The Boulder River Watershed Study, Jefferson County, Montana
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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. -
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. -
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. -
SP114-Earthqake Map.FH10
Special Publication No. 114 MONTANA BUREAU OF MINES AND GEOLOGY Stickney et al. 2000 A Department of Montana Tech of The University of Montana Table 1. Names and parameters of Quaternary faults in western Montana. Fault Fault name Most recent Slip rate End-to-end Strike Fault type, Introduction quality for epicentral locations of pre-1995 earthquakes in northwest no. earthquake (mm/yr) length (km) (average) down direction The year 1999 marked the fortieth anniversary of the last destructive Montana is generally below that for southwest Montana. For the Montana earthquake. In contrast, the previous 40 years (19201960) same reason, many small northwest Montana earthquakes went 606 Deadman fault* <1.6 Ma <0.2 (?) 70.8 306° Normal, SW 614 Unnamed fault near Monida* <1.6 Ma <0.2 (?) 13.7 302° Normal, SW saw the occurrence of four major earthquake sequences in Montana. undetected prior to 1995. 641 Red Rock fault -------- ------ 40.7 326° Normal, NE Considering the state's history of damaging earthquakes, it is natural 641a Unnamed (north) section <1.6 Ma <0.2 (?) 14.4 337° Normal, NE that one may ponder the causes and sources of these earthquakes. The quality of seismic monitoring in northwest Montana improved 641b Timber Butte section <130 ka <0.2 (?) 9.3 327° Normal, NE In western Montana and throughout the Intermountain West, only dramatically in 1995 when the MBMG entered into a cooperative 641c Sheep Creeks section <15 ka 0.2-1.0 (?) 14.8 316° Normal, NE the very largest historic earthquakes can be ascribed to specific agreement with the Confederated Kootenai and Salish Tribes 642 Emigrant fault -------- ------ 52.0 41° Normal, NW 642a Unnamed (north) section <130 ka 0.2-1.0 (?) 12.9 21° Normal, W faults with certainty. -
The Mission Mountains Tribal Wilderness
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 1995 A Confluence of sovereignty and conformity : the Mission Mountains Tribal Wilderness Diane L. Krahe 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 Krahe, Diane L., "A Confluence of sovereignty and conformity : the Mission Mountains Tribal Wilderness" (1995). Graduate Student Theses, Dissertations, & Professional Papers. 8956. https://scholarworks.umt.edu/etd/8956 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]. A CONFLUENCE OF SOVEREIGNTY AND CONFORMITY: THE MISSION MOUNTAINS TRIBAL WILDERNESS by Diane L Krahe BA Bridgewater College, 1986 presented in partial fulfillment of the requirements for the degree of Master of Science The University of Montana 1995 Approved by; Chairperson Dean, Graduate School Date UMI Number: EP39757 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. UMT OiSiMflAtion Pubiishrig UMI EP39757 Published by ProQuest LLC (2013). Copyright in the Dissertation held by the Author. -
Cabinet-Yaak Grizzly Bear Recovery 2016 Research and Monitoring Progress Report
CABINET-YAAK GRIZZLY BEAR RECOVERY AREA 2016 RESEARCH AND MONITORING PROGRESS REPORT PREPARED BY WAYNE F. KASWORM, THOMAS G. RADANDT, JUSTIN E. TEISBERG, ALEX WELANDER, MICHAEL PROCTOR, AND HILARY COOLEY 2017 UNITED STATES FISH AND WILDLIFE SERVICE GRIZZLY BEAR RECOVERY COORDINATOR'S OFFICE UNIVERSITY OF MONTANA, MAIN HALL ROOM 309 MISSOULA, MONTANA 59812 (406) 243-4903 1 This annual report is cumulative and represents data collected since the inception of this monitoring program in 1983. New information collected or made available to this study is incorporated, reanalyzed, and summarized annually. Information in this report supersedes previous reports. Please obtain permission prior to citation. Cite this report as follows: Kasworm, W. F., T. G. Radandt, J.E. Teisberg, A. Welander, M. Proctor, and H. Cooley. 2017. Cabinet-Yaak grizzly bear recovery area 2016 research and monitoring progress report. U.S. Fish and Wildlife Service, Missoula, Montana. 101 pp. ABSTRACT Sixteen grizzly bears were monitored with radio collars during portions of 2016. Research monitoring included seven females (three adults and four subadults) and nine males (five adults and four subadults) in the Cabinet-Yaak ecosystem (CYE). Two bears of these bears were from the Cabinet Mountains (1 subadult male and 1 subadult female) and part of the augmentation program. Grizzly bear monitoring and research has been ongoing in the Cabinet Mountains since 1988 and in the Yaak River since 1986. Sixty-eight resident bears have been captured and monitored through telemetry in the two areas from 1986-2016. Research in the Cabinet Mountains indicated that only a small population remained as of 1988. -
Quaternary and Late Tertiary of Montana: Climate, Glaciation, Stratigraphy, and Vertebrate Fossils
QUATERNARY AND LATE TERTIARY OF MONTANA: CLIMATE, GLACIATION, STRATIGRAPHY, AND VERTEBRATE FOSSILS Larry N. Smith,1 Christopher L. Hill,2 and Jon Reiten3 1Department of Geological Engineering, Montana Tech, Butte, Montana 2Department of Geosciences and Department of Anthropology, Boise State University, Idaho 3Montana Bureau of Mines and Geology, Billings, Montana 1. INTRODUCTION by incision on timescales of <10 ka to ~2 Ma. Much of the response can be associated with Quaternary cli- The landscape of Montana displays the Quaternary mate changes, whereas tectonic tilting and uplift may record of multiple glaciations in the mountainous areas, be locally signifi cant. incursion of two continental ice sheets from the north and northeast, and stream incision in both the glaciated The landscape of Montana is a result of mountain and unglaciated terrain. Both mountain and continental and continental glaciation, fl uvial incision and sta- glaciers covered about one-third of the State during the bility, and hillslope retreat. The Quaternary geologic last glaciation, between about 21 ka* and 14 ka. Ages of history, deposits, and landforms of Montana were glacial advances into the State during the last glaciation dominated by glaciation in the mountains of western are sparse, but suggest that the continental glacier in and central Montana and across the northern part of the eastern part of the State may have advanced earlier the central and eastern Plains (fi gs. 1, 2). Fundamental and retreated later than in western Montana.* The pre- to the landscape were the valley glaciers and ice caps last glacial Quaternary stratigraphy of the intermontane in the western mountains and Yellowstone, and the valleys is less well known. -
Greater Yellowstone Ecosystem, with Yellowstone at Its Core, Is One of the Largest Nearly Intact Temperate- Zone Ecosystems on Earth
ECOSYSTEM The Greater Yellowstone Ecosystem, with Yellowstone at its core, is one of the largest nearly intact temperate- zone ecosystems on Earth. Greater Yellowstone Ecosystem At 3,437.5 square miles (8,903 km2),Yellowstone As development throughout the West increased, National Park forms the core of the Greater the 2.2 million acres (8,903 km2) of habitat that now Yellowstone Ecosystem—one of the largest nearly compose Yellowstone National Park became an intact temperate-zone ecosystems on Earth. Greater important sanctuary for the largest concentration of Yellowstone’s diversity of natural wealth includes wildlife in the lower 48 states. the hydrothermal features, wildlife, vegetation, lakes, The abundance and distribution of these animal and geologic wonders like the Grand Canyon of the species depend on their interactions with each other Yellowstone River. and on the quality of their habitats, which in turn is the result of thousands of years of volcanic activ- Heart of an Ecosystem ity, forest fires, changes in climate, and more recent Yellowstone National Park was established in 1872 natural and human influences. Most of the park primarily to protect geothermal areas that contain is above 7,500 feet (2,286 m) in elevation and un- about half the world’s active geysers. At that time, the derlain by volcanic bedrock. The terrain is covered natural state of the park was largely taken for granted. with snow for much of the year and supports forests Quick Facts Space and Ownership • Managed by state governments, Management Challenges