Conservation Plan for the Closed Lakes Basin
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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 ........................................................................................................ -
Beatys Butte Herd Management Area Description
Beatys Butte Herd Management Area Lakeview District LOCATION: The area is located 65 miles east of Lakeview, Oregon. It is adjacent to and southeast of the Hart Mountain Antelope Refuge, is southeast of Catlow Valley, and bordered on the South by the Charles Sheldon National Antelope Refuge. ACREAGE: 437,120 acres of federal, state and privately owned land. ELEVATION/LANDMARKS: Beatys Butte, located in the north‐central part of the area is the most prominent landmark. It’s elevation of 7,885 feet above sea level makes it the highest point in the Lakeview Resource Area. There is a complex of smaller buttes surrounding Beatys Butte. TOPOGRAPHY/VEGETATION: Vegetation consists primarily of big sagebrush and bunch grasses. Low sagebrush communities are interspersed throughout the area. Topography varies from gently rolling hills to steep rugged hills and buttes with a number of broad valleys and shallow or dry lake beds. Slopes range from 0 to 60%. Precipitation averages 9 inches annually, mainly from winter snowfall. Summers are short, warm and dry while winters are typically long and cold. WILDLIFE: The area has a wide diversity of wildlife habitats and species including resident, migratory and nomadic populations. Large mammals include California bighorn sheep, pronghorn antelope and mule deer. Animals typical in the area are coyote, raven, red‐tail hawk, American kestrel, prairie falcon, turkey vulture, rough‐legged hawk, chukar partridge, valley quail, morning dove, Northern harrier, common crow, magpie, great horned owl, mountain lion, bobcat, Great Basin fence lizard and rattlesnake. Also, there are numerous small mammals and wetland birds. HERD SIZE: 100‐250 head. -
Caspian Tern Nesting Island Construction Draft Supplemental
Draft Supplemental Environmental Assessment (with Draft Amended FONSI) and Clean Water Act Section 404(b)(1) Alternatives Analysis Caspian Tern Nesting Island Construction Project Lower Klamath National Wildlife Refuge Siskiyou and Modoc Counties, California U.S. Army Corps of Engineers, Portland District June 2017 TABLE OF CONTENTS 1.0 Proposed Project 1.1 Proposed Project Description 1.2 Proposed Location 1.3 Purpose and Need for Proposed Action 1.4 Project Authority 2.0 Scope of Analysis 3.0 Proposed Action 3.1 Habitat Construction: Sheepy Lake in Lower Klamath NWR 3.1.1 Demolition and Disposal of Sheepy Floating Island 3.1.2 Sheepy Rock Island Design 3.1.3 Timing of Construction 3.1.4 Construction Methods 3.1.5 Access 3.1.6 Staging Area 3.1.7 Temporary Access Road 3.1.8 Maintenance Methods 3.1.9 Summary of Fill Requirements and Footprint 3.1.10 Post-Construction Monitoring 4.0 Alternatives 4.1 No Action Alternative 4.2 Repair the existing floating island 5.0 Impact Assessment 6.0 Summary of Indirect and Cumulative Effects 6.1 Indirect Effects 6.1.1 Caspian Terns 6.1.2 Fishes 6.1.3 Endangered and Threatened Species 6.1.4 Other Birds 6.1.5 Socioeconomic Effects 6.2 Cumulative Impacts 7.0 Environmental Compliance 8.0 Agencies Consulted and Public Notifications 9.0 Mitigation Measures 10.0 Draft Amended FONSI LIST OF FIGURES 1.1 Map of Tule Lake NWR and Lower Klamath NWR within the vicinity of Klamath Basin NWRs, Oregon and California 3.1 Sheepy Lake Floating Island Failure (1 of 3) 3.2 Sheepy Lake Floating Island Failure (2 of 3) 3.3 -
Research, Monitoring, and Evaluation of Avian Predation on Salmonid Smolts in the Lower and Mid‐Columbia River
Bonneville Power Administration, USACE – Portland District, USACE – Walla Walla District, and Grant County Public Utility District Research, Monitoring, and Evaluation of Avian Predation on Salmonid Smolts in the Lower and Mid‐Columbia River 2013 Draft Annual Report 1 2013 Draft Annual Report Bird Research Northwest Research, Monitoring, and Evaluation of Avian Predation on Salmonid Smolts in the Lower and Mid‐Columbia River 2013 Draft Annual Report This 2013 Draft Annual Report has been prepared for the Bonneville Power Administration, the U.S. Army Corps of Engineers, and the Grant County Public Utility District for the purpose of assessing project accomplishments. This report is not for citation without permission of the authors. Daniel D. Roby, Principal Investigator U.S. Geological Survey ‐ Oregon Cooperative Fish and Wildlife Research Unit Department of Fisheries and Wildlife Oregon State University Corvallis, Oregon 97331‐3803 Internet: [email protected] Telephone: 541‐737‐1955 Ken Collis, Co‐Principal Investigator Real Time Research, Inc. 52 S.W. Roosevelt Avenue Bend, Oregon 97702 Internet: [email protected] Telephone: 541‐382‐3836 Donald Lyons, Jessica Adkins, Yasuko Suzuki, Peter Loschl, Timothy Lawes, Kirsten Bixler, Adam Peck‐Richardson, Allison Patterson, Stefanie Collar, Alexa Piggott, Helen Davis, Jen Mannas, Anna Laws, John Mulligan, Kelly Young, Pam Kostka, Nate Banet, Ethan Schniedermeyer, Amy Wilson, and Allison Mohoric Department of Fisheries and Wildlife Oregon State University Corvallis, Oregon 97331‐3803 2 2013 Draft Annual Report Bird Research Northwest Allen Evans, Bradley Cramer, Mike Hawbecker, Nathan Hostetter, and Aaron Turecek Real Time Research, Inc. 52 S.W. Roosevelt Ave. Bend, Oregon 97702 Jen Zamon NOAA Fisheries – Pt. -
Conservation Status of Threatened Fishes in Warner Basin, Oregon
Great Basin Naturalist Volume 50 Number 3 Article 5 10-31-1990 Conservation status of threatened fishes in arnerW Basin, Oregon Jack E. Williams Division of Wildlife and Fisheries, Bureau of Land Management, Washington, D.C. Mark A. Stern The Nature Conservancy, Portland, Oregon Alan V. Munhall Bureau of Land Management, Lakeview, Oregon Gary A. Anderson Oregon Department of Fish and Wildlife, Lakeview, Oregon Follow this and additional works at: https://scholarsarchive.byu.edu/gbn Recommended Citation Williams, Jack E.; Stern, Mark A.; Munhall, Alan V.; and Anderson, Gary A. (1990) "Conservation status of threatened fishes in arnerW Basin, Oregon," Great Basin Naturalist: Vol. 50 : No. 3 , Article 5. Available at: https://scholarsarchive.byu.edu/gbn/vol50/iss3/5 This Article is brought to you for free and open access by the Western North American Naturalist Publications at BYU ScholarsArchive. It has been accepted for inclusion in Great Basin Naturalist by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. Creat &Isio N:l.luraUst 50(3), 1900, pp. 243-248 CONSERVATION STATUS OF THREATENED FISHES IN WARNER BASIN, OREGON 1 l 3 Jack E. Williams , MarkA. Stern \ Alan V. Munhall , and Cary A. Anderson"" A8S'TRACT.-Two fedemlJy listed fisbes, the Foskett speckled daceand Warnersucker, are endemic to Warner Basin in south central Oregon. The Foskett speckled dace is native only to a single spring in Coleman Valley. Anearby'spring was stocked with dace in 1979 and 1980, and now provides a second population. The present numbers ofdace probably are at their Wgbest levels since settlement ofthe region. -
Standards for Rangeland Health Assessment O'keeffe FRF
ee e_ O'KEEFFE FRF INDIVIDUAL ALLOTMENT #0203 Standards for Rangeland Health and Guidelines for Livestock Grazing Management (BLM, 1997) Introduction The Range Reform '94 Record of Decision (BLM, 1995a) recently amended current grazing administration and management practices. The ROD required that region-specific standards and guidelines be developed and approved by the Secretary of the Interior. In the State of Oregon, several Resource Advisory Councils (RACs) were established to develop these regional standards and guidelines. The RAC established for the part of the state covering the O'Keeffe FRF Individual Allotment is the Southeastern Oregon RAe. These standards and guidelines for Oregon and Washington were finalized on August 12, 1997 and include: Standard 1 - Upland Watershed Function Upland soils exhibit infiltration and permeability rates, moisture storage, and stability that are appropriate to soil, climate, and landform. • dard 2 - Riparian/Wetland Watershed Function • Riparian-wetland areas are in properly functioning physical condition appropriate to soil, climate, and landform. Standard 3 - Ecological Processes Healthy, productive, and diverse plant and animal populations and communities appropriate to soil, climate, and landform are supported by ecological processes of nutrient cycling, energy flow, and the hydrologic cycle. Standard 4 - Water Quality Surface water and groundwater quality, influenced by agency actions, complies with State water quality standards. Standard 5 - Native, T&E, and Locally Important Species Habitats support healthy, productive, and diverse populations and communities of native plants and animals (including special status species and species of local importance) appropriate to soil, climate, and landform. NDARD 1 - UPLAND WATERSHED CONDITION: Upland soils exhibit infiltration and permeability rates, moisture storage, and stability that are appropriate to soil, climate, and landform. -
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. -
Wilderness Study Areas
I ___- .-ll..l .“..l..““l.--..- I. _.^.___” _^.__.._._ - ._____.-.-.. ------ FEDERAL LAND M.ANAGEMENT Status and Uses of Wilderness Study Areas I 150156 RESTRICTED--Not to be released outside the General Accounting Wice unless specifically approved by the Office of Congressional Relations. ssBO4’8 RELEASED ---- ---. - (;Ao/li:( ‘I:I)-!L~-l~~lL - United States General Accounting OfTice GAO Washington, D.C. 20548 Resources, Community, and Economic Development Division B-262989 September 23,1993 The Honorable Bruce F. Vento Chairman, Subcommittee on National Parks, Forests, and Public Lands Committee on Natural Resources House of Representatives Dear Mr. Chairman: Concerned about alleged degradation of areas being considered for possible inclusion in the National Wilderness Preservation System (wilderness study areas), you requested that we provide you with information on the types and effects of activities in these study areas. As agreed with your office, we gathered information on areas managed by two agencies: the Department of the Interior’s Bureau of Land Management (BLN) and the Department of Agriculture’s Forest Service. Specifically, this report provides information on (1) legislative guidance and the agency policies governing wilderness study area management, (2) the various activities and uses occurring in the agencies’ study areas, (3) the ways these activities and uses affect the areas, and (4) agency actions to monitor and restrict these uses and to repair damage resulting from them. Appendixes I and II provide data on the number, acreage, and locations of wilderness study areas managed by BLM and the Forest Service, as well as data on the types of uses occurring in the areas. -
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. -
Coyote Lake Lahontan Cutthroat Trout
Oregon Native Fish Status Report – Volume II Coyote Lake Lahontan Cutthroat Trout Existing Populations Lahontan cutthroat trout populations in the Coyote Lakes basin are remnant of a larger population inhabiting pluvial Lake Lahontan during the Pleistocene era. Hydrologic access routes of founding cutthroat trout from Lake Lahontan basin into the Coyote Lakes basin have yet to be described (Coffin and Cowan 1995). The Coyote Lake Lahontan Cutthroat Trout SMU is comprised of five populations (Table 1). All populations express a resident life history strategy; however large individuals in the Willow and Whitehorse Complex populations suggest a migratory component may exist. Table 1. Populations, existence status, and life history of the Coyote Lake Lahontan Cutthroat Trout SMU. Exist Population Description Life History Yes Willow Willow Creek and tributaries. Resident / Migratory Yes Whitehorse Complex Whitehorse and Little Whitehorse Creeks, and Resident / Migratory tributaries. Yes Doolittle Doolittle Creek above barrier. Resident Yes Cottonwood Cottonwood Creek above barrier. Resident Yes Antelope Antelope Creek. Resident Lahontan cutthroat trout from Willow and Whitehorse creeks were transplanted into Cottonwood Creek in 1971 and 1980, and into Antelope Creek in 1972 (Hanson et al. 1993). Whether Lahontan cutthroat trout were present in these creeks prior to stocking activities is disputed (Behnke 1992, Hanson et al. 1993, Coffin and Cowan 1995, K. Jones, ODFW Research Biologist, Corvallis, OR personal communication). For the purpose of this review these populations are considered native. Lahontan cutthroat trout were also transplanted into Fifteenmile Creek above a natural barrier (Hanson et al. 1993), but they did not establish a self- sustaining population (ODFW Aquatic Inventory Project, unpublished data). -
Oregon Oregon Department of Geology and Mineral Industries Vicki S
State of Oregon Oregon Department of Geology and Mineral Industries Vicki S. McConnell, State Geologist USING AIRBORNE THERMAL INFRARED AND LIDAR IMAGERY TO SEARCH FOR GEOTHERMAL ANOMALIES IN OREGON 1 2 3 1 BY IAN P. MADIN , JOHN T. ENGLISH , PAUL A. FERRO , CLARK A. NIEWENDORP 2013 Oregon Department of Geology and Mineral Industries; 2, City of Hillsboro, Oregon; 3, Port of Portland, Oregon OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES, 800 NE OREGON STREET, #28, SUITE 965, PORTLAND, OR 97232 i DISCLAIMER This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. This report does not constitute a standard, specification, or regulation. This product is for informational purposes and may not have been prepared for or be suitable for legal, engineering, or surveying purposes. Users of this information should review or consult the primary data and information sources to ascertain the usability of the information. -
Climatic and Cultural Change in the Northern Great
CLIMATIC AND CULTURAL CHANGE IN THE NORTHERN GREAT BASIN: A GEOSPATIAL ANALYSIS OF NORTHERN SIDE-NOTCHED PROJECTILE POINTS FROM THE BURNS BUREAU OF LAND MANAGEMENT DISTRICT by JORDAN E. PRATT A THESIS Presented to the Department of Anthropology and the Robert D. Clark Honors College in partial fulfillment of the requirements for the degree of Bachelor of Arts June 2015 analyzed to determine significant site characteristics that are then compared to Northern Side-notched site characteristics as previously determined by John Fagan in 1974. Finally, ArcGIS is used to geospatially analyze the distribution of the projectile points throughout the Burn’s BLM District compared to known obsidian sources. By analyzing the distribution of projectile points and movement of materials across the landscape, as well as site attributes, insights can be made into prehistoric mobility and settlement patterns. iii Acknowledgements I would like to thank Dr. Patrick O’Grady for his unwavering support throughout this thesis, and his belief in me as an archaeologist. I would not be where I am today without his guidance, encouragement and support. I would also like to express my gratitude to Dr. C. Melvin Aikens, who stepped in and helped guide this thesis to completion. Additionally, I would like to express my gratitude to Dr. Terry Hunt, he has provided me with a wealth of opportunities and added a different perspective to this thesis. Thank you all for being willing mentors and teachers, I appreciate everything you have done for me, and the knowledge you have shared. Finally, I would like to thank everyone involved in the University of Oregon, Museum of Natural and Cultural History’s Archaeological Field School over the last three years.