Montana/Dakotas Lands Day in September
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Mineral Resource Assessment of the Custer National Forest in The
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Mineral Resource Assessment of the Custer National Forest in the Pryor Mountains, Carbon County, South-Central Montana by Bradley S. Van Gosen1 , Anna B. Wilson1 , and Jane M. Hammarstrom2, with a section on GEOPHYSICS by Dolores M. Kulik1 Open-File Report 96-256 1996 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1 U.S. Geological Survey, Denver, Colorado 2 U.S. Geological Survey, Reston, Virginia CONTENTS Page Abstract .................................................. 1 Introduction ................................................ 2 Geology of the Pryor Mountains ................................... 7 Regional and local structural setting ............................. 7 Stratigraphy .......................................... 11 Uranium-vanadium deposits of the Pryor Mountains ...................... 13 Mining history ......................................... 13 Geology of the host collapse structures .......................... 17 Mineral deposits and associated alteration ........................ 21 Size, grade, and distribution of the deposits ....................... 26 Origin of the deposits .................................... 26 Exploration criteria and previous reconnaissance studies ................ 29 Geophysics by Dolores M. Kulik -
AGRONOMY NEWS University of Saskatchewan
NON-PROFIT ORG U.S. POSTAGE PAID 2525 River Road BISMARCK, ND Bismarck ND 58503 PERMIT NO. 433 RETURN SERVICE REQUESTED Western Ag Labs Announces Accipiter and Peregrine Winter Wheat Varieties WestBred Releases Two New Winter Wheat Varieties Contacts The varieties Boomer and Striker were developed to eventually replace CDC Falcon and Varieties were developed by the Department of Plant Sciences, Falcon. CDC Peregrine has winter hardiness that is better than CDC Buteo in the WestBred winter wheat line up for the Northern Plains. Foundation AGRONOMY NEWS University of Saskatchewan. CDC Falcon and similar to the cold tolerant check cultivar Jerry. Blake Vander Vorst seed was produced in MN and SD in 2009. They are a cross between Jerry and CDC Fal- Vol 9 - Issue 3 CDC ACCIPITER - CDC Accipiter is a hard red winter wheat with It is slightly taller than Jerry, but its straw strength is comparable Senior Agronomist con, the logic behind this cross was to get a winter hardy variety with the yield attributes grain yield potential that is better than CDC Falcon. Its winter har- to Jerry. The stem and leaf rust resistance is similar to the most 2525 River Road of CDC Falcon and Jerry, the standability and height of CDC Falcon and the leaf rust diness is superior to that of CDC Falcon. It has a plant resistant checks. Limited Bismarck, ND 58503 resistance of Jerry. height that is taller than CDC Falcon and considered data from 2006 suggests that 701.355.3500 Boomer and Striker are both high yielding wheat’s with excellent winter hardiness [email protected] an intermediate height semi-dwarf. -
Prevalence of Self-Reported Hypertension and Antihypertensive Medication Use Among Adults — United States, 2017
Morbidity and Mortality Weekly Report Weekly / Vol. 69 / No. 14 April 10, 2020 Prevalence of Self-Reported Hypertension and Antihypertensive Medication Use Among Adults — United States, 2017 Claudine M. Samanic, PhD1,2,3; Kamil E. Barbour, PhD1; Yong Liu, MD1; Jing Fang, MD4; Hua Lu, MS1; Linda Schieb, MSPH4; Kurt J. Greenlund, PhD1 Hypertension, or high blood pressure, is a major risk factor 50 states, the District of Columbia (DC), and U.S. territo- for heart disease and stroke (1). The prevalence of hyperten- ries. In 2017, a total of 450,016 adults were interviewed. The sion is higher among men than among women, increases present study includes data from the 50 states and DC; the with age, is highest among non-Hispanic blacks (blacks) (2), median response rate was 45.9% (range = 30.6%–64.1%).§ and has been consistently highest in the Southeastern region Respondents were classified as having hypertension if they of the United States (1). To update prevalence estimates for answered “yes” to the question “Have you ever been told by a self-reported hypertension and use of antihypertensive medi- doctor, nurse, or other health professional that you have high cation, CDC analyzed data from the 2017 Behavioral Risk § Factor Surveillance System (BRFSS). The overall (unadjusted) https://www.cdc.gov/brfss/annual_data/2017/pdf/2017-sdqr-508.pdf. prevalence of self-reported hypertension was 32.4% (95% con- fidence interval [CI] = 32.1%–32.7%). The age-standardized, INSIDE median state-specific prevalence of self-reported hypertension 399 Vital Signs: Newly Reported Acute and Chronic was 29.7% (range = 24.3%–38.6%). -
2012 Community Profile
2012 Community Profile Chamber of Commerce Resource Guide Grand Forks, ND East Grand Forks, MN Eat. Meet. Stay. Play. With 201 superior guest rooms, 3 restaurants and the state’s largest indoor waterpark, it’s your destination for FUN! Canad Inns Destination Center Grand Forks is connected to the Alerus Center, the region’s largest sports, meeting and entertainment complex and is located close to the University of North Dakota Campus and Grand Forks’ popular shopping areas. Reserve your rooms today! Canad Inns Destination Center Grand Forks 1000 South 42nd Street, Grand Forks, ND 58201 Phone: (701) 772-8404 Call Toll Free: 1-888-33-CANAD (22623) or go online: canadinns.com Chamber Ad.Hugos.121511.ai 1 12/15/2011 12:34:26 PM www.hugoswineandspirits.com 2 GRAND FORKS LOCATIONS EAST GRAND FORKS 1325 S. COLUMBIA ROAD 1950 32nd Ave S 310 14th Street NE between and Scheels Across the parking located at in East Grand Forks lot from on 32nd Ave S EGF Store Hours: GF Store Hours: Mon - Sat: 8:30 am - 10:00 pm Mon - Thurs: 8:00 am - 10:00 pm Fri - Sat: 8:00 am - 11:00 pm Sun: 12:00 pm - 9:00 pm C M Y CM MY CY - Find us on facebook - Please use our products responsibly Fan Page: Hugo’s Wine & Spirits CMY K Family Owned and Operated Since 1939 Open 6 a.m. to Midnight 7 Days a Week! 8 Locations to Serve You! Grand Forks East Grand Forks Crookston Thief River Falls Jamestown gohugos.com gohugos.com Community Profile The Grand Forks/East Grand Forks area is a place for fami- people. -
Mcgough from the Ground up Newsletter Dakotas Region Q1.2021
McGough From the Ground Up Newsletter Dakotas Region Q1.2021 WE’RE PLANTING A NEW FLAG We are pleased to announce that we are opening a new office in Sioux Falls, SD. The new Sioux Falls office builds on McGough’s strong history of successfully managing a wide variety of projects throughout the Dakotas. The recently completed Terex Manufacturing project located in Watertown, SD, won a 2020 ENR Best Project Award. The newly completed Block 9 project has transformed the skyline of downtown Fargo. McGough also has completed successful projects for many of the most well-established organizations in the Dakotas, including Sanford Health, the North Dakota University System, Prairie Lakes Healthcare and Concordia University. Clark Hagen will lead the office as General Manager. Clark has been with McGough for five years, working in the Fargo office as a member of the senior leadership team. Clark and his colleagues are in the process of building out the company’s South Dakota-based team. McGough’s Sioux Falls office, located at 114 N. Main Avenue, will formally celebrate its opening with an open house in the Spring of 2021. Read more. >> South Dakota is an incredibly vibrant and strong BISMARCK OFFICE market that is growing quickly. Many of our current clients and partners are already well established in COMING SOON the state. We are excited about what opportunities McGough is excited to announce the launch of a this expansion in the upper Midwest will bring for new office in Bismarck, ND with intended opening years to come. in early summer of 2021. -
Balkanizing the Balkans Paul L
New England Journal of Public Policy Volume 15 | Issue 2 Article 3 3-21-2000 Balkanizing the Balkans Paul L. Atwood University of Massachusetts Boston, [email protected] Follow this and additional works at: http://scholarworks.umb.edu/nejpp Part of the International Law Commons, Peace and Conflict Studies Commons, and the Soviet and Post-Soviet Studies Commons Recommended Citation Atwood, Paul L. (2000) "Balkanizing the Balkans," New England Journal of Public Policy: Vol. 15: Iss. 2, Article 3. Available at: http://scholarworks.umb.edu/nejpp/vol15/iss2/3 This Article is brought to you for free and open access by ScholarWorks at UMass Boston. It has been accepted for inclusion in New England Journal of Public Policy by an authorized administrator of ScholarWorks at UMass Boston. For more information, please contact [email protected]. Balkanizing the Balkans Paul L. Atwood This article seeks to place the North Atlantic Treaty Organization 's Kosovo war in the context of the larger issue of NATO expansion. It argues that the question of ethnic cleansing in that province of Serbia was largely exploited by the United States, the creator and most powerful member of the alliance, to break up the former Yugoslavia, to divide it, and to make it more manageable for Western interests. In the guise of stopping Serb repression, NATO seized an opportunity to build more bases throughout southeastern Europe, including those being constructed in NATO's newest member states, Poland, the Czech Republic, and Hungary. These actions are deeply threatening to Russia, positioned as it is in either the former USSR or in former Warsaw Pact nations. -
Foraging Ecology of Cougars in the Pryor Mountains of Wyoming and Montana
Utah State University DigitalCommons@USU All Graduate Theses and Dissertations Graduate Studies 5-2014 Foraging Ecology of Cougars in the Pryor Mountains of Wyoming and Montana Linsey Blake Utah State University Follow this and additional works at: https://digitalcommons.usu.edu/etd Part of the Biology Commons Recommended Citation Blake, Linsey, "Foraging Ecology of Cougars in the Pryor Mountains of Wyoming and Montana" (2014). All Graduate Theses and Dissertations. 3292. https://digitalcommons.usu.edu/etd/3292 This Thesis is brought to you for free and open access by the Graduate Studies at DigitalCommons@USU. It has been accepted for inclusion in All Graduate Theses and Dissertations by an authorized administrator of DigitalCommons@USU. For more information, please contact [email protected]. FORAGING ECOLOGY OF COUGARS IN THE PRYOR MOUNTAINS OF WYOMING AND MONTANA by Linsey W. Blake A thesis submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE in Wildlife Biology Approved: _________________ __________________ Eric M. Gese Michael L. Wolfe Major Professor Committee Member __________________ __________________ Toni K. Ruth Mark R. McLellan Committee Member Vice President for Research and Dean of the School of Graduate Studies UTAH STATE UNIVERSITY Logan, Utah 2014 ii Copyright © Linsey W. Blake 2014 All Rights Reserved iii ABSTRACT Foraging Ecology of Cougars in the Pryor Mountains of Wyoming and Montana by Linsey W. Blake, Master of Science Utah State University, 2014 Major Professor: Eric M. Gese Department: Wildland Resources Cougars (Puma concolor) are elusive top-level predators and their predation patterns, particularly upon sensitive species, can be a source of concern to wildlife managers. -
Ii CLIMATE CHANGE THROUGHOUT the DAKOTAS a Thesis Submitted to the Graduate Faculty of the North Dakota State University
CLIMATE CHANGE THROUGHOUT THE DAKOTAS A Thesis Submitted to the Graduate Faculty of the North Dakota State University of Agriculture and Applied Science By Benjamin Robert Uecker In Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE Major Department: Natural Resource Management October 2016 Fargo, North Dakota ii North Dakota State University Graduate School Title CLIMATE CHANGE THROUGHOUT THE DAKOTAS By Benjamin Robert Uecker The Supervisory Committee certifies that this disquisition complies with North Dakota State University’s regulations and meets the accepted standards for the degree of MASTER OF SCIENCE SUPERVISORY COMMITTEE: Adnan Akyuz Chair Christina Hargiss Jack Norland Approved: October 31, 2016 Edward DeKeyser Date Department Chair ii ABSTRACT How is the climate changing on a county level throughout North Dakota (ND) and South Dakota (SD)? To determine this answer, 13 different climate variables were analyzed: temperature minimums and maximums, precipitation, growing degree days (GDD), season length, first and last frost dates, standardized precipitation index (SPI), Palmer drought severity index (PDSI), evapotranspiration (ET), solar radiation, dew point and wind speed. Annual and monthly climatic trends, per decade, were developed and analyzed by county. These climatic variables show various changes throughout North Dakota and South Dakota by either increasing, decreasing or staying the same. iii ACKNOWLEDGEMENTS Special thanks go to Dr. Adnan Akyüz, Dr. Christina Hargiss and Jack Norland, my committee members, for providing the time and equipment necessary to conduct my research and to bring the research to its conclusions. His patience and his expertise on the subject matter are greatly appreciated. I would also like to express my appreciation to everyone who has helped me with this work. -
Child Poverty Higher and More Persistent in Rural America
University of New Hampshire CARSEY RESEARCH Carsey School of Public Policy National Issue Brief #97 Winter 2016 Child Poverty Higher and More Persistent in Rural America Andrew Schaefer, Marybeth J. Mattingly, and Kenneth M. Johnson he negative consequences of growing up in a poor family are well known. Poor children are less likely to have timely immunizations, have Tlower academic achievement, are generally less engaged in school activities, and face higher delinquency rates in adolescent years.1 Each of these has adverse impacts on their health, earnings, and family status in adulthood. Less understood is how the experience of poverty can differ depending on the community context. Being poor in a relatively well-off community with good infrastruc- ture and schools is different from being poor in a place where poverty rates have been high for generations, where economic investment in schools and infrastruc- ture is negligible, and where pathways to success are few.2 The hurdles are even higher in rural areas, where low population density, physical isolation, and the broad spatial distribution of the poor make service delivery and exposure to innovative programs more challenging. Over the past thirty years, the share of counties with high child poverty increased, rising from 36 to 47 More Poor Children, Especially in percent between 1980 and 1990, falling back to 36 Rural Areas percent in 2000, and then surging to include more than half of all counties (58 percent) in 2010. Figure 1 displays the percent of all U.S. counties with high child poverty from 1980 to 20103 by metropolitan status. -
Ecoregions of North Dakota and South Dakota Hydrography, and Land Use Pattern
1 7 . M i d d l e R o c k i e s The Middle Rockies ecoregion is characterized by individual mountain ranges of mixed geology interspersed with high elevation, grassy parkland. The Black Hills are an outlier of the Middle Rockies and share with them a montane climate, Ecoregions of North Dakota and South Dakota hydrography, and land use pattern. Ranching and woodland grazing, logging, recreation, and mining are common. 17a Two contrasting landscapes, the Hogback Ridge and the Red Valley (or Racetrack), compose the Black Hills 17c In the Black Hills Core Highlands, higher elevations, cooler temperatures, and increased rainfall foster boreal Ecoregions denote areas of general similarity in ecosystems and in the type, quality, This level III and IV ecoregion map was compiled at a scale of 1:250,000; it Literature Cited: Foothills ecoregion. Each forms a concentric ring around the mountainous core of the Black Hills (ecoregions species such as white spruce, quaking aspen, and paper birch. The mixed geology of this region includes the and quantity of environmental resources; they are designed to serve as a spatial depicts revisions and subdivisions of earlier level III ecoregions that were 17b and 17c). Ponderosa pine cover the crest of the hogback and the interior foothills. Buffalo, antelope, deer, and elk highest portions of the limestone plateau, areas of schists, slates and quartzites, and large masses of granite that form the framework for the research, assessment, management, and monitoring of ecosystems originally compiled at a smaller scale (USEPA, 1996; Omernik, 1987). This Bailey, R.G., Avers, P.E., King, T., and McNab, W.H., eds., 1994, Ecoregions and subregions of the United still graze the Red Valley grasslands in Custer State Park. -
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. -
Laramide Basement Deformation in the Northern Gallatin Range And
Laramide basement deformation in the northern Gallatin Range and southern Bridger Range, southwest Montana by Erick WB Miller A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Earth Sciences Montana State University © Copyright by Erick WB Miller (1987) Abstract: The mechanical response of Archean "basement" rocks in the cores of Laramide uplifts has received experimental attention, but there have been relatively few field studies documenting Laramide basement behavior. The purpose of this study is to field test existing theoretical basement strain models by documenting the geometry and kinematics of deformation in areas of good exposures. Field studies along well exposed Squaw Creek fault and Canyon Mountain anticline, Gallatin Range, and three anticlines of the southern Bridget Range, southwest Montana, were made by comparing foliations, mesoscopic faults, and slickensides found in basement rocks to Laramide features found in the overlying Cambrian strata. The results show that in regions where the angle of discordance between the base of the Cambrian and Archean metamorphic foliation surfaces was low (Bridget Range anticlines and Canyon Mountain anticline), the basement deformed by oblique flexural-slip on preexisting foliation surfaces. Passive-slip was important in regions where Archean folds blocked foliation parallel slip. Large (12 meter thick) internally undeformed blocks indicate break up of the folded layer into macrogranular segments was preferred over coherent deformation. Deformation in bounding shear zones occurred under sub-greenschist conditions. Decreased grain size and increased fluid influx accompanied a transition from mechanical fracturing and frictional sliding to pressure solution slip. These observations indicate a fold strain model and are compatible with the fold-thrust model (Berg, 1962).