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Forests of Eastern Oregon: an Overview Sally Campbell, Dave Azuma, and Dale Weyermann
Forests of Eastern Oregon: An Overview Sally Campbell, Dave Azuma, and Dale Weyermann United States Forest Pacific Northwest General Tecnical Report Department of Service Research Station PNW-GTR-578 Agriculture April 2003 Revised 2004 Joseph area, eastern Oregon. Photo by Tom Iraci Authors Sally Campbell is a biological scientist, Dave Azuma is a research forester, and Dale Weyermann is geographic information system manager, U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station, 620 SW Main, Portland, OR 97205. Cover: Aspen, Umatilla National Forest. Photo by Tom Iraci Forests of Eastern Oregon: An Overview Sally Campbell, Dave Azuma, and Dale Weyermann U.S. Department of Agriculture Forest Service Pacific Northwest Research Station Portland, OR April 2003 State Forester’s Welcome Dear Reader: The Oregon Department of Forestry and the USDA Forest Service invite you to read this overview of eastern Oregon forests, which provides highlights from recent forest inventories.This publication has been made possible by the USDA Forest Service Forest Inventory and Analysis (FIA) Program, with support from the Oregon Department of Forestry. This report was developed from data gathered by the FIA in eastern Oregon’s forests in 1998 and 1999, and has been supplemented by inventories from Oregon’s national forests between 1993 and 1996.This report and other analyses of FIA inventory data will be extremely useful as we evaluate fire management strategies, opportunities for improving rural economies, and other elements of forest management in eastern Oregon.We greatly appreciate FIA’s willingness to work with the researchers, analysts, policymakers, and the general public to collect, analyze, and distrib- ute information about Oregon’s forests. -
Northwest Newsletter Vol.58 No
TIME SENSITIVE MATERIAL TIME SENSITIVE 84403 S Ogden, UT 4500875S E Burchard,Tom Circulation Societies FederationMineralogical of Northwest Northwest - 2913 Newsletter VOLUME 58, NO. 2 Northwest Federation of Mineralogical Societies FEB 2018 Keith Fackrell President GREETINGS Permit #7Permit McMinnville, McMinnville, OR PAID Postage U.S. Non February? It surely does not appear to be February, but looking at the Calendar it veri- - fies that it really is. Profit Org. I don’t recall any February’s being so dry and so warm for such a long time. It has been cold enough to be a little uncomfortable to do a lot of rock hunting (at least in my local area) so it is a good time to go to your rock pile and pick out some good rocks to cut and polish. It is also the time of year to pre- pare for the upcoming shows. There are many Gem & Mineral Shows on the horizon. Check the listing in your Northwest Federation of Mineralogical Societies (NFMS) Newsletter. If you are traveling beyond the boundaries of NFMS, you can check on the internet for Rock & Gem listing of many shows in any part of the United States. You can enhance your vacation and meet new friends by attending some of the shows wherever you travel. Now, I am asking for your help! I am asking for the NFMS Delegate or the President of your club/Society in the NFMS to make a list consisting of each member in your club/Society who has passed away in the last year since January 1, 2017 to the Present time, along with respective death dates. -
RMSH August 2012 Newsletter.Pdf
VOLUME 47, NO. 8 A UGUST 2012 CHALCEDONY MEETING BY D EAN S AKABE Wednesday This month’s topic is the most worked I call a stone Chalcedony, when it is sort of upon stone in any lapidary operation, translucent and homogeneous in color. August 22 Chalcedony . Chalcedony in a cryptocrys- Such as the Malawi Blue Chalcedony. 6:15-8:00 pm talline form of silica, composed of very Makiki District fine intergrowths of Quartz and Moganite. These are both silica minerals, which differ Park in the respect that quartz has a trigonal Administration crystal structure, while moganite is mono- Building clinic. Chalcedony's standard chemical structure is SiO 2 (Silicon Dioxide). Chalcedony has a waxy luster and is usu- NEXT MONTH ally semitransparent or translucent. It can Wednesday assume a wide range of colors, with the Blue Lace Agate most common seen as white to gray, blue, September 26 or brown ranging from pale to nearly Flourite black. Agates are stones which usually have col- ored layers. These are colored layers of The name "chalcedony" comes from the differently colored layers of Chalcedony. LAPIDARY calcedonius Latin , from a translation from Such as the Blue Lace Agate or Holly Blue Every Thursday khalkedon. the Greek word Unfortu- Agate. 6:30-8:30pm natelly, a connection to the town of Chal- cedon, in Asia Minor could not be found, Forms of Chalcedony are found in all 50 Second-floor Arts but one can always be hopeful. state, occurring in many colors and color and Crafts Bldg combinations. Some of the better known To make things alittle confusing is that ones are: Makiki District Chalcedony and Agate are terms used al- Park most interchangeably, as both are forms of quartz and are both Silicon Dioxide. -
The Harney County Way Collaborative Summit May 2 – 3, 2018 | Lincoln Building Auditorium, Burns, OR
The Harney County Way Collaborative Summit May 2 – 3, 2018 | Lincoln Building Auditorium, Burns, OR The Harney County Way Collaborative Summit 2018 Linking Collaboration Efforts to Build a Best Harney County High Desert Partnership’s Mission Summit Vision The High Desert Partnership exists to cultivate collaboration and We believe this summit will provide a productive time for those support and strengthen diverse partners engaged in solving participating in collaborative work in Harney County to network, complex issues to advance healthy ecosystems, economic well- learn and look for opportunities to work together. Bringing together being and social vitality to ensure a thriving and resilient the collaborative initiatives will create synergy and the story of community. collaboration will reverberate in our community. The outcomes from this summit will lead to more resilient communities. Our Core Values o We believe in our collaborative process to address societal Goals of the Summit issues. o Increase the understanding of collaborative efforts in Harney o We believe in doing things right rather than right now. County. o We believe in recognizing the values of others. o Understand the links where initiatives can work together on o We believe in advocating for the process, not for outcomes. projects or programs. o We believe in taking a holistic approach: social, ecological and o Find the places for sharing resources. economic. o Grow the community's collaborative participation. o We believe that optimism is necessary to successfully address o Provide a venue for those in attendance to gain a better the challenges we face. understanding of the work of High Desert Partnership. -
Symposium on Agate and Cryptocrystalline Quartz
Symposium on Agate and Cryptocrystalline Quartz September 10 – 13, 2005 Golden, Colorado Sponsored by Friends of Mineralogy, Colorado Chapter; Colorado School of Mines Geology Museum; and U.S. Geological Survey 2 Cover Photos {top left} Fortification agate, Hinsdale County, Colorado, collection of the Geology Museum, Colorado School of Mines. Coloration of alternating concentric bands is due to infiltration of Fe with groundwater into the porous chalcedony layers, leaving the impermeable chalcedony bands uncolored (white): ground water was introduced via the symmetric fractures, evidenced by darker brown hues along the orthogonal lines. Specimen about 4 inches across; photo Dan Kile. {lower left} Photomicrograph showing, in crossed-polarized light, a rhyolite thunder egg shell (lower left) a fibrous phase of silica, opal-CTLS (appearing as a layer of tan fibers bordering the rhyolite cavity wall), and spherulitic and radiating fibrous forms of chalcedony. Field of view approximately 4.8 mm high; photo Dan Kile. {center right} Photomicrograph of the same field of view, but with a 1 λ (first-order red) waveplate inserted to illustrate the length-fast nature of the chalcedony (yellow-orange) and the length-slow character of the opal CTLS (blue). Field of view about 4.8 mm high; photo Dan Kile. Copyright of articles and photographs is retained by authors and Friends of Mineralogy, Colorado Chapter; reproduction by electronic or other means without permission is prohibited 3 Symposium on Agate and Cryptocrystalline Quartz Program and Abstracts September 10 – 13, 2005 Editors Daniel Kile Thomas Michalski Peter Modreski Held at Green Center, Colorado School of Mines Golden, Colorado Sponsored by Friends of Mineralogy, Colorado Chapter Colorado School of Mines Geology Museum U.S. -
The Native Trouts of the Genus Salmo of Western North America
CItiEt'SW XHPYTD: RSOTLAITYWUAS 4 Monograph of ha, TEMPI, AZ The Native Trouts of the Genus Salmo Of Western North America Robert J. Behnke "9! August 1979 z 141, ' 4,W \ " • ,1■\t 1,es. • . • • This_report was funded by USDA, Forest Service Fish and Wildlife Service , Bureau of Land Management FORE WARD This monograph was prepared by Dr. Robert J. Behnke under contract funded by the U.S. Fish and Wildlife Service, the Bureau of Land Management, and the U.S. Forest Service. Region 2 of the Forest Service was assigned the lead in coordinating this effort for the Forest Service. Each agency assumed the responsibility for reproducing and distributing the monograph according to their needs. Appreciation is extended to the Bureau of Land Management, Denver Service Center, for assistance in publication. Mr. Richard Moore, Region 2, served as Forest Service Coordinator. Inquiries about this publication should be directed to the Regional Forester, 11177 West 8th Avenue, P.O. Box 25127, Lakewood, Colorado 80225. Rocky Mountain Region September, 1980 Inquiries about this publication should be directed to the Regional Forester, 11177 West 8th Avenue, P.O. Box 25127, Lakewood, Colorado 80225. it TABLE OF CONTENTS Page Preface ..................................................................................................................................................................... Introduction .................................................................................................................................................................. -
Characterization of Ecoregions of Idaho
1 0 . C o l u m b i a P l a t e a u 1 3 . C e n t r a l B a s i n a n d R a n g e Ecoregion 10 is an arid grassland and sagebrush steppe that is surrounded by moister, predominantly forested, mountainous ecoregions. It is Ecoregion 13 is internally-drained and composed of north-trending, fault-block ranges and intervening, drier basins. It is vast and includes parts underlain by thick basalt. In the east, where precipitation is greater, deep loess soils have been extensively cultivated for wheat. of Nevada, Utah, California, and Idaho. In Idaho, sagebrush grassland, saltbush–greasewood, mountain brush, and woodland occur; forests are absent unlike in the cooler, wetter, more rugged Ecoregion 19. Grazing is widespread. Cropland is less common than in Ecoregions 12 and 80. Ecoregions of Idaho The unforested hills and plateaus of the Dissected Loess Uplands ecoregion are cut by the canyons of Ecoregion 10l and are disjunct. 10f Pure grasslands dominate lower elevations. Mountain brush grows on higher, moister sites. Grazing and farming have eliminated The arid Shadscale-Dominated Saline Basins ecoregion is nearly flat, internally-drained, and has light-colored alkaline soils that are Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and America into 15 ecological regions. Level II divides the continent into 52 regions Literature Cited: much of the original plant cover. Nevertheless, Ecoregion 10f is not as suited to farming as Ecoregions 10h and 10j because it has thinner soils. -
Historical and Current Forest and Range Landscapes in the Interior
United States Department of Historical and Current Forest Agriculture Forest Service and Range Landscapes in the Pacific Northwest Research Station United States Interior Columbia River Basin Department of the Interior and Portions of the Klamath Bureau of Land Management General Technical and Great Basins Report PNW-GTR-458 September 1999 Part 1: Linking Vegetation Patterns and Landscape Vulnerability to Potential Insect and Pathogen Disturbances Authors PAUL F. HESSBURG is a research plant pathologist and R. BRION SALTER is a GIS analyst, Pacific Northwest Research Station, Forestry Sciences Laboratory, 1133 N. Western Avenue, Wenatchee, WA 98801; BRADLEY G. SMITH is a quantitative ecologist, Pacific Northwest Region, Deschutes National Forest, 1645 Highway 20 E., Bend, OR 97701; SCOTT D. KREITER is a GIS analyst, Wenatchee, WA; CRAIG A. MILLER is a geographer, Wenatchee, WA; CECILIA H. McNICOLL was a plant ecol- ogist, Intermountain Research Station, Fire Sciences Laboratory, and is currently at Pike and San Isabel National Forests, Leadville Ranger District, Leadville, CO 80461; and WENDEL J. HANN was the regional ecologist, Northern Region, Intermountain Fire Sciences Laboratory, and is currently the National Landscape Ecologist stationed at White River National Forest, Dillon Ranger District, Silverthorne, CO 80498. Historical and Current Forest and Range Landscapes in the Interior Columbia River Basin and Portions of the Klamath and Great Basins Part 1: Linking Vegetation Patterns and Landscape Vulnerability to Potential Insect and Pathogen Disturbances Paul F. Hessburg, Bradley G. Smith, Scott D. Kreiter, Craig A. Miller, R. Brion Salter, Cecilia H. McNicoll, and Wendel J. Hann Interior Columbia Basin Ecosystem Management Project: Scientific Assessment Thomas M. -
Quicksilver Deposits in the Steens and Pueblo Mountains Southern Oregon
UNITED STATES DEPARTMENT OF THE INTERIOR Harold L. Ickes, Secretary GEOLOGICAL SURVEY W. C. Mendenhall, Director Bulletin 931-J QUICKSILVER DEPOSITS IN THE STEENS AND PUEBLO MOUNTAINS SOUTHERN OREGON BY CLYDE P. ROSS Strategic Minerals Investigations, 1941 (Pages 227-258) UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1942 For sale by the Superintendent of Documents, Washington, D. C. ------- Price 40 cents CONTENTS Page Abstract.................................................. 227 Introduction.............................................. 227 Location.............................................. 227 Scope of the report................................... 229 Acknowledgments....................................... 229 Topography................................................ 230 Geology................................................... 232 Pre-Tertiary rocks.................................... 232 Age............................................... 232 Tertiary volcanic rocks............................... 232 Age............................................... 235 Older alluvium........................................ 236 Quaternary alluvium................................... 237 Structure............................................. 237 Quicksilver deposits...................................... 240 Mineralogy............................................. 240 The lodes............................................. 244 Origin................................................ 246 Outlook.............................................. -
Regional Conservation Partnership Program Investing in Idaho
Regional Conservation Partnership Program Investing in Idaho Regional Conservation Partnership Program Created by the 2014 Farm Bill, the Regional Conservation Partnership Program (RCPP) is a partner- Idaho Projects to driven, locally-led approach to conservation. It offers new opportunities for USDA’s Natural Resources Date Conservation Service (NRCS) to harness innovation, welcome new partners to the conservation mission, and demonstrates the value and efficacy of voluntary, private lands conservation. Projects by Resource Concern In 2017, NRCS is investing up to $225 million in 88 projects that impact nearly every state in the nation, including three in Idaho. Since 2014, NRCS has invested more than $825 million in 286 high- 3 3 impact projects, bringing together more than 2,000 conservation partners who have invested an additional $1.4 billion. By 2018, NRCS and partners will have invested at least $2.4 billion. These projects are leading to cleaner and more abundant water, better soil and air quality, enhance wildlife habitat, more resilient and productive agricultural lands and stronger rural economies. 4 Water Quantity/Drought Water Quality Wildlife Habitat 10 Projects $26.3 million NRCS Investment 93 Partners Idaho RCPP Projects Existing RCPP Projects Year Title Funding Lead Partner Number of NRCS Pool Partners Investment 2016 Farmer's Cooperative Ditch Company Project State Farmer’s Cooperative Ditch 7 $500,000 Company 2016 Greater Spokane River Watershed National Spokane Conservation 21 $7.7 million Implementation District 2016 -
State Rocks Table.Pdf
GATOR GIRL ROCKS THE BEST EVER OFFICIAL STATE ROCK, GEM, MINERAL, FOSSIL, & DINOSAUR SUMMARY TABLE STATE ROCK/(STONE) GEM MINERAL FOSSIL DINOSAUR Basilosaurus cetoides Marble Star Blue Quartz Hematite ALABAMA [whale] 19691 19902 19673 19844 Jade Mammuthus primigenius Gold ALASKA [Nephrite Jade] [woolly mammoth] 1967 1968 1986 STATE ROCKS STATE – Araucarioxylon Turquoise arizonicum ARIZONA 1974 [petrified wood] 1988 Bauxite Diamond Quartz Crystal ARKANSAS 19675 19676 19677 1 Alabama, Act 69-755, Acts of Alabama, September 12, 1969. 2 Alabama, Act 90-203. Acts of Alabama, March 29, 1990. GATORGIRLROCKS.COM GATORGIRLROCKS.COM 3 Alabama, Act 67-503, Acts of Alabama, September 7, 1967. 4 Alabama, Act 84-66, Acts of Alabama, 1984. 5 Arkansas General Assembly 1967. 6 Arkansas General Assembly 1967. 7 Arkansas General Assembly 1967. ©Gator Girl Rocks (2012) – All Rights Reserved GATOR GIRL ROCKS THE BEST EVER OFFICIAL STATE ROCK, GEM, MINERAL, FOSSIL, & DINOSAUR SUMMARY TABLE STATE ROCK/(STONE) GEM MINERAL FOSSIL DINOSAUR Smilodon californicus Serpentine Benitoite Native Gold CALIFORNIA 8 9 10 [saber-tooth cat] 1965 1985 1965 11 1973 Stegosaurus stenops Yule Marble Aquamarine Rhodochrosite COLORADO [dinosaur] 200412 197113 200214 198215 STATE ROCKS STATE Garnet Eubrontes Giganteus – CONNECTICUT [almandine garnet] [dinosaur tracks] 197716 1991 8 California Gov. Code § 425.2. Senate Bill 265 (Laws Chap. 89, Sec. 1) was signed by Govenor Brown on April 20, 1965. California designated the very first official state rock with this legislation (which also created the first official state mineral). 9 California State Legislature October 1, 1985. 10 California Gov. Code § 425.1. Senate Bill 265 (Laws Chap. 89, Sec. -
Quicksilver Deposits of Steens Mountain and Pueblo Mountains Southeast Oregon
Quicksilver Deposits of Steens Mountain and Pueblo Mountains Southeast Oregon GEOLOGICAL SURVEY BULLETIN 995-B A CONTRIBUTION TO ECONOMIC GEOLOGY QUICKSILVER DEPOSITS OF STEENS MOUNTAIN AND PUEBLO MOUNTAINS, SOUTHEAST OREGON By HOWEL WILLIAMS and ROBERT R. The object of this survey was to examine the quicksilver deposits with the hope of locating large tonnages of low-grade ore. The deposits occur in the south-central part of Harney County and are more than 100 miles from either Burns, Oreg., or Winuemucca, Nev., the nearest towns. The region is sparsely settled by stockmen; Fields, Denio, and Andrews are the only settlements. The range consisting of Steens Mountain and Pueblo Mountains is a dissected fault block, 90 miles long in a north-south direction and as much as 25 miles wide, tilted gently to the west. Pre-Tertiary rnetarnorphic and plutonic rocks occur at the southern end, but most of the block consists of Pliocene volcanic rocks. The major boundary faults on the east side of the range are concealed by alluvium. Minor northwestward-trending faults branch from them, their throws diminish ing toward the crest of the range; other minor fractures occur near, and parallel to, the mountain front. The quicksilver lodes were formed in and along these subsidiary fractures. The lodes occur in a more or less continuous belt just west of the eastern front of the range. They are steeply dipping and arranged in subparallel clusters, commonly standing out as resistant siliceous ribs against the softer kaolinized rocks that flank them. The lodes were formed in two hydrothermal stages, the first producing the reeflike masses of chalcedony and quartz with their halos of limonitic and calcitic clays and the second introducing silica and barite along with sulfides of iron, copper, and mercury.