Yellowstone Paleontological Survey
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0 Vol 6, No 3 |Ey SPRING 1993 Newslettar of the Llontana Natlve Plant Srclety
--'-'-- Kelseya uniflora cI 0 Vol 6, No 3 |ey SPRING 1993 Newslettar of the llontana Natlve Plant Srclety Type Localities and the Botanical Exploration of Montana - Peter Lesica lf you're a member of the Montana Native Plant Society, you're colfections of blanketflower (Gaillardia aristata), balsamroot probably getting usad to hearing plants referred to by their (Balsamorhiza sagittata), silvery lupine (Lupinus argenteusl and scientific name. Even though the/re often long and hard to mountain death-camas (Zgadenus elegans) - not bad for a da/s pronounce, perhaps you're even becoming convinced that they're work. Two weeks later he found scarlet globe-mallow useful. But where do these names come from, and how do (Sphaeralcea coccinea) near the Marias River in Toole County. taxonomists know what name clrrec.tly applies to which plant? Another early explorer in western Montana was Nathaniel When spotted knapweed first appeared in North America, how did Wyeth. He made a number of type collections from what he said taxonomists know that it was a European weed, Centaurea was the vicinity of the Flathead River. Among these were maculosa, instead of something else - perhaps an undescribed Columbia virgin's-bower (Clematis columbiana), low larkspur species? Taxonomy rests on a system of standards: for each (Delphinium bicololl and Wyeth's lupine (Luprnus wyethiil. He species that is described new to science, there is a type also made the first collections of white-head mule's-ears and specimen. This type specimen represents what the ta,ronomist northern mu le's-ears (Wy eth i a am pl e x i cau I i s artd W. -
Big Sky, MT 59716 Images Via Email to [email protected] Or Use #Explorebigsky on Social Media to Be (406) 995-2055 • [email protected] Eligible
May 12 - May 25, 2017 Volume 8 // Issue #10 Gallatin Valley gives big Nearly $700,000 raised in 24 hours Yellowstone River open for business Music in the Mountains kicks off June 22 Special Travel Section Day trips, weekend getaways and exotic locales Back 40: Gardening tips for a short growing season #explorebigsky explorebigsky explorebigsky @explorebigsky ON THE COVER: Tessa Moeckel climbs at Practice Rock, a popular crag located in Hyalite Canyon. PHOTO BY JOHN MEYER TABLE OF CONTENTS May 12 – May 25, 2017 Volume 8, Issue No. 10 Section 1: News Gallatin Valley gives big Owned and published in Big Sky, Montana Opinion.............................................................................4 Nearly $700,000 raised PUBLISHER Eric Ladd Local.................................................................................5 12 in 24 hours EDITORIAL Montana.........................................................................13 MANAGING EDITOR Regional.........................................................................15 Tyler Allen Yellowstone River SENIOR EDITOR Section 2: Environment, Sports, Health & Dining Amanda Eggert open for business 21 ASSOCIATE EDITOR Environment..................................................................17 Sarah Gianelli Sports.............................................................................20 CREATIVE Music in the Mountains LEAD DESIGNER Business.........................................................................21 Carie Birkmeier kicks off June 22 Health.............................................................................24 -
Custer Gallatin National Forest Beartooth Ranger District Information Packet
CUSTER GALLATIN NATIONAL FOREST BEARTOOTH RANGER DISTRICT INFORMATION PACKET www.fs.usda.gov/custergallatin Did You Know? • The highest 41 peaks in Montana are in the Beartooth Mountains. 22 of these are over 12,000ft. • Granite Peak is Montana’s highest peak, at 12,799ft. It is known for its remoteness and extreme weather. • The Absaroka- Beartooth Wilderness is the 6th largest wilderness area in the lower 48 states. • There are over 300 lakes and 10 major sub-alpine tundra plateaus in the Beartooths, with even more lakes across the Absaroka-Beartooth Wilderness. • At 3.96 billion years old, rock samples from the Beartooths are some of the oldest rocks on Earth. • The Beartooth Highway reaches an altitude of 10, 947 ft. and is often considered one of the most beautiful roads in America. 406-446-2103 ∙ 6811 Hwy 212, Red Lodge, MT 59068 You are camping in bear country. Wilderness Restrictions and Regulations The Beartooth Ranger District has an area of 587,000 acres. Of this, 345,000 acres are within the Absaroka-Beartooth Wilderness. The boundary of the Absaroka-Beartooth Wilderness continues west into the Gallatin National Forest (in all, the Absaroka-Beartooth Wilderness is 943,626 acres). General Use 15 people is the maximum group size 16 days at a camp site is the maximum camp stay limit No camping/campfires within 200 feet of a lake No camping/campfires within 100 feet of flowing water No use/possession of motorized vehicles, motorboats, chainsaws and other mechanized equipment Bicycles, wagons, carts, hang gliders or other mechanized equipment cannot be possessed or used Dispose of human waste properly. -
The University of Wyoming Board of Trustees' Report
THE UNIVERSITY OF WYOMING BOARD OF TRUSTEES’ REPORT September 6-8, 2007 The Final Report can be found on the University of Wyoming Board of Trustees website at www.uwyo.edu/trustees/meetings University of Wyoming Mission Statement (April 2002) The University of Wyoming aspires to be one of the nation’s finest public land-grant research universities, dedicated to serving as a statewide resource for accessible and affordable higher education of the highest quality, rigorous scholarship, technology transfer, economic and community development, and responsible stewardship of our cultural, historical, and natural resources. In the exercise of our primary mission to teach and educate students, we seek to provide academic and co-curricular opportunities that will: • Expose students to the frontiers of scholarship and creative activity, and the complexities of an interdependent world; • Ensure individual interactions among students, faculty, and staff; • Nurture an environment that values and manifests diversity, free expression, academic freedom, personal integrity, and mutual respect; and • Promote opportunities for personal growth, physical health, athletic competition, and leadership development for all members of the University community. As Wyoming’s only university, we are committed to outreach and service that extend our human talent and technological capacity to serve the people in our communities, our state, the nation, and the world. The primary vehicles for identifying the specific actions and resource allocations needed to achieve this complex mission are the University’s Academic Plan, Support Services Plan, and Capital Facilities Plan, each revised periodically. TRUSTEES OF THE UNIVERSITY OF WYOMING AGENDA September 6-8, 2007 Thursday, September 6, 2007 9:30 a.m.-11:45 p.m. -
Peter H. Griggs
STRATIGRAPHIC SIGNIFICANCE OF FOSSIL POLLEN AND SPORES OF THE CHUCKANUT FORMATION, NORTHWEST WASHINGTON Thosis far the Degree of. M. S. MICHIGAN STATE UNIVERSI'I’Y Peter H. Griggs 1965 ~-.. 'Wfi— wwWWL ‘1. .Illilllflu‘fllllf -Jnl.| IEI‘II‘I'IIIIVFI (II 'llllll‘lll.‘ I, l {III-III! I’lII 'II (III! III, [I , . III! [III [I I'll! (III. (I ABSTRACT STRATIGRAPHIC SIGNIFICANCE OF FOSSIL POLLEN AND SPORES OF THE CHUCKANUT FORMATION, NORTHWEST WASHINGTON by Peter H. Griggs The Chuckanut Formation, a series of strongly folded, terrestrial sandstones and shales, outcrops in northwestern Washington. The rocks have been previously assigned an age of Upper Cretaceous to lower Eocene based upon plant megafossils. The microfossil flora of the standard section along the east shore of Samish Bay was examined in order to determine the relationship of the Chuckanut to the Burrard (middle Eocene) of British Columbia. A zonation and envir- onmental interpretation of the standard section was desired for further refinement of the geological history of Tertiary rocks in the Pacific Northwest. Twenty—two samples, representing 9,H8u feet of section, were examined for palynomorphs. Data were collected for both relative frequency and stratigraphic analysis. Seventy— nine palynomorphs are described. The Samish Bay section is divided into three zones. The zonation is based on changes in the relative frequency f and the stratigraphic range of the palynomorphs. These ’ '_ ‘ V'II -7 r1 ' < P812631 ALL. '.,I I» ) I— (1 0'). OT changes were brought about by changing environmental and climatic conditions during the deposition of the rocks. An age of Paleocene to lower Eocene is assigned to the Samish Bay section. -
Geologic Map of the Red Lodge Area, Carbon
GEOLOGIC MAP OF THE RED LODGE AREA, CARBON COUNTY, MONTANA by David A. Lopez Montana Bureau of Mines and Geology Open-File Report MBMG 524 2005 This map has been reviewed for conformity with technical and editorial standards of the Montana Bureau of Mines and Geology. Partial support has been provided by the STATEMAP component of the National Cooperative Geologic Mapping Program of the U.S. Geological Survey under Contract Number 04HQAG0079. Kalispell MONTANA 15 Great Falls 90 Missoula Helena 94 Butte Billings Bozeman 90 90 15 110° 109° Big Timber YELLOWSTONE CO 94 Y Billings r 90 e r e l SWEET GRASS CO v l owsto e i n v R e Riv i r e 90 R e r ld u ne o to B ws STILLWATER CO lo Columbus el Y 45°30' e 78 n o r t ive 212 s R w r o te l a l w e ll Y ti S e h CARBON CO t BIG HORN CO f o Luther k STUDY r o Red Lodge 72 F AREA s rk la C 310 N PARK CO 212 45° 10 0 10 20 Miles Figure 1. Location map of the study area. 1 2 DESCRIPTION OF MAP UNITS SURFICIAL DEPOSITS af Artificial fill—Mine tailings and fill in the Rock Creek valley in northern part of the town of Red Lodge. Qal Alluvium (Holocene)—Gravel, sand, silt, and clay along active stream channels. Qc Colluvium (Holocene and Pleistocene)—Locally derived slope-wash depositsmainly of sand, silt, and clay. Typically thin veneer concealing bedrock, but locally as thick as 30 ft (9 m). -
Yellowstone National Park Geologic Resource Evaluation Scoping
Geologic Resource Evaluation Scoping Summary Yellowstone National Park This document summarizes the results of a geologic resource evaluation scoping session that was held at Yellowstone National Park on May 16–17, 2005. The NPS Geologic Resources Division (GRD) organized this scoping session in order to view and discuss the park’s geologic resources, address the status of geologic maps and digitizing, and assess resource management issues and needs. In addition to GRD staff, participants included park staff and cooperators from the U.S. Geological Survey and Colorado State University (table 1). Table 1. Participants of Yellowstone’s GRE Scoping Session Name Affiliation Phone E-Mail Bob Volcanologist, USGS–Menlo Park 650-329-5201 [email protected] Christiansen Geologist/GRE Program GIS Lead, NPS Tim Connors 303-969-2093 [email protected] Geologic Resources Division Data Stewardship Coordinator, Greater Rob Daley 406-994-4124 [email protected] Yellowstone Network Supervisory Geologist, Yellowstone Hank Heasler 307-344-2441 [email protected] National Park Geologist, NPS Geologic Resources Bruce Heise 303-969-2017 [email protected] Division Cheryl Geologist, Yellowstone National Park 307-344-2208 [email protected] Jaworowski Katie Geologist/Senior Research Associate, 970-586-7243 [email protected] KellerLynn Colorado State University Branch Chief, NPS Geologic Resources Carol McCoy 303-969-2096 [email protected] Division Ken Pierce Surficial Geologist, USGS–Bozeman 406-994-5085 [email protected] Supervisory GIS Specialist, Yellowstone Anne Rodman 307-344-7381 [email protected] National Park Shannon GIS Specialist, Yellowstone National Park 307-344-7381 [email protected] Savage Monday, May 16, involved a welcome to Yellowstone National Park and an introduction to the Geologic Resource Evaluation (GRE) Program, including status of reports and digital maps. -
VOLCANIC INFLUENCE OVER FLUVIAL SEDIMENTATION in the CRETACEOUS Mcdermott MEMBER, ANIMAS FORMATION, SOUTHWESTERN COLORADO
VOLCANIC INFLUENCE OVER FLUVIAL SEDIMENTATION IN THE CRETACEOUS McDERMOTT MEMBER, ANIMAS FORMATION, SOUTHWESTERN COLORADO Colleen O’Shea A Thesis Submitted to the Graduate College of Bowling Green State University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE August: 2009 Committee: James Evans, advisor Kurt Panter, co-advisor John Farver ii Abstract James Evans, advisor Volcanic processes during and after an eruption can impact adjacent fluvial systems by high influx rates of volcaniclastic sediment, drainage disruption, formation and failure of natural dams, changes in channel geometry and changes in channel pattern. Depending on the magnitude and frequency of disruptive events, the fluvial system might “recover” over a period of years or might change to some other morphology. The goal of this study is to evaluate the preservation potential of volcanic features in the fluvial environment and assess fluvial system recovery in a probable ancient analog of a fluvial-volcanic system. The McDermott Member is the lower member of the Late Cretaceous - Tertiary Animas Formation in SW Colorado. Field studies were based on a southwest-northeast transect of six measured sections near Durango, Colorado. In the field, 13 lithofacies have been identified including various types of sandstones, conglomerates, and mudrocks interbedded with lahars, mildly reworked tuff, and primary pyroclastic units. Subsequent microfacies analysis suggests the lahar lithofacies can be subdivided into three types based on clast composition and matrix color, this might indicate different volcanic sources or sequential changes in the volcanic center. In addition, microfacies analysis of the primary pyroclastic units suggests both surge and block-and-ash types are present. -
Yellowstone Wolf Project: Annual Report, 2009
YELLOWSTONE WOLFPROJECT ANNUAL REPORT 2009 Yellowstone Wolf Project Annual Report 2009 Douglas Smith, Daniel Stahler, Erin Albers, Richard McIntyre, Matthew Metz, Kira Cassidy, Joshua Irving, Rebecca Raymond, Hilary Zaranek, Colby Anton, Nate Bowersock National Park Service Yellowstone Center for Resources Yellowstone National Park, Wyoming YCR-2010-06 Suggested citation: Smith, D.W., D.R. Stahler, E. Albers, R. McIntyre, M. Metz, K. Cassidy, J. Irving, R. Raymond, H. Zaranek, C. Anton, N. Bowersock. 2010. Yellowstone Wolf Project: Annual Report, 2009. National Park Ser- vice, Yellowstone Center for Resources, Yellowstone National Park, Wyoming, YCR-2010-06. Wolf logo on cover and title page: Original illustration of wolf pup #47, born to #27, of the Nez Perce pack in 1996, by Melissa Saunders. Treatment and design by Renée Evanoff. All photos not otherwise marked are NPS photos. ii TABLE OF CON T EN T S Background .............................................................iv Wolf –Prey Relationships ......................................11 2009 Summary .........................................................v Composition of Wolf Kills ...................................11 Territory Map ..........................................................vi Winter Studies.....................................................12 The Yellowstone Wolf Population .............................1 Summer Predation ...............................................13 Population and Territory Status .............................1 Population Genetics ............................................14 -
Summits on the Air – ARM for USA - Colorado (WØC)
Summits on the Air – ARM for USA - Colorado (WØC) Summits on the Air USA - Colorado (WØC) Association Reference Manual Document Reference S46.1 Issue number 3.2 Date of issue 15-June-2021 Participation start date 01-May-2010 Authorised Date: 15-June-2021 obo SOTA Management Team Association Manager Matt Schnizer KØMOS Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged. Page 1 of 11 Document S46.1 V3.2 Summits on the Air – ARM for USA - Colorado (WØC) Change Control Date Version Details 01-May-10 1.0 First formal issue of this document 01-Aug-11 2.0 Updated Version including all qualified CO Peaks, North Dakota, and South Dakota Peaks 01-Dec-11 2.1 Corrections to document for consistency between sections. 31-Mar-14 2.2 Convert WØ to WØC for Colorado only Association. Remove South Dakota and North Dakota Regions. Minor grammatical changes. Clarification of SOTA Rule 3.7.3 “Final Access”. Matt Schnizer K0MOS becomes the new W0C Association Manager. 04/30/16 2.3 Updated Disclaimer Updated 2.0 Program Derivation: Changed prominence from 500 ft to 150m (492 ft) Updated 3.0 General information: Added valid FCC license Corrected conversion factor (ft to m) and recalculated all summits 1-Apr-2017 3.0 Acquired new Summit List from ListsofJohn.com: 64 new summits (37 for P500 ft to P150 m change and 27 new) and 3 deletes due to prom corrections. -
Thesis Winter Ecology of Bighorn Sheep In
THESIS WINTER ECOLOGY OF BIGHORN SHEEP IN YELLOWSTONE NATIONAL PARK Submitted by John L. 01demeyer In partial fulfillment of the requirements for the Degree of Master of Science Colorado State University December 1966 COLORADO STATE m~IVERSI1Y December 1966 WE HEREBY RECOl-lEEND 'lRAT lliE 'IHESIS PREPARED UNDER OUR SUPERVISION BY J onn L. 01demeyer ENTITLED tt'v-linter ecolo&;,( of bighorn sheep in yellowstone National ParkU BE ACCEPTED AS FULFILLING nus PART OF 'mE ~UIIill"LENTS FOR THE DillREE OF EASTER OF SCI~CE. CO:TJli ttee on Graduate Work --- - Examination Satisfacto~ Pennission to publish this thesis or any part of it must be obtained from the Dean of the Graduate School. PJL,ORADO STATE UN !VEKS ITY LI BRARIES i ABSTRACT WIN TER ECOLOOY OF ID:GHORN SHEEP IN YELLOVlS'IDHE NA TI ONAL PARK A bighorn sheep study was conducted on the northern winter range of yellowstone National Park, TNY01~inE from JIDle 1965 to June 1966. The objectives of the study were to census the bighorn population, map the winter bighorn distribution, detennine plant conposition and utilization on irnportant bighorn winter ranees, observe daily feedine habits, and assess the effect of competition on bighorn sheep. ~o hundred twen~ nine bighorn sheep wintered on the northern winter range. These herds were located on Nt. Everts, along the Yellowstone River, on Specimen Ridge, and along Soda Butte Creek. The ewe to ram ratio was 100: 78, the ewe to lamb ra tic waS 100: 47, and the ewe to yearling ratio was 100: 20. Range analysis was done on HacHinn Bench, Specimen Ridge, and Druid Peak. -
Pikes Peak Massif
Wild Connections Conservation Plan for the Pike & San Isabel National Forests Chapter 5 – Complexes: Area-Specific Management Recommendations This section contains our detailed, area-specific proposal utilizing the theme based approach to land management. As an organizational tool, this proposal divides the Pike-San Isabel National Forest into eleven separate Complexes, based on geo-physical characteristics of the land such as mountain ranges, parklands, or canyon systems. Each complex narrative provides details and justifications for our management recommendations for specific areas. In order to emphasize the larger landscape and connectivity of these lands with the ecoregion, commentary on relationships to adjacent non-Forest lands are also included. Evaluations of ecological value across public and private lands are used throughout this chapter. The Colorado Natural Heritage Programs rates the biodiversity of Potential Conservation Areas (PCAs) as General Biodiversity, Moderate, High, Very High, and Outranking Significance. The Nature Conservancy assesses the conservation value of its Conservation Blueprint areas as Low, Moderately Low, Moderate, Moderately High and High. The Southern Rockies Ecosystem Project's Wildlands Network Vision recommends land use designations of Core Wilderness, Core Agency, Low and Moderate Compatible Use, and Wildlife Linkages. Detailed explanations are available from the respective organizations. Complexes – Summary List by Watershed Table 5.1: Summary of WCCP Complexes Watershed Complex Ranger District