Appendix E Wild and Scenic Rivers TABLE of CONTENTS
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Siltcoos Lake Nonpoint Source Implementation Grant: Water Quality Conditions and Nutrient Sources
Portland State University PDXScholar Center for Lakes and Reservoirs Publications and Presentations Center for Lakes and Reservoirs 3-2010 Siltcoos Lake Nonpoint Source Implementation Grant: Water Quality Conditions and Nutrient Sources Mark D. Sytsma Portland State University, [email protected] Rich Miller Portland State University, [email protected] Follow this and additional works at: https://pdxscholar.library.pdx.edu/centerforlakes_pub Part of the Environmental Indicators and Impact Assessment Commons, Environmental Monitoring Commons, and the Water Resource Management Commons Let us know how access to this document benefits ou.y Citation Details Sytsma, Mark D. and Miller, Rich, "Siltcoos Lake Nonpoint Source Implementation Grant: Water Quality Conditions and Nutrient Sources" (2010). Center for Lakes and Reservoirs Publications and Presentations. 52. https://pdxscholar.library.pdx.edu/centerforlakes_pub/52 This Report is brought to you for free and open access. It has been accepted for inclusion in Center for Lakes and Reservoirs Publications and Presentations by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. PORTLAND STATE UNIVERSITY, CENTER FOR LAKES AND RESERVOIRS Siltcoos Lake Nonpoint Source Implementation Grant Water quality conditions and nutrient sources Mark Sytsma and Rich Miller, Portland State University, Center for Lakes and Reservoirs 3/18/2010 Final report to the Oregon Department of Environmental Quality for project number W08714 Siltcoos Lake -
Some Recent Physical Changes of the Oregon Coast
rOREGON STATE UNIVERS TY LIBRARIES IIIIII 111IIIII1 IIII III 12 0002098016 65458 .8 05 cop .3 FINAL RE PORT (Report on an investigation carried out under Contract Nonr-2771 (04), Project NR 388-062, between the University of Oregon and the Office of Naval Research, U. S. Department of the Navy.) Reproduction in whole or in part is permitted for any purpose of the United States Government. SOME RECENT PHYSICAL CHANGES OF THE OREGON COAST by Samuel N. Dicken assisted by Carl L. Johannessen and Bill Hanneson Department of Geography University of Oregon Eugene, Oregon November 15, 1961 Reprinted in the public interest by the EugeneRegister-Guard and the Lane County Geographical Society,Inc., April, 1976. ACKNOWLEDGEMENTS The subject of coastal changes is of interest to many people living on or near the Oregon coast and, as a result, numerous interviews, only a few of which can be acknowledged, furnished much information not otherwise available. Valuable assistance came from persons concerned professionally with some aspect of coastal change. The staff of the U. S. Army Corps of Engineers, Portland District, was most helpful, especially H. A. Kidby of the Rivers and Harbors Section, Lloyd Ruff of the Geology Section, Mr. Charles Oros of the Photogrammetry Office and Dorothy McKean, Librarian. Mr. E. Olson of the U. S. Coast and Geodetic Survey located copies of old charts and other materials.Ralph Mason of the Oregon State Department of Geology and Mineral Industriescon- tributed notes on Ecola Park and other areas. Robert L. Brown and the staff of the U. S. Soil Conservation Service furnished photographs andspec- ific information on vegetation changes of the dunes.Park Snavely of the U. -
LANE COUNTY OREGON MULTI-JURISDICTION HAZARD MITIGATION PLAN Page | 46
3. RISK ASSESSMENT 44 CFR Requirement §201.6(c) (2) [The plan shall include] A risk assessment that provides the factual basis for activities proposed in the strategy to reduce losses from identified hazards. Local risk assessments must provide sufficient information to enable the jurisdiction to identify and prioritize appropriate mitigation actions to reduce losses from identified hazards The purpose of risk assessment is to identify and describe hazards that affect Lane County and analyze potential losses for human life and material assets. Through better understanding of potential hazards and the degree of risk they pose, more successful mitigation strategies can be developed and implemented. This risk assessment follows the four-step process described in the FEMA publication 386-2, Understanding Your Risks: Identifying Hazards and Estimating Losses, listed as follows: Step 1: Identify Hazards Step 2: Profile Hazard Events Step 3: Inventory Assets Step 4: Estimate Losses This section is organized into three subsections that address the four steps of the risk assessment process. 3.1 Identifying Hazards. This subsection addresses Step 1 and lists the hazards considered during the planning process and those ultimately profiled in the plan. It also describes methods, definitions and data sources used for the hazard identification and profile process. 3.2 Hazard Profile. This subsection addresses Step 2 and presents a detailed outline for each identified hazard. Each hazard profile is addressed as a plan subsection and includes a general description, affected geographic area, and discussion of previous occurrences, probability of future occurrence, magnitude and severity and an assessment of overall vulnerability to each hazard. -
Comprehensive Plan Is a General Plan for the Logical and Orderly Development of Dunes City Over the Years
CHAPTER I GOALS, POLICIES, RECOMMENDATIONS, AND PLAN IMPLEMENTATION October 10, 2013 INTRODUCTION A. Foreword This Comprehensive Plan is a general plan for the logical and orderly development of Dunes City over the years. There are reasons for writing it beyond the State requirements that each city and county in Oregon have a plan. There are already in existence building codes, zoning ordinances, health and safety codes, anti- pollution requirements, and many more laws that restrict what a person may do with their own property. These are necessary rules so that we can have some assurance of what our neighborhoods will generally be like in the future. Developers should be able to put the proper type of construction in the right place with the least damage to the environment. New citizens may be attracted by having some assurance of what their future surroundings will look like. Residents who are already here should gain confidence that their city will not deteriorate as has been the case in so many unplanned communities. The first section of the plan contains the policies that guide the city decision-makers. Following the policies are sections that contain inventory material that were used to develop the policies and a section on the history of Dunes City and the surrounding area. The original plan, adopted September 9, 1976, was put together by a group of area citizens with a variety of backgrounds. New members were appointed by the Mayor and the City Council at public meetings from a list of interested citizens. This Comprehensive Plan Advisory Committee met 24 times in 1974. -
Why Is the Project Needed, and What CHAPTER 1 Evidence Established These Needs?
OHV-Sand Camping Project Environmental Assessment Siuslaw National Forest South Zone District Lane, Douglas, and Coos Counties, Oregon Lead Agency: USDA Forest Service Responsible Official: Jose Linares, Forest Supervisor Siuslaw National Forest 4077 Research Way Corvallis, OR 97333 For Information Contact: Paul Thomas, South Zone Team Leader South Zone District 4480 Hwy. 101, Building G. Florence, Oregon 97439 (541) 902-6985 [email protected] The United States Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, sex, religion, age, disability, political beliefs, sexual orientation, or marital or family status. (Not all bases apply to all programs). Persons with disabilities who require alternative means for communication of program information (Braille, large print, audio tape, etc.) should contact USDA’s TARGET Center at (202) 720-2600 (voice and TDD). To file a complaint of discrimination, write USDA, Director, Office of Civil Rights, Room 326- W, Whitten Building, 1400 Independence Avenue SW, Washington, DC 20250-9410 or call (202) 720-5964 (voice or TDD). USDA is an equal opportunity provider and employer. OHV Sand Camping Project Comments received in response to this solicitation, including names and addresses of those who comment, will be considered part of the public record on this proposed action and will be available for public inspection. Comments submitted anonymously will be accepted and considered; however, those who only submit anonymous comments will not have standing to appeal the subsequent decision under 36 CFR part 215. Additionally, pursuant to 7 CFR 1.27 (d), any person may request the agency to withhold a submission from the public record by showing how the Freedom of Information Act (FOIA) permits such confidentiality. -
The Distribution, Substrate Selection and Sediment Displacement of Corophium Salmonis (Stimpson) and Corophitjm Spinicorne (Stimpson) on the Coast of Oregon
AN ABSTRACT OF THE THESIS OF JOSEPH EDWARD MCCARTHY for the DOCTOR OF PHILOSOPHY (Name) (Degree) inGeneral Science (Biologcal Science)presented on (Ma3) (Date Title: THE DISTRIBUTION, SUBSTRATE SELECTIONAND SEDI- MENT DISPLACEMENT OF COROPHIUMALMONIS (STIMPSON) AND COROPHIUM SPINICORNE (STIMPSON) ONTHE COAST OF OREGON Redacted for privacy Abstract approved: John H. rd, The arnphipbda, Corophiurn salmonis (Stimp son) andC. spinicorne (Stimpsori) were examined from three aspects.The first study involved the distribution and natural habitat of thesespecies on the Oregon coast.Sediments were sieved in an effort to detect the animalsFive areas were selected for prolonged examinationAni- mals were removed from these study areas in triplicate100cm2 sediment samples, counted and sexed.The seasonal average of ani- mals ranged from40/rn2to 3,300/rn2 dependingupon the area.Both species were found in freshwater(<40/00salinity) and in estuarine water up to10°/oo salinity (Cspinicorne) and 29°/oo salinity (C salmonis). Bothspeciesdisappearedinwintermonths,reoccurringinin- creasing numbers during spring months and reaching highestdensities in the summer. Under natural conditions C.salmonis was found most fre- quently in mud sediments while C. spinicorne occurred moreoften in sand.The males of the species were less numerous than thefemales. Evidence to date suggests that a behavioral difference onthe part of the males allows for selective predation.Both species formed bur- rows in sediments and tubes uponsubmerged surfaces. The second study was to determjne how specific theseanimals were in selecting substrates.The animals were exposed simultane- ously to their native sediments, acid-cleaned sand and a foreignmud or sand.The animals were removed from the sediments where they had established burrows and were tallied.These multiple choice experiments demonstrated that these species of Corophium can readily determine their native substrate. -
Thesis: Origin of the Coos Bay Dune Sheet, South Central Coast, Oregon
THESIS APPROVAL The abstract and thesis of Darren L. Beckstrand for the Master of Science in Geology presented November 22, 2000, and accepted by the thesis committee and the Department. COMMITTEE APPROVALS: _______________________________________ Curt D. Peterson, Chair _______________________________________ Errol C. Stock _______________________________________ Georg H. Grathoff _______________________________________ Virginia L. Butler Representative of the Office of Graduate Studies DEPARTMENTAL APPROVAL: _______________________________________ Ansel G. Johnson, Chair Department of Geology ABSTRACT An abstract of the thesis of Darren L. Beckstrand for the Master of Science in Geology presented November 22, 2000 Title: Origin of the Coos Bay and Florence Dune Sheets, South Central Coast, Oregon The Coos Bay and Florence dune sheets are situated on Oregon’s south central coast, between Florence to the north and Coos Bay to the south. These two dune sheets comprise approximately 70 km of coastline; the largest coastal dune fields of Oregon. Heavy mineral analysis indicates a primary sand source from the Umpqua River, as evidenced by high hypersthene:augite ratios and a secondary source from streams to the south, yielding metamorphic amphiboles. Complex directional emplacement trends indicate onshore transport of sand; however, different data suggest either a southern or a northern sand source. Dune lee- slope azimuth analyses suggest a northern sand source, whereas particle-size analysis indicates a southern source. Dune thickness and depth increase to the north. Accommodation space also increases to the north due to possible tectonic uplift to the south and incision by the paleo-Siuslaw River channel to the north. Previously, these dune sheets were assumed to be Holocene features forced onshore during the latest de-glacial sea level rise.