The Midden the Resource Management Newsletter of Great Basin National Park
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The Confusion Range, West-Central Utah: Fold-Thrust Deformation and a Western Utah Thrust Belt in the Sevier Hinterland
The Confusion Range, west-central Utah: Fold-thrust deformation and a western Utah thrust belt in the Sevier hinterland David C. Greene* Department of Geosciences, Denison University, Granville, Ohio 43023, USA ABSTRACT INTRODUCTION tions together while delineating the lateral and oblique thrust ramps that form a signifi cant The Confusion Range in west-central Utah The Confusion Range is a collection of ridges complicating factor in the structure of the fold- has been considered a broad structural trough and small ranges that together form a low moun- thrust system. Together, these fi ve cross sections or synclinorium with little overall shorten- tain range in western Utah, between the more total almost 300 km in map length. Enlarged ing. However, new structural studies indicate imposing Snake Range on the west and House versions of the cross sections at a scale of that the Confusion Range is more accurately Range on the east (Figs. 1 and 2). The range is 1:50,000, along with a discussion of the petro- characterized as an east-vergent, fold-thrust named for its “rugged isolation and confusing leum potential of the region, may be found in system with ~10 km of horizontal shortening topography” (Van Cott, 1990). The Confusion Greene and Herring (2013). during Late Jurassic to Eocene Cordilleran Range exposes ~5000 m of Ordovician through Similar structural style and fold-thrust struc- contractional deformation. For this study, Triassic strata in what has been considered a tures are continuous southward throughout the four balanced and retrodeformable cross broad structural trough or synclinorium (e.g., length of the originally proposed synclinorium, sections across the Confusion Range and Hose, 1977; Anderson, 1983; Hintze and Davis, forming a fold-thrust belt more than 130 km in adjacent Tule Valley were constructed using 2003; Rowley et al., 2009). -
Isotope Hydrology of Lehman and Baker Creeks Drainages, Great Basin National Park, Nevada
UNLV Retrospective Theses & Dissertations 1-1-1992 Isotope hydrology of Lehman and Baker creeks drainages, Great Basin National Park, Nevada Stephen Yaw Acheampong University of Nevada, Las Vegas Follow this and additional works at: https://digitalscholarship.unlv.edu/rtds Repository Citation Acheampong, Stephen Yaw, "Isotope hydrology of Lehman and Baker creeks drainages, Great Basin National Park, Nevada" (1992). UNLV Retrospective Theses & Dissertations. 195. http://dx.doi.org/10.25669/3kmp-t8wo This Thesis is protected by copyright and/or related rights. It has been brought to you by Digital Scholarship@UNLV with permission from the rights-holder(s). You are free to use this Thesis in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/ or on the work itself. This Thesis has been accepted for inclusion in UNLV Retrospective Theses & Dissertations by an authorized administrator of Digital Scholarship@UNLV. For more information, please contact [email protected]. INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. -
Hydrogeologic and Geochemical Characterization of Groundwater
Prepared in cooperation with the Bureau of Indian Affairs Hydrogeologic and Geochemical Characterization of Groundwater Resources in Deep Creek Valley and Adjacent Areas, Juab and Tooele Counties, Utah, and Elko and White Pine Counties, Nevada Scientific Investigations Report 2015–5097 U.S. Department of the Interior U.S. Geological Survey Windmill over an abandoned stock well on the Goshute Indian Reservation looking east with the Deep Creek Range in the background. Hydrogeologic and Geochemical Characterization of Groundwater Resources in Deep Creek Valley and Adjacent Areas, Juab and Tooele Counties, Utah, and Elko and White Pine Counties, Nevada By Philip M. Gardner and Melissa D. Masbruch Prepared in cooperation with the Bureau of Indian Affairs Scientific Investigations Report 2015–5097 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2015 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod/. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner. -
Membership 2005: Year in Review
ESA Newsletter Information for the Members of the Entomological Society of America MARCH 2006 • VOLUME 29, NUMBER 3 Membership 2005: Year in Review By Chris Stelzig, Director of Membership we get too far into the year, I wanted to fin- not withstanding, this is a great, inexpensive and Marketing ish the update on 2005. way to get general feedback from you on a Sections and Branches—The Pacific wide range of topics. Headquarters uses this For the first time since 1992, ESA posted Branch saw the most growth when we com- data for planning purposes. In the Member- two back-to-back years of membership pare 2004 to 2005 with a 12% increase in ship Toolbox on the website (http://www. growth. This is a milestone, especially when membership. Only the Southeastern Branch entsoc.org/membership/toolbox/support_ coupled with the fact that just five years ago saw an actual decline, and that was merely esa/survey.htm), you will find a list of all our we were losing members by the hundreds by one person (a case in point to say that active surveys and an invitation to partici- every year and our funds were quickly dry- EVERY membership renewal is important!). pate in one. ing up. You’ve heard me say “Strength in Section B saw the largest growth last year, Performance—About 80% of members Numbers” for nearly five years now. The leaping more than 10%. who responded felt that they were satisfied reason for this is that membership is the Membership Types—As I mentioned with performance from ESA headquarters. -
Forest Insect Conditions in the United States 1966
FOREST INSECT CONDITIONS IN THE UNITED STATES 1966 FOREST SERVICE ' U.S. DEPARTMENT OF AGRICULTURE Foreword This report is the 18th annual account of the scope, severity, and trend of the more important forest insect infestations in the United States, and of the programs undertaken to check resulting damage and loss. It is compiled primarily for managers of public and private forest lands, but has become useful to students and others interested in outbreak trends and in the location and extent of pest populations. The report also makes possible n greater awareness of the insect prob lem and of losses to the timber resource. The opening section highlights the more important conditions Nationwide, and each section that pertains to a forest region is prefaced by its own brief summary. Under the Federal Forest Pest Control Act, a sharing by Federal and State Governments the costs of surveys and control is resulting in a stronger program of forest insect and disease detection and evaluation surveys on non-Federal lands. As more States avail themselves of this financial assistance from the Federal Government, damage and loss from forest insects will become less. The screening and testing of nonpersistent pesticides for use in suppressing forest defoliators continued in 1966. The carbamate insecticide Zectran in a pilot study of its effectiveness against the spruce budworm in Montana and Idaho appeared both successful and safe. More extensive 'tests are planned for 1967. Since only the smallest of the spray droplets reach the target, plans call for reducing the spray to a fine mist. The course of the fine spray, resulting from diffusion and atmospheric currents, will be tracked by lidar, a radar-laser combination. -
Insects That Feed on Trees and Shrubs
INSECTS THAT FEED ON COLORADO TREES AND SHRUBS1 Whitney Cranshaw David Leatherman Boris Kondratieff Bulletin 506A TABLE OF CONTENTS DEFOLIATORS .................................................... 8 Leaf Feeding Caterpillars .............................................. 8 Cecropia Moth ................................................ 8 Polyphemus Moth ............................................. 9 Nevada Buck Moth ............................................. 9 Pandora Moth ............................................... 10 Io Moth .................................................... 10 Fall Webworm ............................................... 11 Tiger Moth ................................................. 12 American Dagger Moth ......................................... 13 Redhumped Caterpillar ......................................... 13 Achemon Sphinx ............................................. 14 Table 1. Common sphinx moths of Colorado .......................... 14 Douglas-fir Tussock Moth ....................................... 15 1. Whitney Cranshaw, Colorado State University Cooperative Extension etnomologist and associate professor, entomology; David Leatherman, entomologist, Colorado State Forest Service; Boris Kondratieff, associate professor, entomology. 8/93. ©Colorado State University Cooperative Extension. 1994. For more information, contact your county Cooperative Extension office. Issued in furtherance of Cooperative Extension work, Acts of May 8 and June 30, 1914, in cooperation with the U.S. Department of Agriculture, -
3.7.10 Curculioninae Latreille, 1802 Jetzt Beschriebenen Palaearctischen Ceuthor- Rhynchinen
Curculioninae Latreille, 1802 305 Schultze, A. (1902): Kritisches Verzeichniss der bis 3.7.10 Curculioninae Latreille, 1802 jetzt beschriebenen palaearctischen Ceuthor- rhynchinen. – Deutsche Entomologische Zeitschrift Roberto Caldara , Nico M. Franz, and Rolf 1902: 193 – 226. G. Oberprieler Schwarz, E. A. (1894): A “ parasitic ” scolytid. – Pro- ceedings of the Entomological Society of Washington 3: Distribution. The subfamily as here composed (see 15 – 17. Phylogeny and Taxonomy below) includes approx- Scudder, S. H. (1893): Tertiary Rhynchophorous Coleo- ptera of the United States. xii + 206 pp. US Geological imately 350 genera and 4500 species (O ’ Brien & Survey, Washington, DC. Wibmer 1978; Thompson 1992; Alonso-Zarazaga Stierlin, G. (1886): Fauna insectorum Helvetiae. Coleo- & Lyal 1999; Oberprieler et al. 2007), provisionally ptera helvetiae , Volume 2. 662 pp. Rothermel & Cie., divided into 34 tribes. These are geographically Schaffhausen. generally restricted to a lesser or larger degree, only Thompson, R. T. (1973): Preliminary studies on the two – Curculionini and Rhamphini – being virtually taxonomy and distribution of the melon weevil, cosmopolitan in distribution and Anthonomini , Acythopeus curvirostris (Boheman) (including Baris and Tychiini only absent from the Australo-Pacifi c granulipennis (Tournier)) (Coleoptera, Curculion- region. Acalyptini , Cionini , Ellescini , Mecinini , idae). – Bulletin of Entomological Research 63: 31 – 48. and Smicronychini occur mainly in the Old World, – (1992): Observations on the morphology and clas- from Africa to the Palaearctic and Oriental regions, sifi cation of weevils (Coleoptera, Curculionidae) with Ellescini, Acalyptini, and Smicronychini also with a key to major groups. – Journal of Natural His- extending into the Nearctic region and at least tory 26: 835 – 891. the latter two also into the Australian one. -
MULE DEER Units 114-115
Nevada Hunter Information Sheet MULE DEER Units 114-115 LOCATION: Eastern White Pine County – Snake Range. Please see unit descriptions in the Nevada Hunt Book. ELEVATION: From 5,100' in Snake Valley to 12,050' on Mount Moriah. TERRAIN: Gentle to extremely difficult. VEGETATION: Ranges from salt-desert shrub on some valley floors through sage and mixed brush, pinyon/juniper, mountain mahogany and aspen types at mid elevations to aspen/fir/spruce/limber pine/bristlecone pine at higher elevations. Mountainous areas support forest types more than brush, with pinyon and juniper dominating many areas between 6,500’ and 8,000’. Aspen is a minor component in both units. LAND STATUS: The majority of deer habitat is public land administered by either the BLM Ely Field Office or the Ely Ranger District of the Humboldt-Toiyabe National Forest (USFS). Hunting is not permitted on National Park Service lands (Great Basin National Park) located in Unit 115. Note: In 2006, Congress added 11,000 acres to the Mt. Moriah Wilderness in Unit 114 and created a new wilderness area (69,000 acres) on the south end of Unit 115. Vehicles and mechanized equipment, including wheeled game carriers are prohibited in wilderness areas. Contact the Federal Land Management Agency responsible for the area you intend to hunt for more information. Most private land is located on valley bottoms and benches. Private lands do not restrict access to public land. HUNTER ACCESS: Good to fair, based on weather and ground conditions. Access to Unit 114 can be impacted by winter storms. Motorized access is limited by existing roads, terrain and wilderness designations. -
Hybrid Granitoid Rocks of the Southern Snake Range, Nevada
Hybrid Granitoid Rocks of the Southern Snake Range, Nevada GEOLOGICAL SURVEY PROFESSIONAL PAPER 668 Hybrid Granitoid Rocks of the Southern Snake Range, Nevada By DONALD E. LEE and RICHARD E, VAN LOENEN GEOLOGICAL SURVEY PROFESSIONAL PAPER 668 A study of assimilation and the resulting systematic and interrelated differences in chemistry and mineralogy within a well-exposed granitoid outcrop area of 2O square miles UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1971 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Congress catalog-card No. 72-811324 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Fage Chemistry and mineralogy of the granitoid rocks Con. Abstract.._-___--___--__-_-___-_-_-_._____--_______ 1 Mineralogy. _________________________________ 21 Location and geologic setting-___-__----_-_________-__ 1 Petrography and petrology of the granitoid rocks-___- 29 Previous work and purpose of this paper.______________ 2 Snake Creek-Williams Canyon area.____________ 29 Intrusive structures, form, and contact effects...------- 3 Petrography. ____________________________ 29 Snake Creek-Williams Canyon area_______________ 4 Petrology. _______________________________ 31 Pole Canyon-Can Young Canyon area__-------___- 5 Petrogenesis.. _ ___________________________ 33 Young Canyon-Kious Basin area.________________ 6 Pole Canyon-Can Young Canyon area_________ 38 Summary of intrusive rocks._____________________ -
July 22-28, 2012 Field Trip to Snake Range Metamorphic Core Complex (Great Basin National Park and Mt
Sign Up!! GES 209B/291 Spring Quarter Class: July 22-28, 2012 Field Trip to Snake Range Metamorphic Core Complex (Great Basin National Park and Mt. Moriah Wilderness) Elizabeth Miller and Jeffrey Lee Associated with GES 209 (Microstructures) taught Fall Quarter 2011-12 by Miller, Warren and Lee (Blaustein visiting scholar 2011/12) Extensional detachment faults remain enigmatic structures that are controversial in terms of their mechanism of formation and kinematic evolution. The Snake Range has spectacular exposures of footwall mylonites, the detachment fault, overlying brittle fault block mosaics and the inverted deposits of Miocene sedimentary basins. This field trip is a rare opportunity to learn more about crustal scale processes and extensional fault systems as they transition from the ductile to the brittle part of the earth’s crust and to contemplate the geologic details that have made these structures so controversial. Advanced planning is needed, so please let [email protected] know your interest in such a trip before the beginning of Spring Quarter. The schedule is detailed below. Note that depending on interest and how we plan this trip, there can be wilderness hiking/camping involved. Precambrian quartz mylonites and schists, Hendry’s Creek Sunday July 22: Drive out to Snake Range Monday July 23: Syn-faulting Tertiary sedimentary section and its avalanche deposits (top). Precambrian- Cambrian section and views, Wheeler Peak/Stella Lake trails (10-11,000’) Great Basin National Park (right) Tuesday July 24: Part of group has option of packing in to N. Snake Range from mouth of Hendry’s Creek and hike to base of “Table” beneath Mt. -
Molecular Phylogenetics of the Superfamily Curculionoidea (Insecta: Coleoptera)
Molecular Phylogenetics of the Superfamily Curculionoidea (Insecta: Coleoptera) Conrad Paulus Dias Trafford Gillett A thesis submitted in fulfilment of the requirements for the degree of Doctor of Philosophy University of East Anglia Norwich, Norfolk, England March 2014 © This copy of the thesis has been supplied on condition that anyone who consults it is understood to recognise that its copyright rests with the author and that use of any information derived there-from must be in accordance with current UK Copyright Law. In addition, any quotation or extract must include full attribution. 1 Molecular Phylogenetics of the Superfamily Curculionoidea (Insecta: Coleoptera) Conrad Paulus Dias Trafford Gillett March 2014 Thesis abstract This thesis examines higher-level evolutionary history within the superfamily Curculionoidea, the most speciose family-level taxon, which includes beetles commonly known as weevils. This is achieved using a phylogenetic approach incorporating the largest datamatrix yet employed for weevil molecular systematics, and includes an investigation into the prospect of obtaining short phylogenetically informative amplicons from archival museum specimens. Newly obtained DNA sequence data is analysed from a variety of mitochondrial and nuclear loci, including 92 mitogenomes assembled through the approach of next-generation sequencing of pooled genomic DNA. The resulting trees are used to test previous morphological- and molecular-based hypotheses of weevil relationships and classification schemes. Mitogenomic-derived trees reveal topologies that are highly congruent with previous molecular studies, but that conflict with some morphological hypotheses. Strong nodal support strengthens inferences into the relationships amongst most weevil families and suggests that the largest family, the Curculionidae, is monophyletic, if the subfamily Platypodinae is excluded. -
Coleoptera: Curculionidae1
Pacific Insects Monograph 27: 225-259 10 November 1971 ENTOMOLOGY OF THE AUCKLANDS AND OTHER ISLANDS SOUTH OF NEW ZEALAND: COLEOPTERA: CURCULIONIDAE1 By G. Kuschel2 Abstract: This is a supplementary report to that published on the Curculionidae from Auckland, Campbell, Antipodes, and Snares Islands (no species are known from Bounty or Macquarie) and is based on some 2000 additional specimens collected during further trips to the islands. The native fauna now contains 17 genera and 35 species belonging to 9 subfamilies; 4 genera (23.53%) and 21 species (60.0%) being endemic. All genera and species have their closest relatives in the New Zealand mainland. A significant fact is that none of the true wood borers, flower dwellers, or leaf miners is endemic, and that the larvae of all the endemic species live either in the soil (76.33%) or in decaying plants (23.67%). Further discussions on the composition of the fauna are presented. The fauna is also compared with that of other cold-temperate areas of the southern hemisphere. Apart from a general key to the genera, separate keys to the species are given for the Aucklands, Campbell, and the Snares. A few nomenclatural changes were necessary after an examination of some type material previously not available. INTRODUCTION Since the last paper on the subantarctic weevil fauna was published (Kuschel 1964) further parties to several islands have obtained some 2000 additional specimens which included four new species. I had the opportunity of participating in trips to Adams I, South of Auckland I, Campbell I, and Antipodes I. My primaiy object was to find out a little more about the environmental con ditions and feeding habits of each species as well as to gather large amounts of leaf litter, swards, mats, and cushion plants for the extraction of the ground and soil fauna, and some wood samples for rearing the wood borers and their associates.