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Porphyry and Other Molybdenum Deposits of Idaho and Montana
Porphyry and Other Molybdenum Deposits of Idaho and Montana Joseph E. Worthington Idaho Geological Survey University of Idaho Technical Report 07-3 Moscow, Idaho ISBN 1-55765-515-4 CONTENTS Introduction ................................................................................................ 1 Molybdenum Vein Deposits ...................................................................... 2 Tertiary Molybdenum Deposits ................................................................. 2 Little Falls—1 ............................................................................. 3 CUMO—2 .................................................................................. 3 Red Mountain Prospect—45 ...................................................... 3 Rocky Bar District—43 .............................................................. 3 West Eight Mile—37 .................................................................. 3 Devil’s Creek Prospect—46 ....................................................... 3 Walton—8 .................................................................................. 4 Ima—3 ........................................................................................ 4 Liver Peak (a.k.a. Goat Creek)—4 ............................................. 4 Bald Butte—5 ............................................................................. 5 Big Ben—6 ................................................................................. 6 Emigrant Gulch—7 ................................................................... -
Montana Forest Insect and Disease Conditions and Program Highlights
R1-16-17 03/20/2016 Forest Service Northern Region Montata Department of Natural Resources and Conservation Forestry Division 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. -
Mineral Resources of the Cow Creek and Antelope Creek Wilderness Study Areas, Blaine and Phillips Counties, Montana
Mineral Resources of the Cow Creek and Antelope Creek Wilderness Study Areas, Blaine and Phillips Counties, Montana U.S. GEOLOGICAL SURVEY BULLETIN 1722-C Chapter C Mineral Resources of the Cow Creek and Antelope Creek Wilderness Study Areas, Blaine and Phillips Counties, Montana By JAMES W. MYTTON, VIKI BANKEY, M. DEAN KLEINKOPF, JOHN W. M'GONIGLE, and EDWARD E. MCGREGOR U.S. Geological Survey MICHAEL S. MILLER and J. DOUGLAS CAUSEY U.S. Bureau of Mines U.S. GEOLOGICAL SURVEY BULLETIN 1722 MINERAL RESOURCES OF WILDERNESS STUDY AREAS EASTERN MONTANA DEPARTMENT OF THE INTERIOR DONALD PAUL MODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1988 For sale by the Books and Open-File Reports Section U.S. Geological Survey Federal Center Box 25425 Denver, CO 80225 Library of Congress Cataloging-in-Publication Data Mineral resources of the Cow Creek and Antelope Creek Wilderness Study Areas, Blaine and Phillips counties, Montana (Mineral resources of wilderness study areas eastern Montana ; ch. C) (U.S. Geological Survey bulletin ; 1722-C) Bibliography: p. Supt. of Docs. No.: I 19.3:1722-C 1. Mines and mineral resources Montana Cow Creek Wilderness. 2. Mines and mineral resources Montana Antelope Creek Wilderness. 3. Cow Creek Wilderness (Mont.) 4. Antelope Creek Wilderness (Mont.) I. Mvtton, James W. II. Series. III. Series: U.S. Geological Survey bulletin ; 1722-C. QE75.B9 no. 1722-C 557.3 s [553'.09786'15] 87-600377 [TN24.M9] STUDIES RELATED TO WILDERNESS Bureau of Land Management Wilderness Study Areas The Federal Land Policy and Management Act (Public Law 94-579, October 21, 1976) requires the U.S. -
Compilation of Reported Sapphire Occurrences in Montana
Report of Investigation 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg 2015 Cover photo by Richard Berg. Sapphires (very pale green and colorless) concentrated by panning. The small red grains are garnets, commonly found with sapphires in western Montana, and the black sand is mainly magnetite. Compilation of Reported Sapphire Occurrences, RI 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg Montana Bureau of Mines and Geology MBMG Report of Investigation 23 2015 i Compilation of Reported Sapphire Occurrences, RI 23 TABLE OF CONTENTS Introduction ............................................................................................................................1 Descriptions of Occurrences ..................................................................................................7 Selected Bibliography of Articles on Montana Sapphires ................................................... 75 General Montana ............................................................................................................75 Yogo ................................................................................................................................ 75 Southwestern Montana Alluvial Deposits........................................................................ 76 Specifi cally Rock Creek sapphire district ........................................................................ 76 Specifi cally Dry Cottonwood Creek deposit and the Butte area .................................... -
Lord Ranch on Trout Creek Philipsburg, Montana
Lord PHILIRanchPSBURG, on MONTANATrout Creek Lord Ranch on Trout Creek PHILIPSBURG, MONTANA Introduction: The Lord Ranch on Trout Creek enjoys exceptional trout fishing and elk, deer and bird hunting with access to national forest and close proximity to recreation. These 2,691.7 acres are an idyllic mix of pivot- NTRODUCTION I irrigated hay fields, brush-lined creek, riparian zone, rolling grass and timbered mountainside. Ranch improvements include five modern center pivot irrigation systems, two basic homes and assorted barns, RINGS RANCH sheds and outbuildings. Nearby recreational opportunities abound P with winter actives at Discovery Ski Area and summer pursuits at Georgetown Lake. ROCKING CHAIR S Craig Janssen, Montana Managing Broker Jack McInerney, Sales Associate Toll Free 866.734.6100 www.LiveWaterProperties.com Lord Ranch on Trout Creek- Excellent Fishing & Hunting Ranch Location: Located on the scenic byway, Skalkaho Highway, 10 minutes south of the charming mountain town of Philipsburg is the Lord Ranch on Trout Creek. The ranch borders the Deerlodge National Forest and is in the foothills of the Anaconda Mountain Range. Georgetown Lake lies less than a mile east. Philipsburg is the county seat of Granite County and is named for mining engineer Philip Deidesheimer, who platted the town site near gold and silver mines in 1867. Dining, shopping and everyday amenities are available in Phillipsburg. Riddick Field, a public airport with a paved 3,600 foot runway, is nearby for convenience. The cultural center of Missoula, home to the University of Montana, is an hour northwest. Butte, Montana, lies approximately 40 minutes to the east. Both of these communities have a rich history and offer shopping, fine dining and commercial air service. -
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. -
FORT BELKNAP RESERVATION List of Topics
FORT BELKNAP RESERVATION List of Topics BACKGROUND Reservation Overview Regional Geologic Overview GEOLOGIC OVERVIEW Geologic History Summary of Play Types CONVENTIONAL PLAY TYPES Play 1 - Shallow Cretaceous Biogenic Gas Play Play 2 - Northern Plains Biogenic Gas Play Plays 3,4,5 - Jurassic/Cretaceous and Mississippian Plays UNCONVENTIONAL / HYPOTHETICAL PLAY TYPES Plays 6,7 - Fractured Bakken and Cambrian Sandstone Plays REFERENCES Historical Background of the OVERVIEW (i.e. joint ventures) in contrast to procedures and regulatory minimums imposed Assiniboine and Gros Ventre Tribes at Fort Belknap by the previous 1938 Minerals Leasing Act. The 1982 Act further provides that FORT BELKNAP RESERVATION The Fort Belknap Indian Reservation was created in 1887 as the home for the individual Indian allottees may join agreements negotiated for tribal lands. The Assiniboine and Gros Ventre Tribes Assiniboine and Gros Ventre Indian Tribes. The ancestors of these tribes have section entitled Operating Regulations discusses the procedures for obtaining lived on the northern plains for several centuries. The Assiniboine were allottee participance in the negotiated agreement. recognized by Europeans as part of the great Sioux Nation and speak a Siouan Principal components for the formal corporate proposal should include the TRIBAL HEADQUARTERS: Fort Belknap Agency, Montana language. However, their name is taken from a Chippewa word referring to area(s) of interest, type of contract, elaboration of proposed agreement terms, GEOLOGIC SETTING: Williston Basin "those who cook with stones." At some point in time the Assiniboine bands points of potential negotiation, diligence commitments (i.e. drilling), bonus broke with the traditional Sioux and allied themselves with the Cree. -
The Structural Geology and Tectonic History of the Northern Flint Creek
The structural geology and tectonic history of the northern Flint Creek Range, western Montana by Jeffrey Frank Baken A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Earth Science Montana State University © Copyright by Jeffrey Frank Baken (1984) Abstract: The Flint Creek Range of west-central Montana represents an important and rather atypical segment of the Cordilleran fold and thrust belt. The formation of opposing structural asymmetry in the range has not been satisfactorily explained. Field mapping and structural lab work have been incorporated with modern concepts of fold-and-thrust belt geometry to resolve this question. The range has been subdivided into three structural provinces based upon distinct structural geometries. The western province, which represents the eastern edge of the Sapphire allochthon, is characterized by "typical" eastward assymmetry; however, the eastern province displays "atypical" westward asymmetry. The northern province is represented by a change in structural trend (convex to the northeast) and opposing fold-plunges where the Flint Creek and Garnet Ranges meet across the Montana lineament. The kinematic sequence of deformation in the Flint Creek Range incorporates regional tectonic events and features. The Deer Lodge block, which occupies the Belt embayment, moved eastward along a major decollament as the result of combined east-west compression and intrusive wedging by the Idaho batholith (100 m.y. ago). Following development of this allochthon, the Boulder batholith initiated emplacement along the decollement with the Racetrack Creek pluton and the Elkhorn Mountains Volcanics (78-72 m.y. ago) as satellite effects. The "atypical" geometry of the eastern province was produced by the formation of a ramp interface beneath the Flint Creek Range. -
Hydrogeologic Framework of the Upper Clark Fork River Area: Deer Lodge, Granite, Powell, and Silver Bow Counties R15W R14W R13W R12W By
Montana Bureau of Mines and Geology Montana Groundwater Assessment Atlas No. 5, Part B, Map 2 A Department of Montana Tech of The University of Montana July 2009 Open-File Version Hydrogeologic Framework of the Upper Clark Fork River Area: Deer Lodge, Granite, Powell, and Silver Bow Counties R15W R14W R13W R12W by S Qsf w Qsf Yb Larry N. Smith a n T21N Qsf Yb T21N R Authors Note: This map is part of the Montana Bureau of Mines and Geology (MBMG) a n Pz Pz Groundwater Assessment Atlas for the Upper Clark Fork River Area groundwater Philipsburg ValleyUpper Flint Creek g e Pz Qsf characterization. It is intended to stand alone and describe a single hydrogeologic aspect of the study area, although many of the areas hydrogeologic features are The town of Philipsburg is the largest population center in the valley between the Qsc interrelated. For an integrated view of the hydrogeology of the Upper Clark Fork Area Flint Creek Range and the John Long Mountains. The Philipsburg Valley contains 47o30 the reader is referred to Part A (descriptive overview) and Part B (maps) of the Montana 040 ft of Quaternary alluvial sediment deposited along streams cut into Tertiary 47o30 Groundwater Assessment Atlas 5. sedimentary rocks of unknown thickness. The east-side valley margin was glaciated . T20N Yb t R during the last glaciation, producing ice-sculpted topography and rolling hills in side oo B kf l Ovando c INTRODUCTION drainages on the west slopes of the Flint Creek Range. Prominent benches between ac la kf k B Blac oo N F T20N tributaries to Flint Creek are mostly underlain by Tertiary sedimentary rocks. -
Smith River Complaint
Timothy J. Preso Jenny K. Harbine Earthjustice 313 East Main Street Bozeman, MT 59715 Phone: (406) 586-9699 Fax: (406) 596-9695 [email protected] [email protected] Counsel for Plaintiffs MONTANA FOURTEENTH JUDICIAL DISTRICT COURT MEAGHER COUNTY ______________________________________ ) MONTANA ENVIRONMENTAL ) Case No. _______________ INFORMATION CENTER and ) EARTHWORKS, ) ) Plaintiffs, ) ) VERIFIED COMPLAINT FOR v. ) DECLARATORY RELIEF AND ) APPLICATION FOR WRIT OF MONTANA DEPARTMENT OF ) MANDATE ENVIRONMENTAL QUALITY and TINTINA ) ALASKA EXPLORATION, INC., ) ) Defendants. ) ) ) INTRODUCTION 1. This case challenges a decision by the Montana Department of Environmental Quality (“DEQ”) that has the potential to impair the ecological integrity and recreational value of the renowned Smith River and its tributaries. Specifically, this case challenges DEQ’s decision to approve Tintina Alaska Exploration Incorporated’s (“Tintina”) application to amend its exploration license to gain underground access to a mineral deposit at the Black Butte Copper Project near White Sulphur Springs, Montana, without adequately assessing the environmental impacts of such exploration activities—including potential impacts to the Smith River watershed—and in violation of DEQ’s clear legal duties. 2. On November 7, 2012, Tintina submitted an exploration license amendment proposal to expand exploration activities on its Black Butte Copper Project property, located approximately 15 miles north of White Sulphur Springs in Meagher County, Montana. As proposed, Tintina’s amended license would allow for the construction of an exploration tunnel, or “decline,” that would extend underground for nearly a mile into the upper Johnny Lee copper- cobalt-silver deposit zone. The decline is expected to produce a 10,000-ton bulk sample of rock for metallurgical testing. -
Contract for Deed Billings Montana
Contract For Deed Billings Montana Dell remains unargued: she castaways her knitter waste too charmingly? Dresden Howie unthread some socage and feudalize his toiletry so barometrically! Moral and congested Alfred quartersaw almost presentably, though Hadleigh exteriorize his sandbag outsell. Must be a graduate within an accredited law school. Borders thousands of acres of BLM lands. One line you support do harm to provide sure that utilize tax bills are edge to you directly from possible tax collector. Which types of real estate cases so should handle water often? House hunting made easy. Montana foreclosed home auctions and Montana bank owned properties. Crow Agency, requesting that the Graham leases be canceled. Owners of exempted mobile homes will be notified by the department when they receive his property classification and appraisal notices. Never miss an opportunity remains a cheap home, by saving your searches. Are you spin you enough to delete this alert? The movies The Re. The petition was directed to the Billings Area Director, Bureau of Indian Affairs. This is Yellowstone Country! Contact us to side working and one concept our agents to land access to power entire island of homes available. It was violent enough and had just want others to collect when something works. Since forfeiture often beside the concern remedy, notice form name be used in access all cases where a default is imminent. DISMISSED and the decision of the Acting Area Director is AFFIRMED. Did the District Court err in finding that question First Citizens Bank of Billings had no obligation to terrain that thirst the required deeds were placed in escrow by Double S Investors? The Departmentis charged with the responsibility of the management of bay trust obligations inthe best play of Indian beneficiaries. -
Southwest MONTANA Visitvisit Southwest MONTANA
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