Characterization of Ecoregions of Idaho
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Geologic Mapping from Aerial Photography in the Boston Mountains, Northwestern Arkansas Mikel R
Journal of the Arkansas Academy of Science Volume 31 Article 31 1977 Geologic Mapping from Aerial Photography in the Boston Mountains, Northwestern Arkansas Mikel R. Shinn Follow this and additional works at: http://scholarworks.uark.edu/jaas Part of the Geomorphology Commons, and the Stratigraphy Commons Recommended Citation Shinn, Mikel R. (1977) "Geologic Mapping from Aerial Photography in the Boston Mountains, Northwestern Arkansas," Journal of the Arkansas Academy of Science: Vol. 31 , Article 31. Available at: http://scholarworks.uark.edu/jaas/vol31/iss1/31 This article is available for use under the Creative Commons license: Attribution-NoDerivatives 4.0 International (CC BY-ND 4.0). Users are able to read, download, copy, print, distribute, search, link to the full texts of these articles, or use them for any other lawful purpose, without asking prior permission from the publisher or the author. This Article is brought to you for free and open access by ScholarWorks@UARK. It has been accepted for inclusion in Journal of the Arkansas Academy of Science by an authorized editor of ScholarWorks@UARK. For more information, please contact [email protected], [email protected]. Journal of the Arkansas Academy of Science, Vol. 31 [1977], Art. 31 Geologic Mapping from AerialPhotography in The Boston Mountains, Northwest Arkansas MIKELR.SHINN Department of Geology, University ofArkansas Fayetteville, Arkansas 72701 ABSTRACT Aerial photography has been employed to map stratigraphic and structural features in the Boston Mountains of Washington and Crawford Counties, Arkansas. Exposures of resis- tant stratigraphic units within the lower Atoka Formation were delineated on a series of large scale aerial photographs over an area of about 150 square miles. -
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. -
Imaginative Geographies of Mars: the Science and Significance of the Red Planet, 1877 - 1910
Copyright by Kristina Maria Doyle Lane 2006 The Dissertation Committee for Kristina Maria Doyle Lane Certifies that this is the approved version of the following dissertation: IMAGINATIVE GEOGRAPHIES OF MARS: THE SCIENCE AND SIGNIFICANCE OF THE RED PLANET, 1877 - 1910 Committee: Ian R. Manners, Supervisor Kelley A. Crews-Meyer Diana K. Davis Roger Hart Steven D. Hoelscher Imaginative Geographies of Mars: The Science and Significance of the Red Planet, 1877 - 1910 by Kristina Maria Doyle Lane, B.A.; M.S.C.R.P. Dissertation Presented to the Faculty of the Graduate School of The University of Texas at Austin in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy The University of Texas at Austin August 2006 Dedication This dissertation is dedicated to Magdalena Maria Kost, who probably never would have understood why it had to be written and certainly would not have wanted to read it, but who would have been very proud nonetheless. Acknowledgments This dissertation would have been impossible without the assistance of many extremely capable and accommodating professionals. For patiently guiding me in the early research phases and then responding to countless followup email messages, I would like to thank Antoinette Beiser and Marty Hecht of the Lowell Observatory Library and Archives at Flagstaff. For introducing me to the many treasures held deep underground in our nation’s capital, I would like to thank Pam VanEe and Ed Redmond of the Geography and Map Division of the Library of Congress in Washington, D.C. For welcoming me during two brief but productive visits to the most beautiful library I have seen, I thank Brenda Corbin and Gregory Shelton of the U.S. -
Ecoregions of New England Forested Land Cover, Nutrient-Poor Frigid and Cryic Soils (Mostly Spodosols), and Numerous High-Gradient Streams and Glacial Lakes
58. Northeastern Highlands The Northeastern Highlands ecoregion covers most of the northern and mountainous parts of New England as well as the Adirondacks in New York. It is a relatively sparsely populated region compared to adjacent regions, and is characterized by hills and mountains, a mostly Ecoregions of New England forested land cover, nutrient-poor frigid and cryic soils (mostly Spodosols), and numerous high-gradient streams and glacial lakes. Forest vegetation is somewhat transitional between the boreal regions to the north in Canada and the broadleaf deciduous forests to the south. Typical forest types include northern hardwoods (maple-beech-birch), northern hardwoods/spruce, and northeastern spruce-fir forests. Recreation, tourism, and forestry are primary land uses. Farm-to-forest conversion began in the 19th century and continues today. In spite of this trend, Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and 5 level III ecoregions and 40 level IV ecoregions in the New England states and many Commission for Environmental Cooperation Working Group, 1997, Ecological regions of North America – toward a common perspective: Montreal, Commission for Environmental Cooperation, 71 p. alluvial valleys, glacial lake basins, and areas of limestone-derived soils are still farmed for dairy products, forage crops, apples, and potatoes. In addition to the timber industry, recreational homes and associated lodging and services sustain the forested regions economically, but quantity of environmental resources; they are designed to serve as a spatial framework for continue into ecologically similar parts of adjacent states or provinces. they also create development pressure that threatens to change the pastoral character of the region. -
The Eastern Africa Coastal Forests Ecoregion
The Eastern Africa Coastal Forests Ecoregion Strategic Framework for Conservation 2005 – 2025 Strategic Framework for Conservation (2005–2025) The Eastern Afrca Coastal Forests Ecoregon Strategc Framework for Conservaton 2005–2025 The Eastern Africa Coastal Forests Ecoregion Publshed August 2006 Editor: Kimunya Mugo Design and layout: Anthony Mwangi Cover design: Kimunya Mugo Front cover main photo: WWF-EARPO / John SALEHE Front cover other photos: WWF-UK / Brent STIRTON / Getty Images Back cover photo: WWF-EARPO / John SALEHE Photos: John Salehe, David Maingi and Neil Burgess or as credited. © Graphics (2006) WWF-EARPO. All rights reserved. The material and geographic designations in this report do not imply the expression of any opinion whatsoever on the part of WWF concerning the legal status of any country, territory or area or concerning the delimitation of its frontiers and boundaries. WWF Eastern Africa Regional Programme Office ACS Plaza, Lenana Road P.O. Box 62440-00200 Nairobi, Kenya Tel: +254 20 3877355, 3872630/1 Fax: +254 20 3877389 E-mail: [email protected] Web: www.panda.org/earpo Strategic Framework for Conservation (2005–2025) Contents Acknowledgements......................................................................................................... iv Foreword........................................................................................................................... v Lst of abbrevatons and acronyms.............................................................................. v A new approach to -
September 29, 2014 Land Management Plan Revision USDA
September 29, 2014 Land Management Plan Revision USDA Forest Service Ecosystem Planning Staff 1323 Club Drive Vallejo, CA 94592 Submitted via Region 5 website Re: Comments on Notice of Intent and Detailed Proposed Action for the Forest Plan Revisions on the Inyo, Sequoia and Sierra National Forests To the Forest Plan Revision Team: These comments are provided on behalf of Sierra Forest Legacy and the above conservation organizations. We have reviewed the Notice of Intent (NOI), detailed Proposed Action (PA), and supporting materials posted on the Region 5 planning website and offer the following comments on these documents. We have submitted numerous comment letters since the forest plan revision process was initiated for the Inyo, Sequoia, and Sierra national forests. Specifically, we submitted comment letters on the forest assessments for each national forest (Sierra Forest Legacy et al. 2013a, Sierra Forest Legacy et al. 2013b, Sierra Forest Legacy et al. 2013c), comments on two need for change documents (Sierra Forest Legacy et al. 2014a, Sierra Forest Legacy et al. 2014b) and comments on detailed desired conditions (Sierra Forest Legacy et al. 2014c). We incorporate these comments by reference and attach the letters to these scoping comments. We have included these letters in our scoping comments because significant issues that we raised in these comments have not yet been addressed in the NOI, or the detailed PA creates significant conflict with resource areas on which we commented. Organization of Comments The following comments address first the content of the NOI, including the purpose and need for action, issues not addressed in the scoping notice, and regulatory compliance of the PA as written. -
Flood Basalts and Glacier Floods—Roadside Geology
u 0 by Robert J. Carson and Kevin R. Pogue WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Information Circular 90 January 1996 WASHINGTON STATE DEPARTMENTOF Natural Resources Jennifer M. Belcher - Commissioner of Public Lands Kaleen Cottingham - Supervisor FLOOD BASALTS AND GLACIER FLOODS: Roadside Geology of Parts of Walla Walla, Franklin, and Columbia Counties, Washington by Robert J. Carson and Kevin R. Pogue WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Information Circular 90 January 1996 Kaleen Cottingham - Supervisor Division of Geology and Earth Resources WASHINGTON DEPARTMENT OF NATURAL RESOURCES Jennifer M. Belcher-Commissio11er of Public Lands Kaleeo Cottingham-Supervisor DMSION OF GEOLOGY AND EARTH RESOURCES Raymond Lasmanis-State Geologist J. Eric Schuster-Assistant State Geologist William S. Lingley, Jr.-Assistant State Geologist This report is available from: Publications Washington Department of Natural Resources Division of Geology and Earth Resources P.O. Box 47007 Olympia, WA 98504-7007 Price $ 3.24 Tax (WA residents only) ~ Total $ 3.50 Mail orders must be prepaid: please add $1.00 to each order for postage and handling. Make checks payable to the Department of Natural Resources. Front Cover: Palouse Falls (56 m high) in the canyon of the Palouse River. Printed oo recycled paper Printed io the United States of America Contents 1 General geology of southeastern Washington 1 Magnetic polarity 2 Geologic time 2 Columbia River Basalt Group 2 Tectonic features 5 Quaternary sedimentation 6 Road log 7 Further reading 7 Acknowledgments 8 Part 1 - Walla Walla to Palouse Falls (69.0 miles) 21 Part 2 - Palouse Falls to Lower Monumental Dam (27.0 miles) 26 Part 3 - Lower Monumental Dam to Ice Harbor Dam (38.7 miles) 33 Part 4 - Ice Harbor Dam to Wallula Gap (26.7 mi les) 38 Part 5 - Wallula Gap to Walla Walla (42.0 miles) 44 References cited ILLUSTRATIONS I Figure 1. -
ARKANSAS-BOSTON MOUNTAINS CHAPTER the Missouri & Louisiana Railroad
Volume 31, No. 5 January 2018 Official Monthly Publication of the ARKANSAS-BOSTON MOUNTAINS CHAPTER NATIONAL RAILWAY HISTORICAL SOCIETY Chapter No. 188 founded in 1987 2018 DIRECTORY OF OFFICERS President Bob Stark Vice President Al Kaeppel Secretary Malcolm Cleaveland Treasurer Tom Duggan Nominations Bill Merrifield National Director Ken Eddy Board Director Gary McCullah Editor Mike Sypult The Missouri & Louisiana Railroad - 1902-1914 M&L Mogul #114 builder photo at Baldwin Locomotive Works in August 1912. – John Dill collection Page 1 - THE ARKANSAS SCRAMBLER January 2018 The Missouri & Louisiana Railroad Arkansas well, a well-known Kansas City Banker. Stilwell was Branch already in the railroad business by this date and his By John Dill railroads all needed a reliable, relatively inexpensive supply of coal. Stilwell and his associates were then How do you write about a virtually unknown railroad in the process of assembling what would become the that does not fit well into any category that would nor- Kansas City, Pittsburg & Gulf Railroad, the predeces- mally be used to classify a railroad? The Missouri sor of the Kansas City Southern. Within only a few and Louisiana Railroad is the railroad in question. years, Central was heavily involved in the regional Have you ever heard of it? Few have. This article is coal business, mostly in Kansas and Missouri. Lum- as much an appeal to readers for information as a re- ber operations began near Texarkana in southern Ar- cital of the painfully limited knowledge of the author. kansas in January of 1894. A large amount of this Don’t get me wrong, the Missouri and Louisiana was lumber business soon became the production of rail- a very interesting, small but semi-important railroad in road ties and bridge timbers. -
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. -
Grasslands 4/16/03 3:46 PM
Ecoregion: Grasslands 4/16/03 3:46 PM Grasslands INTRODUCTION About 25% of Earth’s land surface is covered by temperate grassland. These large expanses of flat or hilly country cover much of North America, as well as large areas of Europe, Asia, and South America. Most grasslands are found in the interiors of continents, where there is too little rainfall for a forest but too much rain for a desert. Art Explosion Art Explosion Rolling hills covered with grasses and very few trees A few scattered trees are found on savannas, are typical of North American grassland prairies. tropical grasslands of Africa. Temperate grasslands have subtle differences and different names throughout the world. Prairies and plains of North America are grasslands with tall grasses, while the steppes of Russia are grasslands with short grasses. Veldts are found in South Africa, the puszta in Hungary, and the pampas in Argentina and Uruguay. Savannas are tropical grasslands that support scattered trees and shrubs. They often form a transitional biome file:///Ecoregion/grass/content.html Page 1 of 6 Ecoregion: Grasslands 4/16/03 3:46 PM between deserts and rain forests. Some temperate grasslands are also called savannas. The word savanna comes from the Spanish word zavanna, meaning “treeless plain.” Savannas cover almost half of Africa (mostly central Africa) and large areas of Australia and South America. ABIOTIC DATA The grassland climate is rather dry, averaging about 20 to 100 centimeters (8–40 inches) of precipitation a year. Summers are very hot and may reach 45°C (113°F). Winter temperatures often fall below freezing, which is 0°C (32°F). -
Fact Sheet- Central California Coast Ecoregion
California State Wildlife Action Plan (SWAP) 2015 Central California Coast Region Annual and Perennial Grassland Habitat About Our Region and the Grassland Habitat Annual grassland habitats are open grasslands composed primarily of annual plant species such as introduced annual grasses and forbs. Annual grasslands also occur as understory plants in Valley Oak Woodland and other habitats. Perennial grassland habitats occur as coastal prairie and interspersed within annual grasslands. Vernal pools also are an important habitat component of many grassland systems. The structure of grasslands depends upon prevailing weather patterns and grazing. A number of wildlife species spend their entire life within grasslands while others use grasslands for foraging and breeding. What are the sensitive species found in the grassland habitat? The following 32 grassland dependent species from this region are found to be sensitive: Amphibian [3] CALIFORNIA TIGER SALAMANDER WESTERN SPADEFOOT RED-LEGGED FROG Reptile [1] BLUNT-NOSED LEOPARD LIZARD Bird [15] BURROWING OWL NORTHERN HARRIER CALIFORNIA CONDOR OREGON VESPER SPARROW GIANT KANGAROO RAT PURPLE MARTIN GRASSHOPPER SPARROW SAND-HILL CRANE GOLDEN EAGLE SHORT-EARED OWL LOGGERHEAD SHRIKE SWAINSON’S HAWK LONG-BILLED CURLEW TRICOLORED BLACKBIRD MOUNTAIN PLOVER Mammal [13] BIG FREE-TAILED BAT PALLID SAN DIEGO POCKET MOUSE CALIFORNIA LEAF-NOSED BAT POCKETED FREE-TAILED BATRINGTAIL HOARY BAT SOUTHERN GRASSHOPPER MOUSE JACUMBA POCKET MOUSE SAN JOAQUIN KIT FOX LONG-EARED MYOTIS TOWNSEND BIG- EARED BAT MAINLAND -
Irrigation of Wi in Rapes
42 NO VEMBER/DECEMBER 2001 WINEGR OWING ative. The same can be said of a plant's water potential. For example, when more water is Irrigation lost from a leaf via transpiration than moves into the leaf from the vascular tissue, its water potential will become more negative due to a relative increase in its solute concentration. of w i rapes This is important as water in plants and soils moves from regions where water potential is relatively high to regions where water potential is rela- tively low. Such differences in water in potential will result in movement of water from cell to cell within a plant or from regions within the soil profile that Cal Lorry E. WIIIIams y.t portion of the growing season in contain more moisture to those with Department of Viticulture Enology these areas and vineyard water use less. University of California-Qavis, and can be greater than the soil's water One way to measure the water Kearney Agricultural Center reservoir after the winter rainfall, potential of a plant organ in the field supplemental irrigation of vineyards (such as a leaf) is by using a pressure SYNOPSIS: How much irrigation water is may be required at some point dur- chamber. required to grow quality winegrapes ing summer months. The leaf's petiole is cut and the leaf depends upon site, the stage of vine quickly placed into the chamber with growth, row spacing, size of the vine's IRRIGATION MANAGEMENT the cut end of the petiole protruding canopy, and amount of rainfall occur- No matter where grapevines are out of the chamber.