Geology and Ground Water Heart Mountain and Chapman Bench Divisions Shoshone Irrigation Project Wyoming
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Secondary Carbonate Accumulations in Soils of the Baikal Region: Formation Processes and Significance for Paleosoil Investigations
Вестник Томского государственного университета. Биология. 2017. № 39. С. 6–28 АГРОХИМИЯ И ПОЧВОВЕДЕНИЕ УДК 631.48 (571.5) doi: 10.17223/19988591/39/1 В.А. Голубцов Институт географии им. В.Б. Сочавы СО РАН, г. Иркутск, Россия Карбонатные новообразования в почвах Байкальского региона: процессы формирования и значение для палеопочвенных исследований Работа выполнена при поддержке РФФИ (проект № 17-04-00092). На данный момент вопросы, касающиеся строения, хронологии и специфики формирования педогенных карбонатов в резкоконтинентальных областях юга Восточной Сибири, остаются практически незатронутыми. Выполнено обобщение сформировавшихся за последние годы представлений о механизмах формирования карбонатных новообразований почв, а также их связи с условиями среды и процессами почвообразования. Оценены пути поступления карбонатов и основные факторы их аккумуляции в профиле почв. Описаны особенности вещественного и изотопного состава карбонатных новообразований в почвах, формирующихся в различных климатических условиях. На основании собственных исследований приводятся данные о разнообразии карбонатных аккумуляций в почвах Байкальского региона, их вещественном составе и роли в качестве палеогеографических индикаторов. Детально рассмотрены следующие формы карбонатных новообразований: ризолиты, игольчатый кальцит, гипокутаны, белоглазка, нодули, кутаны, лессовые куколки. Ключевые слова: карбонаты; педогенные карбонатные новообразования; стабильные изотопы; почвы; палеореконструкции. Введение Первостепенное значение при изучении эволюции почв имеет -
Celebrating 100 Years ■ 2018 Bierstadt Exhibition
fall & winter 2017 Celebrating100 years ■ 2018 Bierstadt exhibition ■ From Thorofare to destination, part 2 ■ Dispatches from the Field: the eagles of Rattlesnake Gulch to the point BY BRUCE ELDREDGE | Executive Director About the cover: In Irving R. Bacon’s (1875 – 1962) Cody on the Ishawooa Trail, 1904, William F. “Buffalo Bill” Cody is either gauging the trail before him, or assessing the miles he left behind. As the Buffalo Bill Center of the West nears the end of its Centennial year, we find ourselves on an Ishawooa Trail of our own—celebrating and appraising the past while we plan for the next hundred years. #100YearsMore ©2017 Buffalo Bill Center of the West. Points West is published for members and friends of the Center of the West. Written permission is required to copy, reprint, or distribute Points West materials in any medium or format. All photographs in Points West are Center of the West photos unless otherwise noted. Direct all questions about image rights and reproduction to [email protected]. Bibliographies, works cited, and footnotes, etc. are purposely omitted to conserve space. However, such information is available by contacting the editor. Address correspondence to Editor, Points West, Buffalo Bill Center of the West, As we near the end of 2017, it’s hard to believe our Centennial is soon to become 720 Sheridan Avenue, Cody, Wyoming 82414, or a memory! We’ve had a great celebratory year filled with people and tales about [email protected]. our first hundred years. Exploring our history in depth these past few months has truly validated the words of Henry Ford, who said, “Coming together is a beginning; ■ Managing Editor | Marguerite House keeping together is progress; working together is success.” ■ Assistant Editor | Nancy McClure The Buffalo Bill Center of the West’s beginning was the coming together in ■ Designer | Desirée Pettet & Jessica McKibben 1917 of the Buffalo Bill Memorial Association (BBMA) to honor their namesake and ■ preserve the Spirit of the American West. -
Common Birds of the Brinton Museum and Bighorn Mountains Foothills
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Zea E-Books Zea E-Books 8-9-2017 Common Birds of The rB inton Museum and Bighorn Mountains Foothills Jackie Canterbury University of Nebraska-Lincoln, [email protected] Paul Johnsgard University of Nebraska - Lincoln, [email protected] Follow this and additional works at: http://digitalcommons.unl.edu/zeabook Part of the Biodiversity Commons, and the Ornithology Commons Recommended Citation Canterbury, Jackie and Johnsgard, Paul, "Common Birds of The rB inton Museum and Bighorn Mountains Foothills" (2017). Zea E- Books. 57. http://digitalcommons.unl.edu/zeabook/57 This Book is brought to you for free and open access by the Zea E-Books at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Zea E-Books by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Common Birds of The Brinton Museum and Bighorn Mountains Foothills Jacqueline L. Canterbury & Paul A. Johnsgard Jacqueline L. Canterbury acquired a passion for birds and conservation in college, earning bachelor’s degrees at the University of Washington and Evergreen State Col- lege plus MS and PhD degrees from the University of Nebraska–Lincoln with an em- phasis in physiology and neuroscience. Her master’s degree program involved de- veloping a conservation strategy for nongame birds for the state of Nebraska, and she worked for several years as a US Forest Service biologist, studying bird popula- tions in the Tongass National Forest in southeast Alaska. She is currently president of the Bighorn Audubon Society chapter in Sheridan, Wyoming, working on estab- lishing regional Important Bird Areas (IBAs). -
What in the World Fall/Winter 2011-2012 Newsletter Geography Awarness Week Pg
In This Issue: Letter from the Chair Pg. 1 What in the World Fall/Winter 2011-2012 Newsletter Geography Awarness Week Pg. 2 “Geography is a Field Discipline” Pg. 2 Letter from the Chair National Geographic Internship Pg. 3 Dear Alumni and Friends of Geography Notably, Caroline McClure completed a at the Univeristy of Wyoming, NGS internship during the spring semester Regional AAG Meeting in Denver Pg. 3 2011 (see page 3). Awards and Recognitions Pg. 4 Greetings from Laramie and the Department The graduate program in geography at UW of Geography at the University of Wyoming! is also thriving. This year eleven new MA UW Geographers in Ethiopia Pg. 5 As you will see while reading this students joined the program coming from newsletter, the Department Donor Challenge Pg. 6 around the United States of Geography at UW and world. We have two Recent Faculty Publications Pg. 7 continues to be active new students from Nepal, in its teaching, research and another from Thailand. Faculty Highlights Pg. 8 and service missions. Additionally, students from We are fortunate to have Michigan, Illinois, Colorado Heart Mountain Pg. 9 a dedicated faculty, and Oklahoma as well knowledgeable staff and as Wyoming joined our great students. Confirming departmental community. this statement is the number A new class of this size and of awards and recognitions diversity is a testament to received over the past few the quality of our faculty months by our departmental and their willingness to community. develop strong mentoring relationships with our Last spring three of our incoming students. We graduate students, Richard are currently reviewing Vercoe, Suzette Savoie, applications for next year, and Alexa Dugan, were Professor and Chair, Gerald R. -
Heart Mountain Wyoming Foundation Newsletter
KOKORO KARA Summer 2014 HEART MOUNTAIN WYOMING FOUNDATION In This Issue: n Advisor in Residence: Eva Kuwata n Archivist Joins HMWF Staff n An Artistic Legacy at Heart Mountain Celebrating the Generations at Heart Mountain: Board Chair Shirley Ann Higuchi I hope you had a wonderful Asian Pa- children. What is more American than tain Draft Resisters Trial as part of the cific American Heritage Month in May! that? National Consortium Conference. This I want to thank all of our friends who When I was a child, though, schools did August, veterans, like Jack Kunitomi, will joined us at the Hogan Lovells offices in not teach the story of the forced relocation come to our August Pilgrimage, and we Washington, D.C., on May 12 for a screen- of Japanese Americans. That is a problem. will honor them for their contribution to ing of David Ono and Jeff MacIntyre’s Because when this story is not told, we be- this country. Witness: The Legacy of Heart Mountain. come at risk of repeating the mistakes of Nisei, Sansei and Yonsei alike are all It was a huge success. Secretary Norman the past. When we do not remember what working together to make sure that the Mineta and I participated on a panel dis- happened to the Issei and Nisei, we lose a story of Heart Mountain is remembered. cussion with Vincent Eng, Partner and part of our history. When we do not use Every summer, we will celebrate genera- CEO of the VENG Group, and Mee Moua, our voices to tell this story when everyone tions—as three or sometimes four genera- President and Executive Director of Asian else seems to have forgotten it, we are at tions of one family join us in Wyoming for Americans Advancing Justice. -
WYOMING Adventure Guide from YELLOWSTONE NATIONAL PARK to WILD WEST EXPERIENCES
WYOMING adventure guide FROM YELLOWSTONE NATIONAL PARK TO WILD WEST EXPERIENCES TravelWyoming.com/uk • VisitTheUsa.co.uk/state/wyoming • +1 307-777-7777 WIND RIVER COUNTRY South of Yellowstone National Park is Wind River Country, famous for rodeos, cowboys, dude ranches, social powwows and home to the Eastern Shoshone and Northern Arapaho Indian tribes. You’ll find room to breathe in this playground to hike, rock climb, fish, mountain bike and see wildlife. Explore two mountain ranges and scenic byways. WindRiver.org CARBON COUNTY Go snowmobiling and cross-country skiing or explore scenic drives through mountains and prairies, keeping an eye out for foxes, coyotes, antelope and bald eagles. In Rawlins, take a guided tour of the Wyoming Frontier Prison and Museum, a popular Old West attraction. In the quiet town of Saratoga, soak in famous mineral hot springs. WyomingCarbonCounty.com CODY/YELLOWSTONE COUNTRY Visit the home of Buffalo Bill, an American icon, at the eastern gateway to Yellowstone National Park. See wildlife including bears, wolves and bison. Discover the Wild West at rodeos and gunfight reenactments. Hike through the stunning Absaroka Mountains, ride a mountain bike on the “Twisted Sister” trail and go flyfishing in the Shoshone River. YellowstoneCountry.org THE WORT HOTEL A landmark on the National Register of Historic Places, The Wort Hotel represents the Western heritage of Jackson Hole and its downtown location makes it an easy walk to shops, galleries and restaurants. Awarded Forbes Travel Guide Four-Star Award and Condé Nast Readers’ Choice Award. WortHotel.com welcome to Wyoming Lovell YELLOWSTONE Powell Sheridan BLACK TO YELLOW REGION REGION Cody Greybull Bu alo Gillette 90 90 Worland Newcastle 25 Travel Tips Thermopolis Jackson PARK TO PARK GETTING TO KNOW WYOMING REGION The rugged Rocky Mountains meet the vast Riverton Glenrock Lander High Plains (high-elevation prairie) in Casper Douglas SALT TO STONE Wyoming, which encompasses 253,348 REGION ROCKIES TO TETONS square kilometres in the western United 25 REGION States. -
A Publication of the Wyoming Native Plant Society
Castilleja A Publication of the Wyoming Native Plant Society October 2004, Volume 23, No. 3 www.uwyo.edu/wyndd/wnps/wnps_home.htm In this issue: Relicts and Refugia . 1 Floristic Diversity of Wyoming Counties . 3 Botanical Novitiates Find Botanical Novelty . 4 Critical Habitat for the Colorado Butterfly Plant . 5 Requiem for a Lawnmower – review. 6 Rocky Mountain Natural History – review . .7 Whitebark Pine - excerpt. 8 Cynoglossum boreale – addition to the state flora 9 Raising Livestock and Lowering Carbon Dioxide . 10 Scholarship Announcement . 11 Natives vs. Imposters. 12 Relicts and Refugia By Bonnie Heidel For all of the breath-taking alpine topography of the Medicine Bow Range, some of its heart-thumping botany lies low across rolling expanses. Three years and three stages of peatland research have documented vast Above: Eriophorum gracile (slender cotton-grass) is montane fen systems in the Medicine Bow circumboreal, with outlying distribution in northwestern Range, refugia for eleven rare Wyoming Wyoming, the Medicine Bow Range and South Park in vascular plant species of concern including five Colorado By B. Heidel relict species previously unknown from southern Wyoming. peatlands harbor close to 10% of the rare Peatland rare species are disjunct or Wyoming plant species of concern. peripheral as they are present in Wyoming, Botanists took a plunge into peatlands denizens of high latitudes, not state and with pilot site surveys on the Medicine Bow and regional endemics that are the focus of most the Shoshone national forests to compile a Wyoming Natural Diversity Database botany working list of peatland rare species, flora, and research. However, review of the Wyoming vegetation at a small number of known or plant species of concern list in 2002 compared inferred peatland study sites (Heidel and against regional peatland floras indicated that Laursen 2003 a, b; Mellmann-Brown 2004). -
This Is a Digital Document from the Collections of the Wyoming Water Resources Data System (WRDS) Library
This is a digital document from the collections of the Wyoming Water Resources Data System (WRDS) Library. For additional information about this document and the document conversion process, please contact WRDS at [email protected] and include the phrase “Digital Documents” in your subject heading. To view other documents please visit the WRDS Library online at: http://library.wrds.uwyo.edu Mailing Address: Water Resources Data System University of Wyoming, Dept 3943 1000 E University Avenue Laramie, WY 82071 Physical Address: Wyoming Hall, Room 249 University of Wyoming Laramie, WY 82071 Phone: (307) 766-6651 Fax: (307) 766-3785 Funding for WRDS and the creation of this electronic document was provided by the Wyoming Water Development Commission (http://wwdc.state.wy.us) VOLUME 11-A OCCURRENCE AND CHARACTERISTICS OF GROUND WATER IN THE BIGHORN BASIN, WYOMING Robert Libra, Dale Doremus , Craig Goodwin Project Manager Craig Eisen Water Resources Research Institute University of Wyoming Report to U.S. Environmental Protection Agency Contract Number G 008269-791 Project Officer Paul Osborne June, 1981 INTRODUCTION This report is the second of a series of hydrogeologic basin reports that define the occurrence and chemical quality of ground water within Wyoming. Information presented in this report has been obtained from several sources including available U.S. Geological Survey publications, the Wyoming State Engineer's Office, the Wyoming Geological Survey, and the Wyoming Oil and Gas Conservation Commission. The purpose of this report is to provide background information for implementation of the Underground Injection Control Program (UIC). The UIC program, authorized by the Safe Drinking Water Act (P.L. -
13Th Bighorn Mountains
13TH BIGHORN MOUNTAINS BURGESS JUNCTION, WYOMING • AUGUST 26 - 28, 2021 TRAIL RATING 3 - 7 Policies & Reminders For All 2021 Jeep Jamborees Event Waiver Follow The Flow • You are required to complete a Release of Liability When you arrive at a Jeep Jamboree, you Waiver for all occupants of your Jeep 4x4. You must must complete these steps in this order: bring it with you to on-site registration. Vehicle Evaluation Registration Trail Sign-Up • A printed, signed, and dated Release of You will not be permitted sign-up for trails until you have Liability Waiver is required for each participant completed Vehicle Evaluation and Registration. attending a Jeep Jamboree USA event. • All passengers in your Jeep 4x4 must sign a Name Badge Release of Liability Waiver. A parent or the Each participant must wear their name badge throughout minor’s legal guardian must sign and date a the entire Jamboree. waiver for participants under the age of 18 years old. • If you forget your signed Release of Liability Waiver, all Trail Stickers occupants of your vehicle must be present at registration Trail stickers provided at trail sign-ups must be displayed to sign a new waiver before you can receive your on your windshield prior to departing for any off-road event credentials. trail ride. On-Site Registrations Will Not Be Accepted Trail Conditions All new registrations of vehicles as well as adding, deleting, Trail conditions can vary widely between trails and or changing passengers must be completed (10) ten days even on the same trail on different days. Factors such as prior to the Jamboree date. -
Oreohelix Land Snails of Heart Mountain Ranch and Tensleep Preserve, Wyoming
Oreohelix land snails of Heart Mountain Ranch and Tensleep Preserve, Wyoming April 2011 Prepared by: Lusha Tronstad Invertebrate Zoologist Wyoming Natural Diversity Database University of Wyoming Laramie, Wyoming 82071 Tele: 307-766-3115 Email: [email protected] Prepared for: Katherine Thompson, Program Director Northwest Wyoming Program of The Nature Conservancy 1128 12th Street, Suite A Cody, Wyoming 82414 Tele: 307-587-1655 Email: [email protected] Suggested citation: Tronstad, L.M. 2011. Oreohelix land snails of Heart Mountain Ranch and Tensleep Preserve, Wyoming. Prepared by the Wyoming Natural Diversity Database, University of Wyoming for The Nature Conservancy. Mountain snails (Oreohelix sp.) are generally considered rare. In fact, Oreohelix peripherica wasatchensis is a candidate species in Utah under the Endangered Species Act, and several species of Oreohelix are considered critically imperiled by NatureServe. In Wyoming, Oreohelix pygmaea is an endemic species (only found in Wyoming) that lives in the Bighorn Mountains. Another species being watched in Wyoming and South Dakota is Oreohelix strigosa cooperi (referred to as Oreohelix cooperi by some), which is only found in the Black Hills and was petitioned for listing under the Endangered Species Act in 2006, but not listed. Oreohelix are relatively large land snails, but little is known about this genus. As their common names suggests, mountain snails live in mountainous regions of western North America. These land snails are active during wet, cool mouths of the year (i.e., early summer). Oreohelix carry their young internally until they are born at ~2.5 whorls. Mountain snails are one of the more obvious land snail genera, because of their large shell size (10-20 mm diameter). -
South Fork and Heart Mountain Faults: Examples of Catastrophic, Gravity-Driven “Overthrusts,” Northwest Wyoming, Usa
Proceedings of the Seventh International Conference on Creationism. Pittsburgh, PA: Creation Science Fellowship SOUTH FORK AND HEART MOUNTAIN FAULTS: EXAMPLES OF CATASTROPHIC, GRAVITY-DRIVEN “OVERTHRUSTS,” NORTHWEST WYOMING, USA Timothy L. Clarey, PhD, MS, MS, BS, 2878 Oaklawn Park, Saginaw, MI, 48603, KEYWORDS: break-away fault, denudation, detachment, gravity slide, gypsum dehydration, overthrust ABSTRACT Overthrust faults have been a source of debate and discussion in creation literature for many years. Their interpretation demands a better explanation in a Flood context. Two fault systems are examined as analogies for an “overthrust” model. The South Fork Fault System (SFFS) and the Heart Mountain Fault System (HMFS) exhibit folding and faulting consistent with thin- skinned overthrust systems. Both systems moved catastrophically under the influence of gravity. The South Fork Fault system (SFFS, southwest of Cody, Wyoming, exhibits tear faults, tight folds, a triangle zone, and flat-ramp geometries along the leading edge of the system. Transport was southeast, down a gentle slope during early to middle Eocene time (Late Flood), approximately coeval with the Heart Mountain Fault system (HMFS). The SFFS detaches in lower Jurassic strata, rich in gypsum-anhydrite, overlain by about 1250 m of Jurassic through Tertiary sedimentary and volcanic rocks. Movement between 5 km and 10 km to the southeast spread the allochthonous mass over an area exceeding 1400 km2. A break-away fault and an area of tectonic denudation mark the upper northwest part of the system. The exposed denuded surface was buried by additional Eocene-age volcanic rocks soon after slip. Catastrophic rear- loading during emplacement of HMFS may have initiated subsequent movement on the SFFS, with dehydration processes trapping water in a near frictionless anhydrite-water slurry. -
A Preliminary Assessment of Paleontological Resources at Bighorn Canyon National Recreation Area, Montana and Wyoming
A PRELIMINARY ASSESSMENT OF PALEONTOLOGICAL RESOURCES AT BIGHORN CANYON NATIONAL RECREATION AREA, MONTANA AND WYOMING Vincent L. Santucci1, David Hays2, James Staebler2 And Michael Milstein3 1National Park Service, P.O. Box 592, Kemmerer, WY 83101 2Bighorn Canyon National Recreation Area, P.O. Box 7458, Fort Smith, MT 59035 3P.O. Box 821, Cody, WY 82414 ____________________ ABSTRACT - Paleontological resources occur throughout the Paleozoic and Mesozoic formations exposed in Bighorn Canyon National Recreation Area. Isolated research on specific geologic units within Bighorn Canyon has yielded data on a wide diversity of fossil forms. A comprehensive paleonotological survey has not been previously undertaken at Bighorn Canyon. Preliminary paleontologic resource data is presented in this report as an effort to establish baseline data. ____________________ INTRODUCTION ighorn Canyon National Recreation Area (BICA) consists of approximately 120,000 acres within the Bighorn Mountains of north-central Wyoming and south-central Montana B (Figure 1). The northwestern trending Bighorn Mountains consist of over 9,000 feet of sedimentary rock. The predominantly marine and near shore sedimentary units range from the Cambrian through the Lower Cretaceous. Many of these formations are extremely fossiliferous. The Bighorn Mountains were uplifted during the Laramide Orogeny beginning approximately 70 million years ago. Large volumes of sediments, rich in early Tertiary paleontological resources, were deposited in the adjoining basins. This report provides a preliminary assessment of paleontological resources identified at Bighorn Canyon National Recreation Area. STRATIGRAPHY The stratigraphic record at Bighorn Canyon National Recreation Area extends from the Cambrian through the Cretaceous (Figure 2). The only time period during this interval that is not represented is the Silurian.