Medford's Messenger Quarterly Planning Update, Winter 2018
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Play Fairway Analysis of the Central Cascades Arc-Backarc Regime, Oregon: Preliminary Indications
GRC Transactions, Vol. 39, 2015 Play Fairway Analysis of the Central Cascades Arc-Backarc Regime, Oregon: Preliminary Indications Philip E. Wannamaker1, Andrew J. Meigs2, B. Mack Kennedy3, Joseph N. Moore1, Eric L. Sonnenthal3, Virginie Maris1, and John D. Trimble2 1University of Utah/EGI, Salt Lake City UT 2Oregon State University, College of Earth, Ocean and Atmospheric Sciences, Corvallis OR 3Lawrence Berkeley National Laboratory, Center for Isotope Geochemistry, Berkeley CA [email protected] Keywords Play Fairway Analysis, geothermal exploration, Cascades, andesitic volcanism, rift volcanism, magnetotellurics, LiDAR, geothermometry ABSTRACT We are assessing the geothermal potential including possible blind systems of the Central Cascades arc-backarc regime of central Oregon through a Play Fairway Analysis (PFA) of existing geoscientific data. A PFA working model is adopted where MT low resistivity upwellings suggesting geothermal fluids may coincide with dilatent geological structural settings and observed thermal fluids with deep high-temperature contributions. A challenge in the Central Cascades region is to make useful Play assessments in the face of sparse data coverage. Magnetotelluric (MT) data from the relatively dense EMSLAB transect combined with regional Earthscope stations have undergone 3D inversion using a new edge finite element formulation. Inversion shows that low resistivity upwellings are associated with known geothermal areas Breitenbush and Kahneeta Hot Springs in the Mount Jefferson area, as well as others with no surface manifestations. At Earthscope sampling scales, several low-resistivity lineaments in the deep crust project from the east to the Cascades, most prominently perhaps beneath Three Sisters. Structural geology analysis facilitated by growing LiDAR coverage is revealing numerous new faults confirming that seemingly regional NW-SE fault trends intersect N-S, Cascades graben- related faults in areas of known hot springs including Breitenbush. -
South Fork of Little Butte Creek Area Naming Proposals
South Fork of Little Butte Creek Area Naming Proposals Presented by Dr. Alice G. Knotts INTRODUCTION We begin by thanking the Oregon Geographic Names Board for its careful work exhibited and accomplished in recent years for naming geographical features in the State of Oregon. We have identified some physical features in the area of the South Fork of Little Butte Creek located in Jackson County and put forth name suggestions and proposals. We believe that most of them are located on public lands of the U.S. Forest Service or the BLM, but the Knotts Cliff is on private land. 1 Naming Proposals for the South Fork of Little Butte Creek Area Identified in geographic order of approach from Medford, the road up the South Fork of Little Butte Creek and the Soda Springs trail 1009 that follows upstream Dead Indian Creek that is proposed to be named Latgawa Creek. 1. Hole-in-the-Rock Name a rock arch located on top of a hill NW of Poole Hill. Hole-in-the-Rock has been recorded on a BLM map but not with GNIS. 2. Pilgrim Cave Name a rock shelf with ancient campfire smoked walls. A shelter for travelers for thousands of years. 3. Knotts Bluff Name a cliff that defines the northern side of a canyon through which runs the S. Fork of Little Butte Creek. 4. Ross Point Name a prominent point on Knotts Cliff above the cave. 5. Latgawa Pinnacles Name a group of rocky pinnacles located near Camp Latgawa. 6. Marjorie Falls Name a water slide on Latgawa Creek upstream from the soda springs. -
Temperatures Cool by Shading the Stream from Solar Radiation. These
Chapter 3 Affected Environment Conde Shell temperatures cool by shading the stream from solar radiation. These trees and shrubs also contribute nutrients to the system as coarse organic material that is crucial to the macroinvertebrate communities that support fish and other aquatic organisms. Large wood has been identified as a limiting factor in Dead Indian and Conde Creek systems.5 The effects of large wood on stream form and function are positive, creating pools, trapping sediment, providing cover for fish and other aquatic species, and stabilizing banks during high flow events. Beaver have historically contributed wood in the form of beaver dams, to these systems. Beaver dams are present in the upper section of Dead Indian but absent in Conde Creek. Two dams were observed on Dead Indian Creek, below the confluence with Conde Creek.6 South Fork of Little Butte Creek and tributaries have been identified by Department of Environmental Quality (DEQ) (1994) as water quality limited under Section 303(d) of the Clean Water Act. From the mouth to Beaver Dam Creek, South Fork of Little Butte Creek is water quality limited due to flow modification, habitat modification, sediment, and summer temperature. Dead Indian and Conde Creeks are limited by summer high temperatures, exceeding the maximum 7-day average for temperature (>64 F). Temperature monitors placed throughout Conde Creek and upper Dead Indian Creek during the summer of 1998 found water temperatures ranging from 65 - 77 F in late July. 7 The geology of an area plays an important role in describing fish habitat through the physical processes driving a system. -
Little Butte Creek Watershed Assessment
Little Butte Creek Watershed Assessment Little Butte Creek Watershed Council August 2003 Abstract The Little Butte Creek Watershed Assessment has been prepared for the Little Butte Creek Watershed Council with funding from the Oregon Watershed Enhancement Board (OWEB). The Assessment was prepared using the guidelines set forth in the Governor’s Watershed Enhancement Board’s 1999 Oregon Watershed Assessment Manual. The purpose of this document is to assess the current conditions and trends of human caused and ecologic processes within the Little Butte Creek Watershed and compare them with historic conditions. Many important ecological processes within the watershed have been degraded over the last 150 years of human activity. This Assessment details those locations and processes that are in need of restoration as well as those that are operating as a healthy system. The Assessment was conducted primarily at the 5th field watershed level, that of the entire Little Butte Creek Watershed. List and describe field watershed levels below. Where possible, the analyses was refined to the smaller 6th field watershed level, thirteen of which exist within the Little Butte Creek Watershed. The assessment also notes gaps in data and lists recommendations for future research and data collection. It is intended that this document, and the Little Butte Creek Watershed Action Plan be used as guides for future research and watershed protection and enhancement over the next decade. The document was developed using existing data. No new data was collected for this project. Where data was lacking, it was detailed for future work and study. Acknowledgements This assessment was compiled and written by Steve Mason. -
Crater Lake National Park Oregon
DEPARTMENT OF THE INTERIOR HUBERT WORK. SECRETARY NATIONAL PARK SERVICE STEPHEN T. MATHER. DIRECTOR RULES AND REGULATIONS CRATER LAKE NATIONAL PARK OREGON PALISADE POINT, MOUNT SCOTT IN THE DISTANCE 1923 Season from July 1 to September 30 THE PHANTOM SHIP. FISHING IS EXCELLENT IN CRATER LAKE. THE NATIONAL PARKS AT A GLANCE. [Number, 19; total area, 11,372 square miles.] Area in National parks in Distinctive characteristics. order of creation. Location. squaro miles. Hot Springs Middle Arkansas li 40 hot springs possessing curative properties- 1832 Many hotels and boarding houses—20 bath houses under public control. Yellowstone Northwestern Wyo 3.348 More geysers than in all rest of world together- 1872 ming. Boiling springs—Mud volcanoes—Petrified for ests—Grand Canyon of the Yellowstone, remark able for gorgeous coloring—Large lakes—Many largo streams and waterfalls—Vast wilderness, greatest wild bird and animal preserve in world— Exceptional trout fishing. Sequoia. Middle eastern Cali 252 The Big Tree National Park—several hundred 1S90 fornia. sequoia trees over 10 feet in diameter, some 25 to 36 feet, hi diameter—Towering mountain ranges- Startling precipices—Mile long cave of delicate beauty." Yosemito Middle eastern Cali 1,125 Valley of world-famed beauty—Lofty chits—Ro 1890 fornia. mantic vistas—Many waterfalls of extraordinary height—3 groves of big trees—High Sierra— Waterwhcol falls—Good trout fishing. General Grant Middle eastern Cali 4 Created to preserve the celebrated General Grant 1S90 fornia. Tree, 3* feet in diameter—6 miles from Sequoia National Park. Mount Rainier ... West central Wash 321 Largest accessible single peak glacier system—28 1899 ington. -
Inland Rogue Agricultural Water Quality Management Area Plan
Inland Rogue Agricultural Water Quality Management Area Plan Developed by the: Inland Rogue Local Advisory Committee Oregon Department of Agriculture With support from the: Jackson, Two Rivers, and Illinois Valley Soil and Water Conservation Districts February 28, 2018 Oregon Department of Agriculture Water Quality Program 635 Capitol Street NE Salem, Oregon 97301 Phone: (503) 986-4700 oda.direct/AgWQPlans Jackson SWCD 89 Alder St., Central Point, OR 97502 (541) 664-1070 https://jswcd.org/ Two Rivers (Josephine) SWCD 1440 Parkdale Drive, Grants Pass, OR 97527 (541) 474-6840 Illinois Valley SWCD PO Box 352 102 S Redwood Highway Cave Junction, OR 97523 (541) 592-3731 http://www.ivstreamteam.org/ Inland Rogue Agricultural Water Quality Management Area Plan February 6, 2018 Table of Contents Acronyms and Terms Used in this Document ............................................................................... i Foreword .................................................................................................................................................. ii Required Elements of Area Plans .................................................................................................... ii Plan Content ............................................................................................................................................ ii Chapter 1: Agricultural Water Quality Management Program Purpose and Background .......................................................................................................................................... -
Download Index
First Edition, Index revised Sept. 23, 2010 Populated Places~Sitios Poblados~Lieux Peuplés 1—24 Landmarks~Lugares de Interés~Points d’Intérêt 25—31 Native American Reservations~Reservas de Indios Americanos~Réserves d’Indiens d’Améreque 31—32 Universities~Universidades~Universités 32—33 Intercontinental Airports~Aeropuertos Intercontinentales~Aéroports Intercontinentaux 33 State High Points~Puntos Mas Altos de Estados~Les Plus Haut Points de l’État 33—34 Regions~Regiones~Régions 34 Land and Water~Tierra y Agua~Terre et Eau 34—40 POPULATED PLACES~SITIOS POBLADOS~LIEUX PEUPLÉS A Adrian, MI 23-G Albany, NY 29-F Alice, TX 16-N Afton, WY 10-F Albany, OR 4-E Aliquippa, PA 25-G Abbeville, LA 19-M Agua Prieta, Mex Albany, TX 16-K Allakaket, AK 9-N Abbeville, SC 24-J 11-L Albemarle, NC 25-J Allendale, SC 25-K Abbotsford, Can 4-C Ahoskie, NC 27-I Albert Lea, MN 19-F Allende, Mex 15-M Aberdeen, MD 27-H Aiken, SC 25-K Alberton, MT 8-D Allentown, PA 28-G Aberdeen, MS 21-K Ainsworth, NE 16-F Albertville, AL 22-J Alliance, NE 14-F Aberdeen, SD 16-E Airdrie, Can 8,9-B Albia, IA 19-G Alliance, OH 25-G Aberdeen, WA 4-D Aitkin, MN 19-D Albion, MI 23-F Alma, AR 18-J Abernathy, TX 15-K Ajo, AZ 9-K Albion, NE 16,17-G Alma, Can 30-C Abilene, KS 17-H Akhiok, AK 9-P ALBUQUERQUE, Alma, MI 23-F Abilene, TX 16-K Akiak, AK 8-O NM 12-J Alma, NE 16-G Abingdon, IL 20-G Akron, CO 14-G Aldama, Mex 13-M Alpena, MI 24-E Abingdon, VA Akron, OH 25-G Aledo, IL 20-G Alpharetta, GA 23-J 24,25-I Akutan, AK 7-P Aleknagik, AK 8-O Alpine Jct, WY 10-F Abiquiu, NM 12-I Alabaster, -
ECR Summary.Pdf
ISSUES AND CONCERNS AS RELATED TO EXISTING CONDITIONS Introduction The stakeholders who participated in the scoping process, through six four hour meetings, identified over 100 issues that were of concern to landowners, educators, conservationists, farmers, foresters, recreationists, and agency representatives. These issues were categorized into fourteen groups, and from these, the Watershed Advisory Committee (WAC) defined the top ten issues and concerns for the watershed. Please note that the numbers in parentheses after each issue/concern correspond to the order in which issues were raised. They are in no way intended to indicate rank or priority. These concerns were further refined for consensus on exact wording. The top ten issues are as follows: 1. Increased population over the last ten years in the canyon and surrounding areas, as well as future growth, has increased recreational pressures in the watershed without an increased infrastructure to accommodate the use. (Note: infrastructure has not kept up with the increase in population, i.e. the number of wardens.) 2. The decline of the fisheries mainly due to water diversions and lack of screening has resulted in Endangered Species Candidate listing for the spring run Chinook salmon leading to restrictions on Sport fishing and elimination of salmon and trout fishing, and could lead to further watershed-wide restrictions for multiple uses: agriculture, timber management, recreation, urban development, and property rights. 3. The current fuel load in the watershed is at an unacceptable level due to natural response and man- made interventions. 4. Inadequate timber management regulations and practices have potential impact on water quality. 5. -
Methods for Value of Watershed Restoration 2.2.12B
A Brief Economic Analysis of Watershed Restoration Investments: A Case Study of Southwestern Oregon This methodology report was prepared for the Whole Watershed Restoration Initiative and accompanies Ecotrust’s brochure: “The Restoration Economy: Investing in natural capital for the benefit of communities and salmon in Southwestern Oregon” Prepared by Ecotrust Taylor Hesselgrave, Economic Analyst Cathy Kellon, Water & Watersheds Program Director Kristen Sheeran, Ph.D. Updated May 15, 2012 721 NW 9th Ave, Suite 200 Portland, OR 97209 www.ecotrust.org Table of Contents ABOUT THE WWRI AND THIS STUDY ...................................................................................... 3 1. INTRODUCTION ................................................................................................................... 4 2. RESTORATION & THE LOCAL ECONOMY: Southwestern Oregon ................................ 2 2.1. Methods ............................................................................................................................. 2 2.2. Results ............................................................................................................................... 6 2.3. Single Project Analysis: The Rehabilitation of Little Butte Creek ....................................... 8 3. ADDITIONAL BENEFITS FROM RESTORATION ............................................................... 9 3.1. Non-Market Benefits Of Restoration ................................................................................ 10 3.2. The Value -
Interpreting the Timberline: an Aid to Help Park Naturalists to Acquaint Visitors with the Subalpine-Alpine Ecotone of Western North America
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 1966 Interpreting the timberline: An aid to help park naturalists to acquaint visitors with the subalpine-alpine ecotone of western North America Stephen Arno The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Arno, Stephen, "Interpreting the timberline: An aid to help park naturalists to acquaint visitors with the subalpine-alpine ecotone of western North America" (1966). Graduate Student Theses, Dissertations, & Professional Papers. 6617. https://scholarworks.umt.edu/etd/6617 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. INTEKFRETING THE TIMBERLINE: An Aid to Help Park Naturalists to Acquaint Visitors with the Subalpine-Alpine Ecotone of Western North America By Stephen F. Arno B. S. in Forest Management, Washington State University, 196$ Presented in partial fulfillment of the requirements for the degree of Master of Forestry UNIVERSITY OF MONTANA 1966 Approved by: Chairman, Board of Examiners bean. Graduate School Date Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. UMI Number: EP37418 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. -
Erosion Calderas: Origins, Processes, Structural and Climatic Control
Bull Volcanol (1999) 61:174–193 Q Springer-Verlag 1999 ORIGINAL PAPER D. KarÁtson 7 J.-C. Thouret 7 I. Moriya A. Lomoschitz Erosion calderas: origins, processes, structural and climatic control Received: 4 January 1998 / Accepted: 18 January 1999 Abstract The origin and development of erosion-mod- sion. The resulting landform should be classed as an ified, erosion-transformed, and erosion-induced de- erosion-induced volcanic depression if the degradation pressions in volcanic terrains are reviewed and syste- of a cluster of craters produces a single-drained, irregu- matized. A proposed classification, addressing termino- lar-shaped basin, or if flank erosion results in a quasi- logy issues, considers structural, geomorphic, and cli- closed depression. Under humid climates, craters and matic factors that contribute to the topographic modifi- calderas degrade at a faster rate. Mostly at subtropical cation of summit or flank depressions on volcanoes. and tropical ocean-island and island-arc volcanoes, Breaching of a closed crater or caldera generated by their erosion results in so-called amphitheater valleys volcanic or non-volcanic processes results in an outlet that develop under heavy rainfall (1F2500 mm/year), valley. Under climates with up to F2000–2500 mm an- rainstorms, and high-elevation differences. Structural nual rainfall, craters, and calderas are commonly and lithological control, and groundwater in ocean is- drained by a single outlet. The outlet valley can main- lands, may in turn preform and guide development of tain its dominant downcutting position because it high-energy valleys through rockfalls, landsliding, mud- quickly enlarges its drainage basin by capturing the flows, and mass wasting. -
Evaluation of Streamflow Records in Rogue River Basin, Oregon
GEOLOGICAL SURVEY CIRCULAR 187 \ EVALUATION OF STREAMFLOW RECORDS IN ROGUE RIVER BASIN, OREGON B!y Donald Rkhaideon UNITED STATES DEPARTMENT OF THE INTERIOR Oscar L. Chapman, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director GEOLOGICAL SURVEY CIRCULAR 187 EVALUATION OF STREAMFLOW RECORDS IN ROGUE RIVER BASIN, OREGON By Donald Richardson Washington, D. C., 1952 Free on application to the Geological Surrey, Washington 25, D. C. ' CONTENTS Page Page Abstract................................. 1 Syllabus of gaging-stations records--Con. Introduction............................. 1 Gaging-station records-Continued Purpose and Scope...................... 1 Rogue River Continued Acknowledgments........................ 1 Little Butte Creek at Lake Creek... 25 Physical features- of the basin........... 2 Little Butte Creek above Eagle Utilization of water in the basin........ 2 Point............................ 25 Water resources data for Rogue River basin 5 Little Butte Creek near Eagle Streamflow records ..................... 5 Point............................ 25 Storage reservoirs..................... 6 Little Butte Creek below Eagle Adequacy of data....................... 6 Point............................ 26 Syllabus of gaging-station records....... 13 Emigrant Creek (head of Bear Creek) Explanation of data .................... 13 near Ashland..................... 27 Gaging-station records................. 13 Emigrant Creek below Walker Creek, Rogue River above Bybee Creek........ 13 near Ashland..................... 28 Rogue River above