The Vale Rangeland Rehabilitation Program: the Desert Repaired in Southeastern Oregon
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Outreach Notice FREMONT-WINEMA NATIONAL
Outreach Notice FREMONT-WINEMA NATIONAL FOREST District Ranger GS-0340-13 Winter Rim Zone Silver Lake and Paisley Ranger Districts The Position This position is responsible for the development, production, conservation, and utilization of natural resources on forest lands across the Winter Rim Zone of the Fremont-Winema National Forest. Duties include overseeing the inventorying, planning, evaluation, and management of the unit’s timber, soil, land, water, wildlife, fish, mineral, forage, wilderness, visual, and outdoor recreation resources in accordance with Forest Plan goals and requirements. Major project work is associated with the Sustained Yield Unit, Lakeview Collaborative Group, and Collaborative Forest Landscape Restoration. Direction is provided to subordinate programs engaged in work associated with the preparation of National Environmental Policy Act documentation, development of land-use strategies, management of multiple uses, and coordination of resource management planning activities. The incumbent serves as a key member of the Forest Leadership Team and contributes to the group’s formulation of Forest plans, polices, and objectives. Extensive effort is invested in establishing and maintaining cooperative relations with local, county, and state representatives; special interest and civic groups; private industry representatives; Tribal governments; permittees; and members of the general public. PLEASE NOTE: The purpose of this Outreach Notice is to determine the potential applicant pool for this position and to establish the appropriate recruitment method and area of consideration for the advertisement. (e.g., target grade or multi-grade and forest- wide, service-wide, region-wide, government-wide, or DEMO). Responses received from this outreach notice will be relied upon to make this determination. -
Mineral Resources of the Abert Rim Wilderness Study Area, Lake County, Oregon
Mineral Resources of the Abert Rim Wilderness Study Area, Lake County, Oregon U.S. GEOLOGICAL SURVEY BULLETIN 1738-C AVAILABILITY OF BOOKS AND MAPS OF THE U.S. GEOLOGICAL SURVEY Instructions on ordering publications of the U.S. Geological Survey, along with prices of the last offerings, are given in the cur rent-year issues of the monthly catalog "New Publications of the U.S. Geological Survey." Prices of available U.S. Geological Sur vey publications released prior to the current year are listed in the most recent annual "Price and Availability List" Publications that are listed in various U.S. Geological Survey catalogs (see back inside cover) but not listed in the most recent annual "Price and Availability List" are no longer available. Prices of reports released to the open files are given in the listing "U.S. Geological Survey Open-File Reports," updated month ly, which is for sale in microfiche from the U.S. Geological Survey, Books and Open-File Reports Section, Federal Center, Box 25425, Denver, CO 80225. Reports released through the NTIS may be obtained by writing to the National Technical Information Service, U.S. Department of Commerce, Springfield, VA 22161; please include NTIS report number with inquiry. Order U.S. Geological Survey publications by mail or over the counter from the offices given below. BY MAIL OVER THE COUNTER Books Books Professional Papers, Bulletins, Water-Supply Papers, Techniques of Water-Resources Investigations, Circulars, publications of general in Books of the U.S. Geological Survey are available over the terest (such as leaflets, pamphlets, booklets), single copies of Earthquakes counter at the following Geological Survey Public Inquiries Offices, all & Volcanoes, Preliminary Determination of Epicenters, and some mis of which are authorized agents of the Superintendent of Documents: cellaneous reports, including some of the foregoing series that have gone out of print at the Superintendent of Documents, are obtainable by mail from WASHINGTON, D.C.-Main Interior Bldg. -
First Presbyterian Church of Klamath Falls, Oregon
First Presbyterian Church of Klamath Falls, Oregon First Presbyterian Church of Klamath Falls (FPC) seeks a vibrant, outgoing, and loving Pastor who will be a joyful leader of our Church and an active member of our wonderful community. The Pastor will collaborate with the Elders and covenant part- ners of FPC to grow our congregation and to bring the good news of God’s Word to the people of the Klamath Basin FPC’s History and Programs First Presbyterian Church was founded on February 27, 1884, the first organized church in Klamath Falls and for 15 years the only house of worship in this southeastern Oregon pioneer town. From the beginning, FPC attracted pastors and people whose life’s goals were to teach, preach, uplift, and serve the community. At FPC’s 130-Year celebration in 2014, the mayor’s proclamation recognized our church’s critical role in providing rough-and-tumble pioneers who worked in the forests and fields with the “education, infrastructure and medical facilities and all the other elements that make a vibrant, caring community with strong values.” Our historic com- mitment to service remains in our church body’s culture and guides us to this day. FPC attracts regular weekly attendance of 210 between its contemporary and traditional Sunday service. FPC has 266 covenant partners as well as many regular attendees not yet formally affiliated with the church. Our Children’s Ministry helps children discover Christ as the adults in our congregation model our faith and invest in our children’s lives. We rejoice in the “joyful noises” as our children participate with us during our praise and worship time in the sanctuary on Sundays. -
Bird Notes from Southeastern Oregon and Northeastern California
194 Vol. XXI BIRD NOTES FROM SOUTHEASTERN OREGON AND NORTHEASTERN CALIFORNIA By GEORGE WILLETT WITH FIVE PHOTOS HE WRITER spent the greater part of the summer of 1918 at Malheur T Lake, Harney County, Oregon, in the interests of the United States Bio- logical Survey, and, while there, accumulated the bulk of the bird notes that make up this article. There will be found, however, a few additional items from other localities, principally from Clear Lake, Modoc County, California, and from the territory between Malheur Lake and Klamath Falls, the latter having been covered by auto in company with Dr. 0. W. Field and Mr. Stanley 11. Jewett, both of the Biological Survey. More than four months, from April 23 to August 27, were spentat’ Mal- heur Lake, so that the notes from that immediate section may be considered fairly complete for this season of the year, but those from other localities are more or less fragmentary. From April 4 to April 16 was spent at Clear Lake and, though quite a number of species of birds were observed at this time, some of the regular summer visitants had either not appeared at all or were present in small numbers at the date of my departure. The auto trip from Malheur Lake to Klamath Falls occupied nine days, from August 27 to September 4, inclusive. While on this trip we travelled almost continuously during daylighl hours and undoubtedly missed seeing many species of birds that were common in the country traversed.. The principal points touched at this time were Dia. -
Preliminary Plan of Development
Preliminary Plan of Development June 2010 Boardman to Hemingway Transmission Line Project Prepared By: Idaho Power Company 1221 West Idaho Street Boise, ID 83702 Preliminary Plan of Development Boardman to Hemingway Transmission Line Project Prepared By Idaho Power Company 1221 West Idaho Street Boise, ID 83702 June 2010 Preliminary Plan of Development Boardman to Hemingway Transmission Line Project Table of Contents 1 INTRODUCTION...............................................................................................................1-1 1.1 Background ..............................................................................................................1-2 2 PURPOSE AND NEED .....................................................................................................2-1 2.1 Project Proponent – Idaho Power ............................................................................2-1 2.2 Why is Idaho Power Proposing the B2H Project? ....................................................2-1 2.2.1 Federal Energy Regulatory Commission Requirements ..............................2-1 2.2.2 Idaho and Oregon Public Utility Commission Requirements........................2-2 2.2.3 Regional Planning Studies Identify the Need for B2H ..................................2-3 2.2.4 B2H Will Add Necessary Capacity and Improve Reliability ..........................2-4 2.3 The B2H Transmission Line Addresses Identified Needs........................................2-6 3 PROPOSED FACILITIES..................................................................................................3-1 -
Snake River Flow Augmentation Impact Analysis Appendix
SNAKE RIVER FLOW AUGMENTATION IMPACT ANALYSIS APPENDIX Prepared for the U.S. Army Corps of Engineers Walla Walla District’s Lower Snake River Juvenile Salmon Migration Feasibility Study and Environmental Impact Statement United States Department of the Interior Bureau of Reclamation Pacific Northwest Region Boise, Idaho February 1999 Acronyms and Abbreviations (Includes some common acronyms and abbreviations that may not appear in this document) 1427i A scenario in this analysis that provides up to 1,427,000 acre-feet of flow augmentation with large drawdown of Reclamation reservoirs. 1427r A scenario in this analysis that provides up to 1,427,000 acre-feet of flow augmentation with reservoir elevations maintained near current levels. BA Biological assessment BEA Bureau of Economic Analysis (U.S. Department of Commerce) BETTER Box Exchange Transport Temperature Ecology Reservoir (a water quality model) BIA Bureau of Indian Affairs BID Burley Irrigation District BIOP Biological opinion BLM Bureau of Land Management B.P. Before present BPA Bonneville Power Administration CES Conservation Extension Service cfs Cubic feet per second Corps U.S. Army Corps of Engineers CRFMP Columbia River Fish Mitigation Program CRP Conservation Reserve Program CVPIA Central Valley Project Improvement Act CWA Clean Water Act DO Dissolved Oxygen Acronyms and Abbreviations (Includes some common acronyms and abbreviations that may not appear in this document) DREW Drawdown Regional Economic Workgroup DDT Dichlorodiphenyltrichloroethane EIS Environmental Impact Statement EP Effective Precipitation EPA Environmental Protection Agency ESA Endangered Species Act ETAW Evapotranspiration of Applied Water FCRPS Federal Columbia River Power System FERC Federal Energy Regulatory Commission FIRE Finance, investment, and real estate HCNRA Hells Canyon National Recreation Area HUC Hydrologic unit code I.C. -
How to Contact Us: Spotter Field Guide
Joel Tannenholz Winter 2018-19 was wetter or much wetter than normal across most of southeast Oregon and southwest Idaho. Temperatures averaged over the three-month period were near normal, except in the Treasure Valley, which was a few degrees warmer than normal. Comparisons of average temperatures for December, January, and February showed a somewhat unusual pattern. January was warmer than December, which is normal. But February was slightly colder than January at most locations, which, on average, happens in only one year in ten. When should you call us? shifted into the west. Along with warmer air, westerly winds carried a series of Pacific weather systems inland. Most HAIL: pea size or larger. Several locations also observed their seasonal lows in February, which also happens in about one year in ten. Seasonal lows provided only light precipitation and breezy southeast to SNOW: 1” per hour or greater normally occur in December or January, but have been southwest winds. observed as early as October and as late as March. OR storm total 4”+ OR snow A record high temperature of 48 degrees was set at Baker City causing road closures. on the 18th , breaking the old record of 46 set in 1979. REDUCED VISIBILITY: for any A record snowfall of 3.4 inches was set at Boise on the 2nd , reason. breaking the old record of 2.8 inches set in 1948. Snowfall Reports (5 inches or more) WIND: Greater than 40 mph or damage. Date Amount Location HEAVY RAIN: ½”+ in 1 hour Dec 2 6” Boise 8-9“ Cascade FREEZING RAIN: Any 12” Idaho City 8” Table Rock amount. -
Palynology and Age of the Alvord Creek Formation, Steens Mountain, Southeastern Oregon Stephen F
Loma Linda University TheScholarsRepository@LLU: Digital Archive of Research, Scholarship & Creative Works Loma Linda University Electronic Theses, Dissertations & Projects 6-1984 Palynology and Age of the Alvord Creek Formation, Steens Mountain, Southeastern Oregon Stephen F. Barnett, Follow this and additional works at: https://scholarsrepository.llu.edu/etd Part of the Geology Commons, and the Paleobiology Commons Recommended Citation Barnett,, Stephen F., "Palynology and Age of the Alvord Creek Formation, Steens Mountain, Southeastern Oregon" (1984). Loma Linda University Electronic Theses, Dissertations & Projects. 542. https://scholarsrepository.llu.edu/etd/542 This Thesis is brought to you for free and open access by TheScholarsRepository@LLU: Digital Archive of Research, Scholarship & Creative Works. It has been accepted for inclusion in Loma Linda University Electronic Theses, Dissertations & Projects by an authorized administrator of TheScholarsRepository@LLU: Digital Archive of Research, Scholarship & Creative Works. For more information, please contact [email protected]. Abstract PALYNOLOGY A!\TD AGE OF THE ALVORD CREEK FORMATION, STEENS MOUNTAIN, SOUTHEASTERN OREGON by Stephen F. Barnett The age of the Alvord Creek Formation of Steens !fountain, south eastern Oregon, has been a center of controversy since Axelrod's 1944 paleobotanical assigm.icrLt of a Lower Pliocene age to the tuffaceous leaf-bearing shales. This date varies from earlier determinations by Chaney and MacGinitie that the flora was Mascall (Upper Miocene) equivalent. However, it is more sharply contradicted by the report of a Middle Miocene (Barstovian) fauna in the apparently overlying Steens Basalt and by a 21.3 m.y. radiometric date obtained on a basalt flow 61 meters above the leaf-bearing beds. -
Malheur River Basin TMDL and WQMP
Water Quality Report Malheur River Basin Total Maximum Daily Load (TMDL) and Water Quality Management Plan (WQMP) September 2010 Last Updated: 09/2010 DEQ 10-WQ-023 This report prepared by: Oregon Department of Environmental Quality 811 SW 6th Avenue Portland, OR 97204 1-800-452-4011 www.oregon.gov/deq Primary Authors: John Dadoly and Ryan Michie For more information contact: John Dadoly, Basin Coordinator 700 SE Emigrant Avenue, Suite 330 Pendleton, OR 97801 (541) 278-4616 [email protected] Cheryll Hutchens-Woods, Water Quality Manager Oregon Department of Environmental Quality 700 SE Emigrant Avenue, Suite 330 Pendleton, OR 97801 (541) 278-4619 [email protected] Eugene Foster, Manager of Watershed Management Section Oregon Department of Environmental Quality 811 SW 6th Avenue Portland, OR 97204 (503) 229-5325 [email protected] Malheur River Basin TMDL September 2010 Table of Contents Executive Summary Chapter 1 Introduction Chapter 2 Scope of TMDL Chapter 3 Basin Assessment Chapter 4 Pollutant Sources Chapter 5 Summary of Current and Past Pollution Control Efforts Chapter 6 Dissolved Oxygen, Chlorophyll a, pH, and Phosphorus Chapter 7 Bacteria Chapter 8 Pesticides Chapter 9 Temperature Water Quality Management Plan Appendix A Bacteria TMDL Technical Information Appendix B Temperature TMDL Technical Data Appendix C Baseline Beneficial Use Status of the Malheur River Basin Appendix D Quality Assurance Project Plan/Sample & Analysis Plan: Malheur River Basin TMDL Nutrient Water Quality Study -
AUTUMN SANDHILL CRANE MIGRATION in SOUTHEASTERN OREGON Carroll D
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln North American Crane Workshop Proceedings North American Crane Working Group 1992 AUTUMN SANDHILL CRANE MIGRATION IN SOUTHEASTERN OREGON Carroll D. Littlefield U.S. Fish and Wildlife Service, Malheur National Wildlife Refuge Follow this and additional works at: http://digitalcommons.unl.edu/nacwgproc Part of the Behavior and Ethology Commons, Biodiversity Commons, Ornithology Commons, Population Biology Commons, and the Terrestrial and Aquatic Ecology Commons Littlefield, Carroll D., "AUTUMN SANDHILL CRANE MIGRATION IN SOUTHEASTERN OREGON" (1992). North American Crane Workshop Proceedings. 290. http://digitalcommons.unl.edu/nacwgproc/290 This Article is brought to you for free and open access by the North American Crane Working Group at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in North American Crane Workshop Proceedings by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. 1 9 8 8 C R A N E W o R K S H o P AUTUMN SANDHILL CRANE MIGRATION IN SOUTHEASTERN OREGON lCARROLL D. LITILEFIELD, Malheur Field Station, He 72 Box 260, Princeton, OR 97721 Abstract: Each autumn, from 2,000 to 3,000 greater sandhill cranes (Grus canadensis tabi~) of the ~en tral Valley Population congregate on Malheur National Wildlife Refuge. Migratory behavIor, flock SIzes and arrivals and departures from this important autumn use area were observed for 13 years (1970-1986). Average size of flocks arriving from the north was 15.7, with those arriving from the southwest averag ing 7.4. Flocks departing for California wintering areas averaged 9.2, but as ~maller groups merged, fl?ck , sizes increased to 24.8 (35 km southwest from the departure area). -
Field-Trip Guide to the Vents, Dikes, Stratigraphy, and Structure of the Columbia River Basalt Group, Eastern Oregon and Southeastern Washington
Field-Trip Guide to the Vents, Dikes, Stratigraphy, and Structure of the Columbia River Basalt Group, Eastern Oregon and Southeastern Washington Scientific Investigations Report 2017–5022–N U.S. Department of the Interior U.S. Geological Survey Cover. Palouse Falls, Washington. The Palouse River originates in Idaho and flows westward before it enters the Snake River near Lyons Ferry, Washington. About 10 kilometers north of this confluence, the river has eroded through the Wanapum Basalt and upper portion of the Grande Ronde Basalt to produce Palouse Falls, where the river drops 60 meters (198 feet) into the plunge pool below. The river’s course was created during the cataclysmic Missoula floods of the Pleistocene as ice dams along the Clark Fork River in Idaho periodically broke and reformed. These events released water from Glacial Lake Missoula, with the resulting floods into Washington creating the Channeled Scablands and Glacial Lake Lewis. Palouse Falls was created by headward erosion of these floodwaters as they spilled over the basalt into the Snake River. After the last of the floodwaters receded, the Palouse River began to follow the scabland channel it resides in today. Photograph by Stephen P. Reidel. Field-Trip Guide to the Vents, Dikes, Stratigraphy, and Structure of the Columbia River Basalt Group, Eastern Oregon and Southeastern Washington By Victor E. Camp, Stephen P. Reidel, Martin E. Ross, Richard J. Brown, and Stephen Self Scientific Investigations Report 2017–5022–N U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior RYAN K. ZINKE, Secretary U.S. -
SOUTHEASTSOUTHEAST OREGON 234 Photographing Oregon Southeast Oregon 235
Owyhee Lake at Leslie Gulch Chapter 12 SOUTHEASTSOUTHEAST OREGON 234 Photographing Oregon Southeast Oregon 235 change quickly to howling winds. Unlike the western part of the state, there’s not much chance you’ll run into a bear out here, but it is definitely rattlesnake coun- try. It’s an area of sparse human population, and most of the people who live here like it that way. Cowboy is spoken here. A good way to begin your exploration of this fascinating part of the state is by traveling the Oregon Outback National Scenic Byway, breaking away from the Cascades and journeying south and east into the Great Basin via OR 31. Fort Rock Rising up out of surrounding sagebrush desert, Fort Rock is a towering jagged rock formation, technically a tuff ring, set in an ancient seabed. It is also perhaps the most famous anthropological site in Oregon, as a pair of 9,000–year old sagebrush bark sandals were discovered here. Trails lead up into the bowl of this crater-like formation, and you can scramble to the top for views of the surround- ing desert. Fort Rock has been designated a National Natural Landmark, and an Oregon State Parks interpretive display at the base of the rock does a good job of Lone tree in Harney Valley ranch country near Burns relating the natural and human history of the area. The town of Fort Rock has a museum with several pioneer-days buildings that have good potential for ghost town-like photographs. Hours and access are SOUTHEAST OREGON limited so you can’t get the best angles during the golden hours, but it is possible to make some nice images from the parking area at those times.