Revegetation Guidelines for Western Montana: Considering Invasive Weeds
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Canadian Food Inspection Agency Home > Plants > Plants with Novel Traits > Applicants > Directive 9408 > Biology Documents > Triticum Turgidum Ssp
Canadian Food Inspection Agency Home > Plants > Plants With Novel Traits > Applicants > Directive 9408 > Biology Documents > Triticum turgidum ssp. durum The Biology of Share this page Triticum turgidum ssp. durum (Durum Wheat) This page is part of the Guidance Document Repository (GDR). Looking for related documents? Search for related documents in the Guidance Document Repository Biology Document BIO200607: A companion document to Directive 9408 (Dir9408), Assessment Criteria for Determining Environmental Safety of Plant with Novel Traits Table of Contents Part A General Information A1. Background A2. Scope Part B The Biology of Triticum turgidum ssp. durum B1. General Description, Cultivation and Use as a Crop Plant B2. Brief Outlook at Breeding, Seed Production and Agronomic Practices for Durum Wheat B3. The Reproductive Biology of Triticum turgidum ssp. durum B4. The Centres of Origin of the Species B5. Cultivated Durum Wheat as a Volunteer Weed Part C The Close Relatives of Triticum turgidum ssp. durum C1. InterSpecies / Genus Hybridization C2. Potential for Introgression of Genes from Triticum turgidum ssp. durum into Relatives C3. Occurrence of Related Species of Triticum turgidum ssp. durum in Canada C4. Summary of the Ecology of Relatives of Triticum turgidum ssp. durum Part D Potential Interactions of Triticum turgidum ssp. durum with Other Life Forms During its Life Cycle Table 1. Examples of potential interactions of Triticum turgidum ssp. durum with other life forms during its life cycle in a natural environment Part E Bibliography Part A General Information A1. Background The Canadian Food Inspection Agency (CFIA) is responsible for regulating the field testing of crop plants with novel traits (PNTs) in Canada. -
Historic Settlement of the Rattlesnake Creek Drainage, Montana| an Archaeological and Historical Perspective
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 2005 Historic settlement of the Rattlesnake Creek Drainage, Montana| An archaeological and historical perspective Daniel S. Comer The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Comer, Daniel S., "Historic settlement of the Rattlesnake Creek Drainage, Montana| An archaeological and historical perspective" (2005). Graduate Student Theses, Dissertations, & Professional Papers. 2544. https://scholarworks.umt.edu/etd/2544 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. NOTE TO USERS Page(s) not included in the original manuscript are unavailable from the author or university. The manuscript was microfilmed as received 80-190, 271-289 This reproduction is the best copy available. dfti UMI Maureen and Mike MANSFIELD LIBRARY The University of IVIontdn^ Permission is granted by the author to reproduce this material in its entiret>', provided that this material is used for scholarly purposes and is properly cited in published works and reports. **Please check "Yes" or "No" and provide signature** Yes, I grant permission No, 1 do not grant permission Author's Signature: J. i-O frJir^ Date: Any copying for commercial purposes or fmancial gain may be undertaken only with the author's explicit consent. -
MBMG 505-Jefferson-V2.FH10
GEOLOGIC MAP OF THE CENOZOIC DEPOSITS OF THE UPPER JEFFERSON VALLEY MBMG Open File Report 505 2004 Compiled and mapped by Susan M. Vuke, Walter W. Coppinger, and Bruce E. Cox This report has been reviewed for conformity with Montana Bureau of Mines and Geology’s technical and editorial standards. Partial support has been provided by the STATEMAP component of the National Cooperative Geology Mapping Program of the U.S. Geological Survey under contract Number 03HQAG0090. CENOZOIC DEPOSITS OF THE UPPER JEFFERSON VALLEY Cenozoic deposits are the focus of the Geologic Map of the upper Jefferson Valley. The map is largely a compilation of previous mapping with additional interpretations based on aerial photos and limited additional field work. Older rocks are included to show their relations to the Cenozoic deposits, but they are generalized on the map. Lithologic descriptions of the Cenozoic deposits are given in the map explanation (p. 17). References used for the map compilation are shown on p. 15. The northern and southern parts of the map are discussed separately. NORTHERN PART OF MAP AREA Quaternary deposits A variety of Quaternary deposits blanket much of the slope area of the Whitetail and Pipestone Creek valleys between the flanks of the Highland Mountains and Bull Mountain (Fig. 1). East and southeast of these Quaternary slope deposits are more isolated areas of partly cemented Pleistocene gravels on pediments. One of these gravel deposits near Red Hill (Fig. 1) yielded a late Pleistocene vertebrate assemblage including cheetah, horse, camel, and large mountain sheep. Radiocarbon dates from the lowest part of the sequence range between 10,000 and 9,000 14C yr. -
Plant Releases Forage and Range Research Laboratory - Logan, Utah
PLANT RELEASES FORAGE AND RANGE RESEARCH LABORATORY - LOGAN, UTAH PLANTS FOR THE WEST Plant Materials Release Catalog Featuring Rangeland, Irrigated Pasture, and Turfgrass Germplasm FRRL Reader Instructions Catalog Navigation Table of Contents Using the Table of Contents/Index Rangeland READER INSTRUCTIONS 1. Click on plant of your choice. Recovery Page 1 (See page iii) P-7* Page 2 Discovery Page 3 FirstStrike Page 4 Using the Navigation Bar The navigation bar is located at the bottom Zoom In right of the document. Zoom Out Use the navigation bar to zoom, change the page, and return to the Table of Contents Next Page or Plant Index. Previous Page Press Ctrl+L to enter full screen mode. It may be easier to read the text in this mode. Table of Contents While viewing the document in full screen, only one page is visible at a time. To exit full Reader Instructions screen mode press Ctrl + L again. ? Using the Navigation Panel Adobe Reader features a navigation panel. To activate the Navigation Panel, press F4. A THE FORAGE AND RANGE RESEARCH LABORATORY: menu will appear on the left of your screen. Click the bookmark name or page image (depending on program preference) to navigate to the desired release documentation. Additional Resources Or visit our website To download a For further information about the Logan, Utah standard .pdf of the Forage and Range Research Laboratory. catalog i http://ars.usda.gov/npa/frrl/plantsforthewest 1-435-797-2249 FRRL : FRRL - Plants For The West PLANTS FOR THE WEST 1-435-797-2249 PLANTS FOR THE WEST ii THE FORAGE AND RANGE RESEARCH LABORATORY LOGAN, UTAH MISSION: FRRL GERMPLASM Provide improved plant materials and management alternatives for sustainable stewardship of rangelands, pastures, and turf in the western U.S. -
Chapter 5 Phylogeny of Poaceae Based on Matk Gene Sequences
Chapter 5 Phylogeny of Poaceae Based on matK Gene Sequences 5.1 Introduction Phylogenetic reconstruction in the Poaceae began early in this century with proposed evolutionary hypotheses based on assessment of existing knowledge of grasses (e.g., Bew, 1929; Hubbard 1948; Prat, 1960; Stebbins, 1956, 1982; Clayton, 1981; Tsvelev, 1983). Imperical approaches to phylogenetic reconstruction of the Poaceae followed those initial hypotheses, starting with cladistic analyses of morphological and anatomical characters (Kellogg and Campbell, 1987; Baum, 1987; Kellogg and Watson, 1993). More recently, molecular information has provided the basis for phylogenetic hypotheses in grasses at the subfamily and tribe levels (Table 5.1). These molecular studies were based on information from chloroplast DNA (cpDNA) restriction sites and DNA sequencing of the rbcL, ndhF, rps4, 18S and 26S ribosomal DNA (rDNA), phytochrome genes, and the ITS region (Hamby and Zimmer, 1988; Doebley et al., 1990; Davis and Soreng, 1993; Cummings, King, and Kellogg, 1994; Hsiao et al., 1994; Nadot, Bajon, and Lejeune, 1994; Barker, Linder, and Harley, 1995; Clark, Zhang, and Wendel, 1995; Duvall and Morton, 1996; Liang and Hilu, 1996; Mathews and Sharrock, 1996). Although these studies have refined our concept of grass evolution at the subfamily level and, to a certain degree, at the tribal level, major disagreements and questions remain to be addressed. Outstanding discrepancies at the subfamily level include: 1) Are the pooids, bambusoids senso lato, or herbaceous bamboos the -
The Boulder River Watershed Study, Jefferson County, Montana
The Boulder River Watershed Study, Jefferson County, Montana By Stanley E. Church, David A. Nimick, Susan E. Finger, and J. Michael O’Neill Chapter B of Integrated Investigations of Environmental Effects of Historical Mining in the Basin and Boulder Mining Districts, Boulder River Watershed, Jefferson County, Montana Edited by David A. Nimick, Stanley E. Church, and Susan E. Finger Professional Paper 1652–B U.S. Department of the Interior U.S. Geological Survey Contents Introduction ................................................................................................................................................. 15 Acknowledgments ...................................................................................................................................... 17 Description of Study Area ......................................................................................................................... 17 Hydrologic Setting ............................................................................................................................. 17 Biologic Setting .................................................................................................................................. 19 Geologic Setting................................................................................................................................. 20 Mining History .................................................................................................................................... 20 Remediation Activities -
The Archean Geology of Montana
THE ARCHEAN GEOLOGY OF MONTANA David W. Mogk,1 Paul A. Mueller,2 and Darrell J. Henry3 1Department of Earth Sciences, Montana State University, Bozeman, Montana 2Department of Geological Sciences, University of Florida, Gainesville, Florida 3Department of Geology and Geophysics, Louisiana State University, Baton Rouge, Louisiana ABSTRACT in a subduction tectonic setting. Jackson (2005) char- acterized cratons as areas of thick, stable continental The Archean rocks in the northern Wyoming crust that have experienced little deformation over Province of Montana provide fundamental evidence long (Ga) periods of time. In the Wyoming Province, related to the evolution of the early Earth. This exten- the process of cratonization included the establishment sive record provides insight into some of the major, of a thick tectosphere (subcontinental mantle litho- unanswered questions of Earth history and Earth-sys- sphere). The thick, stable crust–lithosphere system tem processes: Crustal genesis—when and how did permitted deposition of mature, passive-margin-type the continental crust separate from the mantle? Crustal sediments immediately prior to and during a period of evolution—to what extent are Earth materials cycled tectonic quiescence from 3.1 to 2.9 Ga. These compo- from mantle to crust and back again? Continental sitionally mature sediments, together with subordinate growth—how do continents grow, vertically through mafi c rocks that could have been basaltic fl ows, char- magmatic accretion of plutons and volcanic rocks, acterize this period. A second major magmatic event laterally through tectonic accretion of crustal blocks generated the Beartooth–Bighorn magmatic zone assembled at continental margins, or both? Structural at ~2.9–2.8 Ga. -
Development and Testing of Cool-Season Grass Species, Varieties and Hybrids for Biomass Feedstock Production in Western North America
agronomy Article Development and Testing of Cool-Season Grass Species, Varieties and Hybrids for Biomass Feedstock Production in Western North America Steven R. Larson 1,*, Calvin H. Pearson 2, Kevin B. Jensen 1, Thomas A. Jones 1, Ivan W. Mott 1, Matthew D. Robbins 1, Jack E. Staub 1 and Blair L. Waldron 1 1 USDA-ARS, Forage and Range Research, Utah State University, Logan, UT 84322, USA; [email protected] (K.B.J.); [email protected] (T.A.J.); [email protected] (I.W.M.); [email protected] (M.D.R.); [email protected] (J.E.S.); [email protected] (B.L.W.) 2 Agriculture Experiment Station, Department of Soil and Crop Sciences, Colorado State University, Fruita, CO 81521, USA; [email protected] * Correspondence: [email protected]; Tel.: +1-436-5-797-1703 Academic Editors: John W. Forster and Smith Kevin F. Smith Received: 29 September 2016; Accepted: 14 December 2016; Published: 1 January 2017 Abstract: Breeding of native cool-season grasses has the potential to improve forage production and expand the range of bioenergy feedstocks throughout western North America. Basin wildrye (Leymus cinereus) and creeping wildrye (Leymus triticoides) rank among the tallest and most rhizomatous grasses of this region, respectively. The objectives of this study were to develop interspecific creeping wildrye (CWR) × basin wildrye (BWR) hybrids and evaluate their biomass yield relative to tetraploid ‘Trailhead’, octoploid ‘Magnar’ and interploidy-hybrid ‘Continental’ BWR cultivars in comparison with other perennial grasses across diverse single-harvest dryland range sites and a two-harvest irrigated production system. -
Mission Mountains Wilderness Flathead Nazionafou4t Montana
A Proposal. Mission Mountains Wilderness Flathead NaZionaFou4t Montana beyond civilization lies Wilderness, where the earth and its community of life are untrammeled by man, where man himself is a visitor who does not remain. UNITED STATES DEPARTMENT OF AGRICULTURE FOREST SERVICE 7'-'i"J - t7 A PROPOSAL MISSION MOUNTAINS WILDERNESS FLATHEAD NATIONAL FOREST MONTANA Recommended by: (Chief, Forest Service) ir"17' Report Approved: /77/ (éetar of Agriculture) tate) Report on the Proposed MISSION MOUNTAINS WILDERNESS Flathead National Forest Montana Recommendation: This report recommends that 71,927 acres of the Mission Mountains Primitive Area and 1 ,280 contiguous acres, for a total of 73,207 acres, in the Flathead National Forest, State of Montana, be added to the National Wilderness Preservation System by Act of Congress. It will be called the Mission Mountains Wilderness, Flathead National Forest. Administration will be in accordance with the provisions of the Wilderness Act, Public Law 88-577, dated September 3, 1964, and the Regulations of the Secretary of Agriculture, Title 36, Code of Federal Regulations 251.70-251.84. It is further recommended that Primitive Area status be lifted from 2,018 acres found to be unsuitable for inclusion in the National Wilderness Preservation System. U. S. Department of Agriculture Forest Service Northern Region Missoula, Montana TABLE OF CONTENTS PAGE SUMMARY Location Principal Features and Attractions Proximity to Population and Other Classified Areas Acreage Summary I THE AREA 2 Historical 2 General -
Structural Geology of the Northern Snowcrest Range, Beaverhead and Madison Counties, Montana
Western Michigan University ScholarWorks at WMU Master's Theses Graduate College 4-1984 Structural Geology of the Northern Snowcrest Range, Beaverhead and Madison Counties, Montana Mark Kenneth Sheedlo Follow this and additional works at: https://scholarworks.wmich.edu/masters_theses Part of the Geology Commons Recommended Citation Sheedlo, Mark Kenneth, "Structural Geology of the Northern Snowcrest Range, Beaverhead and Madison Counties, Montana" (1984). Master's Theses. 1571. https://scholarworks.wmich.edu/masters_theses/1571 This Masters Thesis-Open Access is brought to you for free and open access by the Graduate College at ScholarWorks at WMU. It has been accepted for inclusion in Master's Theses by an authorized administrator of ScholarWorks at WMU. For more information, please contact [email protected]. STRUCTURAL GEOLOGY OF THE NORTHERN SNOWCREST RANGE, BEAVERHEAD AND MADISON COUNTIES, MONTANA by Mark Kenneth Sheedlo A Thesis Submitted to the Faculty of The Graduate College in partial fu lfillm e n t of the requirements for the Degree of Master of Science Department of Geology Western Michigan University Kalamazoo, Michigan April 1984 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission STRUCTURAL GEOLOGY OF THE NORTHERN SNOWCREST RANGE, BEAVERHEAD AND MADISON COUNTIES, MONTANA Mark Kenneth Sheedlo, M.S. Western Michigan University, 1984 The Snowcrest Range was uplifted in Late Cretaceous and Early •Tertiary time as a consequence of thrusting in Precambrian basement and Phanerozoic cover rocks. The Snowcrest-Greenhorn thrust system is associated with large- scale overturned, eastward verging folds. Mean orientation of the thrust system is N.40°E., 35°N.W.. The trend of the thrust system and associated transverse faults appear to be controlled by earlier structures. -
Surrounded by Mountains
Surrounded by Mountains he Gallatin Valley is one of the most picturesque and Rockies into the jagged peaks we see today. Over the last 50 Geo-Facts: agriculturally productive valleys in Montana. From million years, western Montana experienced several phases of • From the summit of Sacagawea Peak (9,596 ft.) in the northern here, you can see four prominent Montana mountain regional extension and block-faulting, resulting in the creation Bridger Range, you can see even more ranges in a spectacular Tranges: the Bridger Range (east), Gallatin Range (south), of modern Basin-and-Range topography. The crest of the 360o panorama of southwest Montana. Spanish Peaks (southwest), and the Big Belt Mountains Bridger Range arch slowly down-dropped one earthquake at a • A pluton is an intrusive igneous rock body that crystallized from (north). Each range has its own unique geology and topography. time to form the modern Gallatin Valley. Thick layers of mid- magma slowly cooling below the surface of the Earth. Its name The high peaks of the Gallatin Range are carved from volcanic and late Cenozoic sedimentary rocks and more recent stream comes from Pluto, the Roman god of the underworld. rocks and volcanic-derived mudflows that erupted during the deposits have been deposited in the Gallatin Valley, producing • One of the richest gold strikes in Montana history was made at Eocene, approximately 45 million years ago. The Spanish Peaks the fertile landscape that Native Americans called the “Valley of Confederate Gulch in the Big Belt Mountains in 1864. Miners expose metamorphic rocks that date back to the Earth’s early Flowers” – the Gallatin Valley. -
Around Western Montana 2019 by Caroline Provost
“Swifting” All Around Western Montana 2019 by Caroline Provost All photos by Caroline Provost For the first time, Montana Audubon had a team of two technicians, myself and Danny Stark, survey for Black Swifts throughout Western Montana, outside of Glacier National Park. This season we were able to score twenty-one waterfalls, and perform nineteen evening surveys, along with several morning surveys. We are happy to report that after six weeks of traveling and hiking to remote waterfalls we were able to record one site, Rock Creek Falls, in the Cabinet Mountain Wilderness as occupied by a Black Swift (Cypseloides niger). At last, we got lucky during our final pursuit of the season. During our evening survey, we caught a quick glimpse of the crescent moon shaped wings, and knew that it wasn’t another bat we were seeing, it was a Black Swift! In order to confirm our observation, we woke up the following morning at 6:00 AM to perform one last morning survey. We lucked out once again, spotting a black swift zipping in and then back out of its pocket nest niche! While every other site was observed as unoccupied, we were able to acquire valuable habitat characteristic data on each waterfall that has helped us determine which ones would be worth revisiting in the future. The data also gives us more clues as to which variables contribute to the presence or absence of the species, such as moss availability, elevation, or even rock type.This long- term work helps state managers, especially the Montana Natural Heritage Program, determine this specie’s conservation status in a rigorous manner.