oral communication, 2010). The basalt flowed south down the downstream <1 m (3.3 ft) thick. Normal fault: ball and bar on downthrown side; dashed where Qel/Qyh Qyh Henrys Fork drainage. It has reverse magnetic polarity. approximately located; dotted where concealed. Qtff Fine sand and silt (Holocene)—Fine sand, silt, and clay in deposits; <20 cm (8 Qel/Qbsp The basalt of Chester occupies an abandoned stream valley between the in) thick on flood plains, in depressions, and in fields surround by dikes, Lateral faults; arrows indicate direction of motion; dashed where Qyh highlands of the Huckleberry Ridge and the lowlands of the Snake River roads or irrigation canals. Found where slack water was present during approximately located; dotted where concealed. Qyh Plain. Petrologically similar to the basalt of Moody Creek, the basalt of flooding. Mapped where thicker than 5 cm (2 in). Sources were compacted Chester has an age of about 256 ka (D. Champion, 2010) and normal loess core of the Teton Dam, eolian sand, fine-grained artificial fills, and the Qbc Qyh magnetic polarity. fine fraction of gravelly embankments. Fold axis; arrow indicates direction of plunge. Qel/Qbsp Qbsp Qyh Downdropping of the upper Snake River Plain and the Teton Basin relative Qls Landslide deposits (Holocene)—Landslides resulting from the rapid drawdown Overturned antiform; dashed where approximately located; Qyh Qyh Qel/Ts to the adjacent Big Hole Mountains caused the Rexburg Bench to be of the Teton Reservoir after the failure of Teton Dam (see Figure 1). Majority dotted where concealed. Qa incised by the Teton River. Most of the incision was accomplished between of landslides are translational earth slides with failure surfaces near contact Qbsp Ts Antiform; dashed where approximately located; dotted where Qbsp eruption of the Huckleberry Ridge Tuff and the eruption of basalt of Moody between overburden (loess, colluvium, and/or slope wash) and underlying concealed. Creek. Huckleberry Ridge Tuff. Thickness from 0.3-0.6 m (1-2 ft) to ~3 m (10 ft.) Ts 10P01 Qyh Where overburden was >3m (10 ft), landslides began as shallow rotational 60 Strike and dip of bedding. During the glacial periods of the middle and late Pleistocene, a large ice 25 slumps 6-7.5 m (20-25 ft) thick, then evolved into earth flows and debris Qbc Qyh sheet and numerous alpine valley glaciers occupied much of the headwa- flows. Some flows reached out into the river and caused temporary Strike and dip of vertical bedding. Qa Qyh Qyh ters of Henrys Fork and Teton River in the Yellowstone and Grand Teton damming or changed stream configurations. Rock falls and slides involving Qbsp Qyh areas. Outwash streams from these glaciers deposited thick fills of gravel tuff bedrock also occurred. Landslides of all types are more numerous on 22 Strike and dip of eutaxitic foliation. Qel/Qbc Qyh along the Henrys Fork. At the same time, strong northeast-directed winds south side of Teton River because of greater thickness of unconsolidated Strike and dip of vertical eutaxitic foliation. deposited loess over the Rexburg Bench. Part of the surface of the basalt of material from preferential deposition of loess. Most slides occurred at or Qbsp Snake River Plain was probably scoured by outwash streams, as shown by below the maximum reservoir elevation of 5,301.7 ft. Slides were mapped Strike and dip of overturned eutaxitic foliation. the anomalously thin loess cover on the flow. 78 Qyh using air photos taken in June 1976; many of the slides remain visible on Qyh 83 images taken in 2004. Boundary of Teton Reservoir on June 5, 1976, elevation 5301.7 ft. Qel/Qbsp UNST-8 TETON DAM DISASTER Boundary of area inundated by floodwater from Teton Dam Flood Qyh Qyh of June 1976. Because of errors in the original quadrangle On June 5, 1976, the Teton Dam failed catastrophically, killing 14 people ALLUVIAL, COLLUVIAL AND LACUSTRINE DEPOSITS Qa base map, the extent of flooding may not agree with topogra- Qbc Qyh and causing $400 million to $1 billion dollars (1976 dollars) in flooding Alluvium of the Teton River, Falls River, and Henrys Fork (Holocene)—Unconsolidated phy in all areas. Qyh damage. The causes of the disaster have been extensively studied (e.g. Seed clayey silt, silty sand, and gravel. Generally less than 3 m (10 ft) thick. and Duncan, 1987) and show that poor understanding of the geologic Asymmetric ripples in deposits of the Teton Dam failure; ripples 34 conditions at the dam site contributed directly to the disaster. Qc Colluvium and slope wash (Holocene)—unconsolidated angular blocks of tuff are 0.3 to 3 m thick and 2 to 50 m long. The larger ripples in silty tuffaeous matrix at base of steep slopes in Teton River canyon. occur on bars in the Teton River canyon and at the canyon Qbc The dam site in the Teton River canyon (NE/4, Section 30, T. 7 N., R. 42 E.) Generally <5 m thick (16 ft). mouth; smaller ripples occur in downstream areas. consists of Huckleberry Ridge Tuff and a maximum of about 30 m (100 ft) 22 of alluvium in the river channel. Uplands adjacent to the canyon are Qgh Gravel alluvium of the Henrys Fork and Falls River (late Pleistocene)—Poorly Thermal wells showing maximum temperature (°C). Qbc Qel/Qbc covered with up to 9 m (30 ft) of loess. The loess was used to construct most to moderately sorted gravel and sand; thickness from <10 m to about 50 m Qtff Qyh 87 Test wells.
Load more

Recommended publications
  • 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).
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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
    [Show full text]
  • 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.
    [Show full text]
  • 1 Friends of the Teton River 2015 Water Quality Monitoring Program
    Friends of the Teton River 2015 Water Quality Monitoring Program Report: Upper Teton River Watershed Water quality monitoring remains a critical tool for maintaining and protecting our valuable water resources. Program Introduction Water quality in Teton Valley is an area of strong concern to residents, visitors, natural resource experts, and governmental agencies. Although the rapid rate of growth and development in the Valley has slowed in the past several years, significant concerns remain about the effect of changing land use practices on water quality. Adverse changes in the upper Teton River have been observed over the last several decades, including increased siltation, hydrologic alteration, elevated levels of nitrates, elevated levels of bacteria, and a sharp decline in the native Yellowstone cutthroat trout population. The upper Teton River runs from its headwaters on the western side of the Teton Range in Teton County, Wyoming, through Teton Valley to Highway 33 in Teton County, Idaho. In 1998, the United States Environmental Protection Agency (EPA) designated the upper Teton River (from the headwaters to Highway 33) and many of its tributaries as impaired under Section 303 (d) of the federal Clean Water Act (CWA). EPA listed excessive nutrients, temperature increases, flow alterations, and sedimentation as the causes of impairment. In response to these listings, Friends of the Teton River (FTR) designed and implemented a water quality monitoring program for the upper Teton River watershed in 2001. Initially, Idaho Department of Environmental Quality (IDEQ) funded the water quality monitoring program as it collected data from twelve (12) monitoring sites located throughout Teton County, Idaho, and Teton County, Wyoming, at four (4) times per year (see Figure 1 depicting the location of all monitoring sites).
    [Show full text]
  • Henrys Fork Basin Study Final Report 1 1.0 Introduction
    Henrys Fork Basin Study Final Report Produced in partnership with the State of Idaho Water Resource Board U.S. Department of the Interior Idaho Water Resource Board Bureau of Reclamation State of Idaho Pacific Northwest Region Boise, Idaho Snake River Area Office Boise, Idaho January 2015 MISSION OF THE U.S. DEPARTMENT OF THE INTERIOR PROTECTING AMERICA'S GREAT OUTDOORS AND POWERING OUR FUTURE The U.S. Department of the Interior protects America's natural resources and heritage, honors our cultures and tribal communities, and supplies the energy to power our future. MISSION OF THE BUREAU OF RECLAMATION The mission of the Bureau of Reclamation is to manage, develop, and protect water and related resources in an environmentally and economically sound manner in the interest of the American public. Photograph on front cover: Fly fishing, irrigated agriculture, and wildlife habitat are important activities in the Henrys Fork River basin Disclaimer The Henrys Fork Basin Study was funded jointly by the Bureau of Reclamation (Reclamation) and the Idaho Water Resource Board (IWRB), and is a collaborative product of the study participants as identified in Section 1.3, page 5 of this report. The purpose of the study is to assess current and future water supply and demand in the Henrys Fork Basin and adjacent areas that receive water from the basin, and to identify a range of potential strategies to address any projected imbalances. The study is a technical assessment and does not provide recommendations or represent a statement of policy or position of the Bureau of Reclamation, the Department of the Interior, or the funding partners.
    [Show full text]
  • Teton View Regional Plan
    for sustainable development MAY 2015 The work that provided the basis for this publication was supported by funding under an award with the U.S. Department of Housing and Urban Development. The substance and findings of the work are dedicated to the public. The author and publisher are solely responsible for the accuracy of the statements and interpretations contained in this publication. Such interpretations do not necessarily reflect the views of the Government. Preface Sustainable communities partnership On June 16, 2009, the U.S. Department of Housing and Urban Development (HUD), the U.S. Department of Transportation (DOT), and the U.S. Environmental Protection Agency (EPA) joined together to help communities nationwide improve access to affordable housing, increase transportation options, and lower transportation costs, all while protecting the environment. This “Sustainable Communities Partnership” identified six livability principles that would form a framework for the variety of funding programs that each agency intended to design over a multi-year period. These principles are: • Provide more transportation choices • Provide equitable, affordable housing • Enhance economic competitiveness • Support existing communities • Coordinate policies and leverage investment • Value communities and neighborhoods The Sustainable Communities Regional Planning Grant program was launched by HUD in 2010 to encourage cities and counties to collaborate on studies related to regional land use, affordable housing, economic development, community vitality, food equity, public transportation and environmental quality. The grants also provided for training and technical assistance for local communities as means to build their resilience for the future. In November 2011, the Western Greater Yellowstone Consortium (Consortium) was awarded a $1.5 million HUD grant and launched its three-year planning process in February 2012.
    [Show full text]
  • West Rim Ranch CLEMENTSVILLE, IDAHO
    WestCLEMENTSVILLE, Rim Ranch IDAHO West Rim Ranch CLEMENTSVILLE, IDAHO Introduction: The West Rim Ranch is located on the quiet side of the Teton Mountain Range on the northwestern rim of the Big Hole Mountains in both Teton County and Madison County, Idaho. The ranch is comprised of 2,553.56 deeded acres of diverse landscape that includes timbered hillsides, large open pastures, deep tree-lined canyons and a 2.5-mile shared border with the Caribou-Targhee National Forest. From north to south, the ranch ascends to meet the forest border with elevated views of the nearby agricultural landscape and larger ranch holdings to the north and west. Wide-open spaces dominate the horizon, which is framed by numerous mountain ranges including the Lemhi Range, Lost River Range, Centennial Range, and the Big Hole Range. On a clear day, one can see the tree-covered hillsides of Yellowstone National Park. Tate Jarry, Associate Broker Carlos Ordonez, Associate Broker Toll Free 866.734.6100 www.LiveWaterProperties.com Wide Open Spaces...Spanning both Teton and Madison Counties Location: The ranch is located in both Teton and Madison counties, on Idaho’s easternmost edge along the famous Teton Range. Jackson Hole, Wyoming, is positioned an hour and a half away and offers commercial air service, fine dining and endless recreational pursuits. This alpine ranch borders the Caribou-Targhee National Forest along the northern foothills of the Big Hole Mountain Range commonly known as the west rim. The Big Hole Range provides a natural divison between the bustling communities of Idaho Falls and Brigham Young University’s (BYU) Idaho campus in the town of Rexburg (population 80,000) and the Teton Valley communities (population 6,000).
    [Show full text]
  • Idaho Fishing 2019–2021 Seasons & Rules
    Idaho Fishing 2019–2021 Seasons & Rules 1st Edition 2019 Free Fishing Day June 8, 2019 • June 13, 2020 • June 12, 2021 idfg.idaho.gov Craig Mountain Preserving and Sustaining Idaho’s Wildlife Heritage For over 25 years, we’ve worked to preserve and sustain Idaho’s wildlife heritage. Help us to leave a legacy for future generations, give a gift today! • Habitat Restoration • Wildlife Conservation • Public Access and Education For more information visit IFWF.org or call (208) 334-2648 YOU CAN HELP PREVENT THE SPREAD OF NOXIOUS WEEDS IN IDAHO! 1. Cleaning boats, trailers and watercraft after leaving a water body 2. Pumping the bilge of your boat before entering a water body 3. Cleaning boating and fishing gear from any plant material 4. Reporting infestations to your County Weed Superintendent CALL 1-844-WEEDSNO WWW.IDAHOWEEDAWARENESS.COM DIRECTOR MOORE’S OPEN LETTER TO THE HUNTERS, ANGLERS AND TRAPPERS OF IDAHO y 6-year-old grandson caught his first steelhead last year. It was a wild fish and he had Mto release it. We had quite a discussion of why Grandpa got to keep the fish that I had caught earlier, but he had to release his. In spite of my explanation about wild fish vs. hatchery-raised fish, he was confused. Although ultimately, he understood this, when his dad caught a wild steelhead and he had to release it, as well. Both of my grandsons insisted on taking a picture of us with my fish. These moments in the field with our families and friends are the most precious of memories that I hope to continue to have for several decades as a mentor of anglers and hunters, demonstrating “how to harvest” and more importantly how to responsibly interact with wildlife.
    [Show full text]
  • Teton River Canyon Resource Management Plan
    Teton River Canyon Resource Management Plan U.S. Department of the Interior Pacific Northwest Region Snake River Area Office December 2006 Teton River Canyon Resource Management Plan u.s. Department of the Interior Bureau of Reclamation Approved: a Manager Date " ake River Area Office Bo ;~, 1""0 ~ Date ~~~~Pacific Northwest Region Boise, Idaho This Resource Management Plan was prepared by EDA W, CH2M Hill, and JP A under contract for the Department ofthe Interior, Bureau of Reciamation, Pacific Northwest Region. Point of Contact: Robert "Hap" Boyer, Resource Manager Snake River Area Office 1359 Hansen Avenue Burley, ID 83318 (208) 678-0461 MISSION STATEMENT THE MISSION OF THE BUREAU OF RECLAMATION IS TO MANAGE, DEVELOP, AND PROTECT WATER AND RELATED RESOURCES IN AN ENVIRONMENTALLY AND ECONOMICALLY SOUND MANNER IN THE INTEREST OF THE AMERICAN PUBLIC. VISION STATEMENT THROUGH LEADERSHIP, USE OF TECHNICAL EXPERTISE, EFFICIENT OPERATIONS, RESPONSIVE CUSTOMER SERVICE AND THE CREATIVITY OF PEOPLE, RECLAMATION WILL SEEK TO PROTECT LOCAL ECONOMIES AND PRESERVE NATURAL RESOURCES AND ECOSYSTEMS THROUGH THE EFFECTIVE USE OF WATER. T E T O N R I V E R C A N Y O N R E S O U R C E M A N A G E M E N T P L A N CONTENTS Chapter 1 Introduction .................................................................................................................. 1-1 1.1 RMP Program and Policy...................................................................................... 1-1 1.2 Purpose and Scope of the Plan .............................................................................. 1-1 1.3 Location and Description of the RMP Study Area................................................ 1-2 1.4 Project Summary ................................................................................................... 1-5 Chapter 2 Existing Conditions ...................................................................................................... 2-1 2.1 Natural Resources.................................................................................................
    [Show full text]