Raft River Aspen Habitat Restoration Project Would Require Certain Precautions During Project Implementation

Total Page:16

File Type:pdf, Size:1020Kb

Raft River Aspen Habitat Restoration Project Would Require Certain Precautions During Project Implementation Albion – Raft River Aspen United States Department of Agriculture Habitat Restoration Project Forest Service Scoping Report February 2017 Minidoka Ranger District, Sawtooth National Forest Cassia County, Idaho and Box Elder County, Utah Photo looking south towards Almo Park, Albion Division by Scott Soletti, October 6, 2014 1 For More Information Contact: Stacy Smith Minidoka Ranger District Office 2306 Hiland Ave South Burley, ID 83318 (208) 678-0430 In accordance with Federal civil rights law and U.S. Department of Agriculture (USDA) civil rights regulations and policies, the USDA, its Agencies, offices, and employees, and institutions participating in or administering USDA programs are prohibited from discriminating based on race, color, national origin, religion, sex, gender identity (including gender expression), sexual orientation, disability, age, marital status, family/parental status, income derived from a public assistance program, political beliefs, or reprisal or retaliation for prior civil rights activity, in any program or activity conducted or funded by USDA (not all bases apply to all programs). Remedies and complaint filing deadlines vary by program or incident. Persons with disabilities who require alternative means of communication for program information (e.g., Braille, large print, audiotape, American Sign Language, etc.) should contact the responsible Agency or USDA’s TARGET Center at (202) 720-2600 (voice and TTY) or contact USDA through the Federal Relay Service at (800) 877-8339. Additionally, program information may be made available in languages other than English. To file a program discrimination complaint, complete the USDA Program Discrimination Complaint Form, AD- 3027, found online at http://www.ascr.usda.gov/complaint_filing_cust.html and at any USDA office or write a letter addressed to USDA and provide in the letter all of the information requested in the form. To request a copy of the complaint form, call (866) 632-9992. Submit your completed form or letter to USDA by: (1) mail: U.S. Department of Agriculture, Office of the Assistant Secretary for Civil Rights, 1400 Independence Avenue, SW, Washington, D.C. 20250-9410; (2) fax: (202) 690-7442; or (3) email: [email protected]. USDA is an equal opportunity provider, employer and lender. 2 Scoping Report Introduction and Current Conditions Aspen has been identified as a keystone species within ecosystems, contributing to not only vegetative biodiversity but also abundance of vertebrae and invertebrate organisms (Campbell and Bartos, 2001.) Quaking aspen (Populous tremuloides) is considered a pioneer species which regenerates following disturbance through root system clones. Research suggests that sage-brush and conifer replaces aspen cover types in the absence of frequent fires and heavy livestock and wildlife browsing (Campbell and Bartos, 2001.) These threats to the aspen cover-type are currently present on the Minidoka Ranger District (MRD). The fire return interval on the landscape has significantly been impacted by humans. Areas that historically burned frequently (for aspen, fire return intervals average between 20 to 60 years) have not burned in 100+ years. Lack of fire has allowed conifers and sage-brush to encroach within previously functioning aspen stands. Properly functioning aspen ecosystems provide benefits for many species and within the project area including mule deer, moose and elk along with cavity nesting birds, raptors and migratory birds that all use aspen for completion of their life cycle. Locally, aspen is a critical forage source for big game, especially during the summer and fall months. During the spring months, multi-age aspen stands provide excellent cover for mule deer fawns. The areas identified for the project encompass some of the larger aspen stands in close proximity to each other. Within the project area, the landscape is naturally broken and has numerous non- target acres included within the analysis area that are dominated by shrub species. However, proposed treatment will specifically target acres that have the potential to regenerate healthy, functioning aspen stands. Prescribed fire is proposed for the majority of treatments to restore aspen stands, however in some areas, hand treatment and pile burning is proposed where broadcast burning is not feasible. Figure 1 below shows the proposed treatments. Project Area This project is located in the Logger Springs area in the south end of the Albion Mountain Range near Elba, Idaho and in the George Peak area on the west end of the Raft River Mountains near Lynn and Yost, Utah. See Figure 1 below. 3 Scoping Report Figure 1. Project Area Map 4 Scoping Report Purpose and Need The purpose of this project is to restore aspen ecosystems in key wildlife habitats on the Minidoka Ranger District. Implementation of proposed treatments will progress towards meeting the Sawtooth National Forest Plan goals and Idaho Department of Fish and Game goals under the Mule Deer Initiative as they relate to aspen habitats. The need for this project is to ensure that the aspen component within these ecosystems does not decline to a point where it becomes eradicated from particular areas of the landscape where it exists now. In addition, these communities currently lack the multi-age structure described in healthy, thriving aspen habitats. Objectives of the Minidoka Aspen Restoration Project Improve wildlife habitat and overall biodiversity by restoring and regenerating aspen stands encroached by conifer. Improve overall ecosystem conditions by creating a “Properly Functioning Condition” (Campbell and Bartos, 2001) that is resistant and resilient to future disturbance. To reduce encroaching conifer species within targeted aspen stands Trigger aspen re-generation of 1,500 stems per acre from burning, on average. Improve big game summer and fall habitats to locally support viable, robust big game populations that meet population goals outlined in state big game management plans. Proposed Action The proposed action includes lop and scatter (slashing), cut and hand-pile, and prescribed fire treatments to reduce conifer encroachment and restore aspen. In areas with very little conifer encroachment, lop and scatter treatments would be used to remove conifers. In most areas, conifer encroachment has reached the point where prescribed fire would be used to set back the conifer species and spur aspen regeneration (Shepperd et. al., 2006.). Cut/hand-pile and/or lop and scatter treatments would be used for acres where prescribed burning is not feasible due to resource concerns or holding issues. Currently, 6,210 acres are identified for slashing and broadcast burning and 2,080 acres for hand cutting and pile burning. No broadcast burning is proposed in the Raft River Division. To achieve the desired mortality in the conifer species, slashing may be needed prior to burning in order to generate fuel loadings that would in turn, create the necessary fire behavior. Slashing broadens the prescription window so that a helitorch may be used on the target acres with minimal risk to the non-target acres and lessening the risk of an escape. Other options for burning would be hand-lighting and plastic sphere dispenser (PSD). Hand-lighting would occur anytime a black line is needed as a holding feature. Using drip torches allows crews on the ground to more easily regulate fire intensity and determine whether the unit is in prescription. In 5 Scoping Report turn, a heli-torch generates more fire intensity than a PSD, so depending on the environmental and weather factors the burn boss can choose the correct tool for the job. Pre- and post-treatment monitoring will occur to ensure project objectives are being met. As post-burn monitoring occurs, project design should provide room for managers implementing these treatments to adapt their fuels and prescribed fire treatments using adaptive management techniques to accomplish the project objectives. Based on the need for aspen restoration and guidelines set forth in the Forest Plan, the goal of these treatments will be to: Description of Treatment Prescriptions Three possible treatments would be available depending on the level of conifer encroachment within aspen stands. Stands with fewer than 50 conifer trees per acre would be lopped and scattered. This would involve cutting all conifer trees existing within the aspen clone to set back the conifer encroachment. Slash generated from the cutting would not exceed 24” (2 feet) in depth and would be scattered away from the bole of the tree to provide nutrients over a broad area as the material decomposes. Any aspen stems damaged during treatment would also be cut in order to spur new regeneration to create a multi-aged stand. The second treatment would target stands with more than 50 conifer trees per acre (on average). Lopping (slashing) treatments would be applied here as well, although the target would be to generate desired fuel and fire behavior conditions for prescribed burning. Prescribed burn objectives would be to create 80-100% mortality of conifer trees within aspen clones, on average. Cutting of conifer within these prescribed burn areas would be dependent on current fuel loading and only done where necessary to generate adequate fire behavior. Some areas may be determined to already possess sufficient ground fuels to generate the targeted fire intensity. The final treatment would be reserved for areas identified as needing treatment, but where underburning is not feasible. In these cases, conifer would be cut and hand-piled and then the piles burned at a later date. These prescribed fire treatments would be done using a helitorch under conditions that limits fire spread outside of target vegetation. Fuel loading generated from slashing and ability to generate heat with the helitorch allows fire managers to burn and meet objectives within the timber without posing a threat to non-timber vegetation. Short runs caused by preheating above timber stands would be expected, however, the further away from the heat pulse generated by the timber, the greater the decrease in pre-heating and associate fire behavior/spread.
Recommended publications
  • 2448, Raft River Mountains Fault
    2448, RAFT RIVER MOUNTAINS FAULT Structure number: 2448. Comments: Hecker's (1993) fault number 6-17. Structure name: Raft River Mountains fault. Comments: Synopsis: Poorly understood middle to late Pleistocene(?) fault in the Raft River Mountains. The fault is in both Utah and Idaho. Date of compilation: 10/99. Compiler and affiliation: Bill D. Black (Utah Geological Survey) and Suzanne Hecker (U.S. Geological Survey). State: Utah. County: Box Elder. 1° x 2° sheet: Brigham City. Province: Basin and Range. Reliability of location: Poor. Comments: Mapped by Compton (1972) and Doelling (1980). Mapping from Doelling (1980). Geologic setting: North-trending normal fault near the Utah-Idaho border along the northeast side of the Raft River Mountains. The Raft River Mountains have a core of Precambrian metamorphic rocks and trend east-west, similar to the Uinta Mountains. Northern slopes of the mountains drain into the Snake River and are considered part of the Snake River Plain, rather than the Great Basin. Sense of movement: N. Comments: Dip: No data. Comments: Dip direction: E. Geomorphic expression: Faulted alluvium. Age of faulted deposits: Middle to late Pleistocene(?). Paleoseismology studies: None. Timing of most recent paleoevent: (4) Middle and late Quaternary (<750 ka). Comments: Recurrence interval: No data. Comments: Slip rate: Unknown, probably <0.2 mm/yr. Comments: Length: End to end (km): 2 Cumulative trace (km): 2 Average strike (azimuth): N1°E REFERENCES Compton, R.R., 1972, Geologic map of the Yost quadrangle, Box Elder County, Utah and Cassia County, Idaho: U.S. Geological Survey Miscellaneous Investigations Series Map I-672, scale 1:31,680.
    [Show full text]
  • Notice Concerning Copyright Restrictions
    NOTICE CONCERNING COPYRIGHT RESTRICTIONS This document may contain copyrighted materials. These materials have been made available for use in research, teaching, and private study, but may not be used for any commercial purpose. Users may not otherwise copy, reproduce, retransmit, distribute, publish, commercially exploit or otherwise transfer any material. The copyright law of the United States (Title 17, United States Code) governs the making of photocopies or other reproductions of copyrighted material. Under certain conditions specified in the law, libraries and archives are authorized to furnish a photocopy or other reproduction. One of these specific conditions is that the photocopy or reproduction is not to be "used for any purpose other than private study, scholarship, or research." If a user makes a request for, or later uses, a photocopy or reproduction for purposes in excess of "fair use," that user may be liable for copyright infringement. This institution reserves the right to refuse to accept a copying order if, in its judgment, fulfillment of the order would involve violation of copyright law. Geothermal Resources Council, TRANSACTIONS Vol. 4, September 1980 SUBSURFACE GEOLOGY OF THE RAFT RIVER GEOTHERMAL AREA, IDAHO H. R. Covington U.S. Geological Survey Box 25046, Denver Federal Center Denver, CO 80225 ABSTRACT . northward onto the Snake River Plain and is flanked on the east by the Sublette and Black Pine The Raft River Valley occupies an upper Mountains, on the west by the Jim Sage and Cenozoic structural basin filled with nearly Cotterel Mountains and on the south by the Raft 1,600 m of fluvial silt, sand, and gravel.
    [Show full text]
  • California National Historic Trail City of Rocks National Reserve
    California National Historic Trail City of Rocks National Reserve A self-guided journey to discovering the California National Historic Trail at City of Rocks City of Rocks National Reserve is a partnership between the National Park Service and the Idaho Department of Parks and Recreation California National Historic Trail City of Rocks National Reserve A self-guided journey to discovering A self-guided journey to discovering the California National Historic Trail at City of Rocks Prepared by Idaho Department of Parks and Recreation and the National Park Service City of Rocks National Reserve PO Box 169 Almo, Idaho 83312 http://parksandrecreation.idaho.gov www.nps.gov/ciro 2015 Contents What’s in store before you explore? There are eight stops, six of which have interpretive signage, along the 10 mile auto route. Introduction 3 Map—Overview 4 Parting of the Ways to the Elba Basin 5 The Almo Valley 6 Twin Sisters in the Distance 7 The Salt Lake Alternate 8 Replica Wagons 9 Wagon Trains 10 Camp 11 Guide Books 12 Trails West Markers 12 Entrance to City of Rocks 13 Trail Ruts 14 First View of Circle Creek Basin 15 Tracy Homestead 16 Camp Rock 17 Treasure Rock 20 Map— Locations of the Waysides and Markers 21 Artists on the Trail 23 Register Rock 24 Pinnacle Pass 27 Ledyard and Margaret Ann Alsip Frink 29 Twin Sisters 30 Salt Lake Alternate-Boise Kelton Stage Route 32 Post Office 33 Granite Pass 34 The Mormon Battalion 35 Life on the Trail 36 Emigrant and Native American Interactions 38 Trouble on the Trail 39 Emigrant Names 40 For Further Study / Credits 41 Bibliography 42 2 Introduction City of Rocks National Reserve (Reserve) was established by Congress on November 18, 1988 in order to preserve and protect the significant historical and cultural resources; to manage recreational use; to protect and maintain scenic quality; and to interpret the nationally significant values of the Reserve.
    [Show full text]
  • Paleozoic Rocks in the Black Pine Mountains, Cassia County, Idaho
    Paleozoic Rocks in the Black Pine Mountains, Cassia County, Idaho GEOLOGICAL SURVEY BULLETIN 1536 Paleozoic Rocks in the Black Pine Mountains, Cassia County, Idaho By]. FRED SMITH, JR. GEOLOGICAL SURVEY BULLETIN 1536 Descriptions of eleven rock units which range in age from Devonian to Permian, the thickest parts being Early Pennsylvanian to· Early Permian UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1983 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data Smith, J. Fred (Joe Fred), 1911-1982 Paleowic rocks in the Black Pine Mountains, Cassia County, Idaho. (Geological Survey Bulletin 1536) Bibliography: 36 p. Supt. of Docs. No.: I 19.3: 1. Geology, Stratigraphic-Paleozoic. 2. Geology-Idaho-Black Pine Mountains. I. Title. II. Series. QE75.B9 no. 1536 557.3s [551.7'2'0979639] 81-607193 [QE.654] AACR2 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Abstract . 1 Introduction . 2 Stratigraphy . 7 Rocks south of West Dry Canyon fault . 8 Lower plate . 8 Devonian System . 8 Jefferson Formation . 8 Mississippian and Pennsylvanian Systems . 9 Manning Canyon Shale . 9 Middle plate . 11 Pennsylvanian System . 11 Oquirrh Formation, limestone member . 11 Lower part . 11 Middle part . 13 Upper part . 15 Oquirrh Formation, limestone, sandstone, and quartzite mem- ber . 17 Oquirrh Formation, limestone and dolomite member . 18 Upper plate . 21 Pennsylvanian and Permian Systems . 21 Oquirrh Formation sandstone and siltstone member . 21 Rocks north of West Dry Canyon fault . 23 Plate I . 23 Pennsylvanian and Permian Systems .
    [Show full text]
  • Summary Table: Characteristics of the Ecoregions of Utah 13
    Summary Table: Characteristics of the Ecoregions of Utah 13. CENTRAL B ASIN AND RANGE 19. WASATCH AND UINTA MOUNTAINS (continued) Level IV Ecoregion Physiography Geology Soil Climate Potential Natural Vegetation*/ Land Use Level IV Ecoregion Physiography GeologyS oil Climate Potential Natural Vegetation*/ Land Use Temperature/ Precipitation Frost Free Mean Temperature Present Vegetation Temperature/ Precipitation Frost Free Mean Temperature Present Vegetation Area Elevation/ Surficial material and bedrockOrder (Great Groups) Common Soil Series Area Elevation/ Surficial material and bedrockOrder (Great Groups) Common Soil Series Moisture Mean annual Mean annual January min/max; Moisture Mean annual Mean annual January min/max; (square Local Relief (square Local Relief Regimes (inches) (days) July min/max, (° F) *Source: Kuchler, 1964 Regimes (inches) (days) July min/max, (° F) *Source: Kuchler, 1964 miles) (feet) miles) (feet) 13a. Salt Deserts 6655 Unglaciated. Mostly barren, nearly level playas, Mostly 4200- Mostly very alkaline, Quaternary mud and Mostly Aridisols (Aquisalids, Mostly Saltair; also Jordan, Mesic/ Mostly 4- 110-190 12/40; Desert/ Mostly barren; some recreational, 19f. Semiarid Foothills 6158 Partially glaciated. Semiarid lower mountain Mostly 5000- Quaternary colluvium, alluvium, and Mollisols (mostly Argixerolls; Agassiz, Yeates Hollow, Mesic, 12-16 60-100 Long, cold Mostly mountain mahogany-oak scrub; Wildlife habitat, livestock grazing, salt flats, mud flats, low terraces, and saline lakes 4650/ salt flat deposits; also Quaternary eolian Haplocalcids); also Alfisols Lakeshore, Bramwell. Soils are Aridic 8; some 50/94 Vegetation is mostly absent; scattered, military,and industrial activity. Tailing slopes, foothills, ridgetops, and alluvial fans. Some 8000; locally glacial drift. Tertiary volcanics, also Argiustolls, Calcixerolls, Broadhead, Charcol, Lizzant, Frigid/ winters also juniper-pinyon woodland/ recreation, and water supply.
    [Show full text]
  • Cassia County, Qs Idaho 113O00’10” O Qw 42 35’05” 86 Qw Ke Iver Ppsp Sna R O Pps 114 03’50” Qa Burley O Qb Sublett Rge
    Cassia County, Qs Idaho 113o0010 o Qw 42 3505 86 Qw ke iver PPsP Sna R o PPs 114 0350 Qa Burley o Qb Sublett Rge. 42 3055 Declo Qs 77 PPsP Qm PPsP Tov Zs Wm QTb Qa PPs QTb Tpf Idahome PPsP Qs Qs PPsP 27 Albion Tps Qs QTb Ps Qs 84 k Zs e Qw Qs e r Tpf 81 TsR Qw C Zs Sublett P Tpf Wm PPs e Malta Qs s Tov Cassia o Wm o Zs Wm Pzu G Tpf Mtns. or Mt. Harrison South Hills PPsP PPsP PPsP Qa Oakley PzZm Elba Ps Ps Qs Qs r e Pzu Tpf Zs Raft River Valley Ps PPsP Ps Blackpine Rge. v Zs i R Tps Tpf Qs Tpf Wm t PzZm f PPs Tpf Zs Tpf a Trapper Pk. Cache Pk. Tms R Qa Tpf Toi Toi PPsP Tpf Zs Tpf Toi Qs Qs Almo Tpf Ms PPsP Tpf Albion Mtns. Wm PPs Zs Zs Toi PPs PPs Almo Qs Qa PzZm Pluton Raft RiverTpf Narrows. Qa Tpf Zs City of Tms Qs Tps Tpf PPsP Qbo Qs Rocks Tpf Qs o o 42 0004 41 5932 o 114o1655 113 0005 Digital Atlas of Idaho, Nov. 2002 0 5 10 miles http://imnh.isu.edu/digitalatlas Compiled by Paul K. Link, 0 8 16 kilometers Idaho State University, Geosciences Dept. http://www.isu.edu/departments/geology/ Cassia County Cassia County, on the south side of the Snake River forms much of Idahos southern boundary with Utah and Nevada on the west. It contains a diverse assemblage of rocks, including the oldest rocks in Idaho, the metamorphic Green Creek gneiss in the Albion Mountains core complex.
    [Show full text]
  • Title 8 Cassia County Comprehensive Plan
    TITLE 8 CASSIA COUNTY COMPREHENSIVE PLAN CASSIA COUNTY, IDAHO COUNTY ADMINISTRATION PLANNING & ZONING / BUILDING DEPARTMENT Courthouse Room #4, 1459 Overland Avenue, Burley, Idaho 83318 Phone (208) 878-7302 • Fax: (208) 878-3510 CASSIA COUNTY, IDAHO COUNTY COMPREHENSIVE PLAN, Revised 2006, Amd. Oct. 2009, Amd. Feb. 2010, Amd. Nov. 2012. TABLE OF CONTENTS Summary .................................................................................................. 2 Introduction ................................................................................................. 2 Purposes of the Plan ...................................................................................... 4 Guidelines .................................................................................................... 5 Components ................................................................................................. 6 Goals, Policies, and Implementation Activities ................................................... 9 A. Property Rights ............................................................................. 12 B. Population .................................................................................... 15 C. School Facilities and Transportation ................................................. 19 D. Economic Development .................................................................. 23 E. Land Use ..................................................................................... 27 F. Natural Resources ........................................................................
    [Show full text]
  • Quaternary Geology of the Albion Mountains, Southern Idaho
    QUATERNARY GEOLOGY OF THE ALBION MOUNTAINS, SOUTHERN IDAHO Kevin Pogue Whitman College Robert Carson Whitman College Doug Clark Western Washington University INTRODUCTION associated with the nearby Yellowstone hot spot to be emplaced on the exposed granite Geologic History (Miller and Bedford, 1999). During the late The Albion Mountains stretch for 50 km Miocene, most of these rhyolitic rocks were between the Idaho/Utah border on the south translated to the east on low-angle normal and the Snake River Plain on the north. The faults as the core complex continued to rise range is part of the Albion–Raft River–Grouse (ref). Quaternary uplift of the range has Creek metamorphic core complex, which occurred along high-angle range-bounding exposes some of the most highly extended and normal faults. The present shape of the deeply-derived rocks of the Basin and Range mountains results primarily from the headward geologic province (Miller, 1980). Granite, erosion of streams that are tributaries of the granitic gneiss, schist and amphibolite Raft and Snake rivers on the north and east belonging to the 2.5 Ga Green Creek Complex and Birch and Goose creeks on the west. are the oldest rocks in the range. These Headward erosion by Raft River tributaries basement rocks are unconformably overlain by eventually breached resistant Proterozoic Proterozoic and Paleozoic sediments that were quartzites in the structural domes of the metamorphosed during crustal thickening in southern Albion Mountains. The Tertiary the hinterland of the Sevier orogenic belt granite cores of the domes where much more (Armstrong, 1968). The highland created by easily weathered, particularly in regions of the Sevier orogeny began to collapse and high joint density and hydrothermal alteration.
    [Show full text]
  • Albion Raft River and Grouse Creek Field Trip Guide
    1 THE ALBION-RAFT RIVER-GROUSE CREEK METAMORPHIC CORE COMPLEX: GEOLOGIC SETTING AND FIELD TRIP GUIDE Elizabeth Miller, Ariel Strickland and Alex Konstantinou, Dept. Geological and Environmental Sciences, Stanford University (Revised from: Elizabeth Miller and Ariel Strickland, 2007 Stanford Field Trip to ARG. Caution: Not necessarily accurate or up-to-date!!!!) Introduction The Albion-Raft River-Grouse Creek metamorphic core complex (ARG) is part of a chain of Cordilleran metamorphic core complexes that lie to the west of the Sevier fold- and-thrust belt (Fig. 1). The ARG is made up of three mountain ranges for which it is named (Fig. 2). The Albion Mountains and Grouse Creek Mountains are characteristic of mountain ranges in the Basin and Range Province; they have a generally north-south orientation and rise abruptly from the surrounding relatively flat topography. The Raft River Mountains have an enigmatic east-west trend and project eastward from the northern end of the Grouse Creek Mountains (Fig. 2). Late Archean crystalline basement is exposed in all three mountain ranges indicating a broad dome or structural culmination beneath this region, where probably 10-15 km minimum of relative vertical uplift (compared to surrounding regions) has occurred. In addition, significant thinning of the overlying upper part of the crust characterizes the geology of this core complex. Eocene and Oligocene granitic plutons are exposed in these ranges and based on geologic relations and cross-sections, most likely underlie much of the ARG. The ARG is unique in the Basin and Range because it is bound on both of its sides (east and west) by normal fault systems and their associated basins.
    [Show full text]
  • Late Quaternary Environmental Change in the Bonneville Basin, Western USA
    Palaeogeography, Palaeoclimatology, Palaeoecology 167 (2001) 243±271 www.elsevier.nl/locate/palaeo Late Quaternary environmental change in the Bonneville basin, western USA D.B. Madsena,*, D. Rhodeb, D.K. Graysonc, J.M. Broughtond, S.D. Livingstonb, J. Hunta, J. Quadee, D.N. Schmitta, M.W. Shaver IIIa aUtah Geological Survey, Salt Lake City, UT 84116, USA bDesert Research Institute, Reno, NV 89512, USA cUniversity of Washington, Seattle, WA 98195, USA dUniversity of Utah, Salt Lake City, UT 84102, USA eUniversity of Arizona, Tucson, AZ 85721, USA Received 9 December 1999; received in revised form 24 July 2000; accepted for publication 7 September 2000 Abstract Excavation and analyses of small animal remains from strati®ed raptor deposits spanning the last 11.5 ka, together with collection and analysis of over 60 dated fossil woodrat midden samples spanning the last 50 ka, provide a detailed record of changing climate in the eastern Great Basin during the late Pleistocene and Holocene. Sagebrush steppe dominated the northern Bonneville basin during the Full Glacial, suggesting that conditions were cold and relatively dry, in contrast to the southern basin, which was also cold but moister. Limber pine woodlands dominated ,13±11.5 ka, indicating increased dryness and summer temperatures ,6±78C cooler than present. This drying trend accelerated after ,11.5 ka causing Lake Bonneville to drop rapidly, eliminating 11 species of ®sh from the lake. From ,11.5±8.2 ka xerophytic sagebrush and shadscale scrub replaced more mesophilic shrubs in a step-wise fashion. A variety of small mammals and plants indicate the early Holocene was ,38C cooler and moister than at present, not warmer as suggested by a number of climatic models.
    [Show full text]
  • Microstructures of a Deformed Kyanite–Quartz Vein of the Raft River Mountains in Northwest Utah, USA
    Microstructures of a deformed kyanite–quartz vein of the Raft River Mountains in northwest Utah, USA Nathaniel A. Ryan Senior Integrative Exercise March 10, 2010 Submitted in partial fulfillment of the requirements for a Bachelor of Arts degree from Carleton College, Northfield, Minnesota. TABLE OF CONTENTS INTRODUCTION.............................................................................................................4 GEOLOGIC SETTING....................................................................................................7 PETROGRAPHY OF THE VEIN.................................................................................15 Outcrop and Sampling...........................................................................................15 Mineralogy............................................................................................................17 KYANITE AND QUARTZ MICROSTRUCTURS......................................................21 Electron backscatter diffraction Analysis..............................................................25 DISCUSSION...................................................................................................................32 CONCLUSIONS .............................................................................................................34 ACKNOWLEDGEMENTS ...........................................................................................36 REFERENCES CITED ..................................................................................................37
    [Show full text]
  • Use, and Seasonal Movements of Greater Sage-Grouse in the Raft River Subunit Management Area, West Box Elder County, Utah - Phase 2 WRI Project ID 2192
    Demography, Vital Rates, Habitat-Use, and Seasonal Movements of Greater Sage-Grouse in the Raft River Subunit Management Area, West Box Elder County, Utah - Phase 2 WRI Project ID 2192: 2013 Annual Report Prepared By: Avery Cook, Brian Wing, and Terry A. Messmer Jack H. Berryman Institute, Utah State University, Logan, UT September 2013 Demography, Vital Rates, Habitat-Use, and Seasonal Movements of Greater Sage-Grouse in the Raft River Subunit Management Area, West Box Elder County, Utah - Phase 2 WRI Project ID 2192: 2013 Annual Report Cooperators: Utah Watershed Restoration Initiative (WRI) Ruby Pipeline and El Paso Corporation Utah Division of Wildlife Resources US Bureau of Land Management Box Elder County Coordinated Resources Management Box Elder County Adaptive Resources Management Sage-grouse Local Working Group Prepared By: Avery Cook, Brian Wing, and Terry A. Messmer Jack H. Berryman Institute, Utah State University, Logan, UT September 2013 2 Table of Contents Introduction .......................................................................................................................... 5 Study Purpose ......................................................................................................................... 5 Objectives .......................................................................................................................... 6 Study Area .......................................................................................................................... 6 Methods .........................................................................................................................
    [Show full text]