Chapter 3 Physical Environment Chapter 4 Biological Environment Chapter 5 Human Environment Maps Appendices Chapter 3 Physical Environment
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Oregon Historic Trails Report Book (1998)
i ,' o () (\ ô OnBcox HrsroRrc Tnans Rpponr ô o o o. o o o o (--) -,J arJ-- ö o {" , ã. |¡ t I o t o I I r- L L L L L (- Presented by the Oregon Trails Coordinating Council L , May,I998 U (- Compiled by Karen Bassett, Jim Renner, and Joyce White. Copyright @ 1998 Oregon Trails Coordinating Council Salem, Oregon All rights reserved. No part of this document may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording, or any information storage or retrieval system, without permission in writing from the publisher. Printed in the United States of America. Oregon Historic Trails Report Table of Contents Executive summary 1 Project history 3 Introduction to Oregon's Historic Trails 7 Oregon's National Historic Trails 11 Lewis and Clark National Historic Trail I3 Oregon National Historic Trail. 27 Applegate National Historic Trail .41 Nez Perce National Historic Trail .63 Oregon's Historic Trails 75 Klamath Trail, 19th Century 17 Jedediah Smith Route, 1828 81 Nathaniel Wyeth Route, t83211834 99 Benjamin Bonneville Route, 1 833/1 834 .. 115 Ewing Young Route, 1834/1837 .. t29 V/hitman Mission Route, 184l-1847 . .. t4t Upper Columbia River Route, 1841-1851 .. 167 John Fremont Route, 1843 .. 183 Meek Cutoff, 1845 .. 199 Cutoff to the Barlow Road, 1848-1884 217 Free Emigrant Road, 1853 225 Santiam Wagon Road, 1865-1939 233 General recommendations . 241 Product development guidelines 243 Acknowledgements 241 Lewis & Clark OREGON National Historic Trail, 1804-1806 I I t . .....¡.. ,r la RivaÌ ï L (t ¡ ...--."f Pðiräldton r,i " 'f Route description I (_-- tt |". -
Greater Harney Basin Agricultural Water Quality Management Area Plan
Greater Harney Basin Agricultural Water Quality Management Area Plan January 2020 Developed by the Oregon Department of Agriculture and the Greater Harney Basin Local Advisory Committee with support from the Harney Soil and Water Conservation District Oregon Department of Agriculture Harney SWCD Water Quality Program 530 Highway 20 South 635 Capitol St. NE Hines, OR 97738 Salem, OR 97301 Phone: (541) 573-5010 Phone: (503) 986-4700 Website: oda.direct/AgWQPlans (This page is blank) Table of Contents Acronyms and Terms .................................................................................................................................... i Foreword ........................................................................................................................................................ iii Required Elements of Area Plans ......................................................................................................... iii Plan Content.................................................................................................................................................. iii Chapter 1: Agricultural Water Quality Program ........................................................................ 1 1.1 Purpose of Agricultural Water Quality Program and Applicability of Area Plans...... 1 1.2 History of the Ag Water Quality Program .............................................................................. 1 1.3 Roles and Responsibilities ........................................................................................................ -
Timing of In-Water Work to Protect Fish and Wildlife Resources
OREGON GUIDELINES FOR TIMING OF IN-WATER WORK TO PROTECT FISH AND WILDLIFE RESOURCES June, 2008 Purpose of Guidelines - The Oregon Department of Fish and Wildlife, (ODFW), “The guidelines are to assist under its authority to manage Oregon’s fish and wildlife resources has updated the following guidelines for timing of in-water work. The guidelines are to assist the the public in minimizing public in minimizing potential impacts to important fish, wildlife and habitat potential impacts...”. resources. Developing the Guidelines - The guidelines are based on ODFW district fish “The guidelines are based biologists’ recommendations. Primary considerations were given to important fish species including anadromous and other game fish and threatened, endangered, or on ODFW district fish sensitive species (coded list of species included in the guidelines). Time periods were biologists’ established to avoid the vulnerable life stages of these fish including migration, recommendations”. spawning and rearing. The preferred work period applies to the listed streams, unlisted upstream tributaries, and associated reservoirs and lakes. Using the Guidelines - These guidelines provide the public a way of planning in-water “These guidelines provide work during periods of time that would have the least impact on important fish, wildlife, and habitat resources. ODFW will use the guidelines as a basis for the public a way of planning commenting on planning and regulatory processes. There are some circumstances where in-water work during it may be appropriate to perform in-water work outside of the preferred work period periods of time that would indicated in the guidelines. ODFW, on a project by project basis, may consider variations in climate, location, and category of work that would allow more specific have the least impact on in-water work timing recommendations. -
Predicting Foundation Bunchgrass Species Abundances: Model-Assisted Decision-Making in Protected-Area Sagebrush Steppe 1, 2 3 3 4 THOMAS J
#825 Predicting foundation bunchgrass species abundances: model-assisted decision-making in protected-area sagebrush steppe 1, 2 3 3 4 THOMAS J. RODHOUSE, KATHRYN M. IRVINE, ROGER L. SHELEY, BRENDA S. SMITH, SHIRLEY HOH, 5 5 DANIEL M. ESPOSITO, AND RICARDO MATA-GONZALEZ 1Upper Columbia Basin Network, National Park Service, 63095 Deschutes Market Road, Bend, Oregon 97701 USA 2Northern Rocky Mountain Science Center, United States Geological Survey, 2327 University Way, Suite 2, Bozeman, Montana 59715 USA 3Agricultural Research Service, United States Department of Agriculture, 67826-A, Highway 205, Burns, Oregon 97720 USA 4John Day Fossil Beds National Monument, National Park Service, 32651 Highway 19, Kimberly, Oregon 97848 USA 5Department of Animal and Rangeland Sciences, Oregon State University, Corvallis, Oregon 97331 USA Citation: Rodhouse, T. J., K. M. Irvine, R. L. Sheley, B. S. Smith, S. Hoh, D. M. Esposito, and R. Mata-Gonzalez. 2014. Predicting foundation bunchgrass species abundances: model-assisted decision-making in protected-area sagebrush steppe. Ecosphere 5(9):108. http://dx.doi.org/10.1890/ES14-00169.1 Abstract. Foundation species are structurally dominant members of ecological communities that can stabilize ecological processes and influence resilience to disturbance and resistance to invasion. Being common, they are often overlooked for conservation but are increasingly threatened from land use change, biological invasions, and over-exploitation. The pattern of foundation species abundances over space and time may be used to guide decision-making, particularly in protected areas for which they are iconic. We used ordinal logistic regression to identify the important environmental influences on the abundance patterns of bluebunch wheatgrass (Pseudoroegneria spicata), Thurber’s needlegrass (Achnatherum thurber- ianum), and Sandberg bluegrass (Poa secunda) in protected-area sagebrush steppe. -
A 1 Case-PR/ }*Rciofft.;Is Report
.A 1 case-PR/ }*rciofft.;is Report (a) This eruption site on Mauna Loa Volcano was the main source of the voluminous lavas that flowed two- thirds of the distance to the town of Hilo (20 km). In the interior of the lava fountains, the white-orange color indicates maximum temperatures of about 1120°C; deeper orange in both the fountains and flows reflects decreasing temperatures (<1100°C) at edges and the surface. (b) High winds swept the exposed ridges, and the filter cannister was changed in the shelter of a p^hoehoc (lava) ridge to protect the sample from gas contamination. (c) Because of the high temperatures and acid gases, special clothing and equipment was necessary to protect the eyes. nose, lungs, and skin. Safety features included military flight suits of nonflammable fabric, fuil-face respirators that are equipped with dual acidic gas filters (purple attachments), hard hats, heavy, thick-soled boots, and protective gloves. We used portable radios to keep in touch with the Hawaii Volcano Observatory, where the area's seismic activity was monitored continuously. (d) Spatter activity in the Pu'u O Vent during the January 1984 eruption of Kilauea Volcano. Magma visible in the circular conduit oscillated in a piston-like fashion; spatter was ejected to heights of 1 to 10 m. During this activity, we sampled gases continuously for 5 hours at the west edge. Cover photo: This aerial view of Kilauea Volcano was taken in April 1984 during overflights to collect gas samples from the plume. The bluish portion of the gas plume contained a far higher density of fine-grained scoria (ash). -
New Lunar Impact Melt Flows As Revealed by Mini-Rf on Lro
43rd Lunar and Planetary Science Conference (2012) 2388.pdf NEW LUNAR IMPACT MELT FLOWS AS REVEALED BY MINI-RF ON LRO. C. D. Neish1, N. Glines2, L. M. Carter3, V. J. Bray4, B. R. Hawke5, D. B. J. Bussey1, and the Mini-RF Science Team, 1The Johns Hopkins University Applied Physics Laboratory, Laurel, MD, 20723 ([email protected]), 2Mount Holyoke College, South Hadley, MA, 01075, 3NASA Goddard Spaceflight Center, Greenbelt, MD, 20770, 4The University of Ari- zona, Tucson, AZ, 85721, 5The University of Hawai’i at Manoa, Honolulu, HI, 96822. Introduction: Flow-like deposits of impact melt fying impact melts. After a candidate melt is identified, are commonly observed on the Moon, typically around data from the LRO Camera (LROC) was used to iden- young fresh craters. These flows are thought to be mix- tify additional features associated with impact melt tures of clasts and melted material that are emplaced deposits, such as cooling cracks in ponds and tension during the late stages of impact crater formation [1]. cracks in veneers, confirming these features as impact Lunar impact melts have been primarily studied at op- melts. tical wavelengths, but complementary information can be obtained by observing impact melts at radar wave- lengths. Radar data is sensitive to surface and sub- surface roughness, and thus can highlight these rough surface features, even when they not easily seen in optical data due to burial or imperfect lighting condi- tions (Fig. 1). Impact melts have been identified in radar data on the lunar near side [2], but they have yet to be studied in depth on the lunar far side, given the lack of global radar data prior to the launch of NASA’s Mini-RF instrument on the Lunar Reconnaissance Or- biter (LRO) in 2009. -
For the Love of Grass IX
For the Love of Grass IX Botanizing the Snake River Plains and Bonneville Lakebeds and Shorelines Jack Carlson, Wendall Oaks, Larry Holzworth, Dan Ogle, and Wendell Hassell May 10-15, 2016 Table of Contents Introduction ......................................................................................................................... 3 Day 1 – Monday, May 10 .................................................................................................... 5 Inventory Site 1 – Forage and Range Reseach Laboratory, Agricultural Research Service (ARS), Logan, Logan County, Utah ............................................................................. 5 Inventory Site 2 – Curlew National Grassland, Oneida County, Idaho ................................ 8 Day 2 – Tuesday, May 11 .................................................................................................. 13 Inventory Site 3 – Aberdeen Plant Materials Center (PMC), Natural Resources Conservation Service (NRCS), Bingham County, Idaho ...................................................... 13 Inventory Site 4 – Coffee Point, Bingham County, Idaho .................................................... 17 Day 3 – Wednesday, May 12 ............................................................................................ 21 Inventory Site 4A – Big Lost River Rest Area, Butte County, Idaho .................................. 21 Inventory Site 4B – Craters of the Moon National Monument, Butte County, Idaho ....... 22 Inventory Site 5 – Camas Prairie Centennial Marsh Wildlife -
International Ecological Classification Standard
INTERNATIONAL ECOLOGICAL CLASSIFICATION STANDARD: TERRESTRIAL ECOLOGICAL CLASSIFICATIONS Groups and Macrogroups of Washington June 26, 2015 by NatureServe (modified by Washington Natural Heritage Program on January 16, 2016) 600 North Fairfax Drive, 7th Floor Arlington, VA 22203 2108 55th Street, Suite 220 Boulder, CO 80301 This subset of the International Ecological Classification Standard covers vegetation groups and macrogroups attributed to Washington. This classification has been developed in consultation with many individuals and agencies and incorporates information from a variety of publications and other classifications. Comments and suggestions regarding the contents of this subset should be directed to Mary J. Russo, Central Ecology Data Manager, NC <[email protected]> and Marion Reid, Senior Regional Ecologist, Boulder, CO <[email protected]>. Copyright © 2015 NatureServe, 4600 North Fairfax Drive, 7th floor Arlington, VA 22203, U.S.A. All Rights Reserved. Citations: The following citation should be used in any published materials which reference ecological system and/or International Vegetation Classification (IVC hierarchy) and association data: NatureServe. 2015. International Ecological Classification Standard: Terrestrial Ecological Classifications. NatureServe Central Databases. Arlington, VA. U.S.A. Data current as of 26 June 2015. Restrictions on Use: Permission to use, copy and distribute these data is hereby granted under the following conditions: 1. The above copyright notice must appear in all documents and reports; 2. Any use must be for informational purposes only and in no instance for commercial purposes; 3. Some data may be altered in format for analytical purposes, however the data should still be referenced using the citation above. Any rights not expressly granted herein are reserved by NatureServe. -
Kadiworking Paper Finalcorrected
ACADEMY OF EUROPEAN LAW EUI Working Papers AEL 2009/10 ACADEMY OF EUROPEAN LAW CHALLENGING THE EU COUNTER-TERRORISM MEASURES THROUGH THE COURTS edited by Marise Cremona, Francesco Francioni and Sara Poli EUROPEAN UNIVERSITY INSTITUTE , FLORENCE ACADEMY OF EUROPEAN LAW ROBERT SCHUMAN CENTRE FOR ADVANCED STUDIES Challenging the EU Counter-terrorism Measures through the Courts EDITED BY MARISE CREMONA , FRANCESCO FRANCIONI AND SARA POLI EUI W orking Paper AEL 2009/10 This text may be downloaded for personal research purposes only. Any additional reproduction for other purposes, whether in hard copy or electronically, requires the consent of the author(s), editor(s). If cited or quoted, reference should be made to the full name of the author(s), editor(s), the title, the working paper or other series, the year, and the publisher. The author(s)/editor(s) should inform the Academy of European Law if the paper is to be published elsewhere, and should also assume responsibility for any consequent obligation(s). ISSN 1831-4066 © 2009 Marise Cremona, Francesco Francioni and Sara Poli (editors) Printed in Italy European University Institute Badia Fiesolana I – 50014 San Domenico di Fiesole (FI) Italy www.eui.eu cadmus.eui.eu Abstract This collection of papers examines the implications of the European Court of Justice’s approach to UN-related counter-terrorism measures against individuals (so-called ‘smart sanctions’), as expressed by its ruling in Case C-402/05P Kadi v Council and Commission , in which it annulled an EC act implementing a UN Security Council resolution. The impact of this seminal judgment on the EC legal order, on its relationship with the UN Charter, and on the case-law of the European Court of Human rights is the theme of this collection. -
Hydrology of Malheur Lake, Harney County, Southeastern Oregon J, ./J V
(200) WRi 7.3>-- ;:). , 3 1818 00029855 Hydrology of Malheur Lake, Harney County, southeastern Oregon J, ./J v- . S. GEOLOGI AL SURV EY / Water esOi:ifceTn vest iga tlo ns 2 1-75 • EP 2 3 1975 Prepared in cooperation with U. S. ARMY CORPS OF E GT EERS, Wall a Wall a Distri ct BI6LIOGR.I.PHIC DATA 11. Report No. 3. Re cipient' Accession No. SHEET 4. Title a nd Subtitle 5. Report Date HYDROLOG Y OF MALHEUR LAKE, HARNEY COUNTY, SOUTHEASTERN August 1975 OREGON 6. 7. Au thor(s ) 8. Performing Organization Rept. Larr y L. Hubbard o. USGS/WRI -21-7 5 9. Performing Organization Name and Address 10. Project/ Task/ Work Unit No. U.S. Geological Survey, Water Resources Division 830 NE. Holladay Street 11. Contra ct/ Grant No . Portland, Oregon 97232 12. Sponsoring Organization Name a nd Address 13. Type of Report & Period U.S . Geological Survey, Water Resources Division Covered 830 NE . Holladay Street Final Portland, Oregon 97232 14. 15. Supplementary orcs Prepared in cooperation with the U.S. Army Corps of Engineers, Walla Walla Distr ict 16. Ab rracrs The various components of inflow and outf low to and from the lake and their relative magnitudes were identified. In 1972 water year the total inf low to the lake was 200,000 acre - feet, but it was only 75 ,000 acre-feet in 1973 water year. In 1972 wa ter year the Donner und Blitzen River contr ibuted 55 percent of the inflow, with Silvies River , direct prec i pitation, and Sodhous e Spring contributing 28, 13, and 4 percent respectively. -
Final Report USDA Ecological Site Description State-And-Transition Models Major Land Resource Area 28A and 28B Nevada February 2015
Final Report USDA Ecological Site Description State-and-Transition Models Major Land Resource Area 28A and 28B Nevada February 2015 Tamzen K. Stringham1 Patti Novak-Echenique2 Paul Blackburn3 Cody Coombs4 Devon Snyder5 Amanda Wartgow6 Authors are 1Professor, 5,6Rangeland Ecologists, Dept. of Agriculture, Nutrition and Veterinary Sciences University of Nevada, Reno, NV, 2State Rangeland Management Specialist, USDA-NRCS Reno, NV, 3MLRA Soil Survey Leader, USDA-NRCS Elko, NV, and 4Hazardous Fuels Program Manager, BLM, Ely, NV Cite as: Stringham, T.K., P. Novak-Echenique, P. Blackburn, C. Coombs, D. Snyder, and A. Wartgow. 2015. Final Report for USDA Ecological Site Description State-and-Transition Models, Major Land Resource Area 28A and 28B Nevada. University of Nevada Reno, Nevada Agricultural džƉĞƌŝŵĞŶƚ^ƚĂƚŝŽŶ Research Report 2015-01. p. 1524. Cooperators: USDA Natural Resource Conservation Service, USDA Agricultural Research Service, USDI Bureau of Land Management and Eureka County, NV. Final Report submitted to USDA Agricultural Research Service as fulfillment of Agreement # 58-5370-2-211 Disturbance Response Group 4B Contents Page DRG 4B – Modal Site Claypan 12-14” 028BY037NV Ecological sites within DRG 4 Ϯϲϰ Narrative Ϯϲϱ Modal State-and-Transition model Ϯϴϭ References Ϯϴϯ Additional STMs within DRG 4 Ϯϴϲ 263 Ecological Sites within Disturbance Response Group 4B: Modal Site: Claypan 12-14” 028BY037NV Group Name Site ID Claypan 12-14"P.Z. 028BY037NV Claypan 14+" P.Z. 028BY036NV 4B Calcareous Claypan 14-16" P.Z. 028BY092NV Gravelly Claypan 14+" P.Z. 028BY035NV Cobbly Claypan 12-14" P.Z. 028BY039NV 264 MLRA 28B Group 4B Disturbance Response Group (DRG) 4B consists of five ecological sites. -
Diamond Craters Oregon's Geologic
Text by Ellen M. Benedict, 1985 Features at stops correspond to points on a clock ago, a huge mass of hot gases, volcanic ashes, bits face. Imagine that you are standing in the middle of a of pumice and other pyroclastics (fire-broken rock) Travel And Hiking Hints clock face. Twelve o’clock is the road in front of you violently erupted. The blast – greater than the May and 6 o’clock the road behind. If you always align the 18, 1980, eruption of Mt. St. Helens – deposited a Diamond Craters is located in the high desert country clock face with the road, you should be able to locate layer of pyroclastics 30 to 130 feet thick over an area about 55 miles southeast of Burns, Oregon. It’s an the features. almost 7,000 square miles! isolated place and some precautions should be taken . when traveling in the area. Start Tour. Mileage begins halfway Pyroclastics are between milepost 40 and 41 on State normal behavior Diamond Craters has no tourist facilities. The nearest Highway 205 at the junction to Diamond. for magmas place where gasoline is sold is at Frenchglen. Turn left. (subsurface That’s the opinion held by scores of molten rocks) Keep your scientists and educators who have visited Diamond, Oregon, a small ranching community, was of rhyolitic (a vehicle on named in 1874 for Mace McCoy’s Diamond brand. volcanic material and studied the area. It has the “best and hard-packed The nearby craters soon became known as Diamond related to granite) most diverse basaltic volcanic features in the road surfaces Craters.