Detroit Lake and Big Cliff Lake, Oregon
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2019 Oregon Administrative Rules Compilation
2019 OREGON ADMINISTRATIVE RULES COMPILATION CHAPTER 736 Parks and Recreation Department Published By DENNIS RICHARDSON Secretary of State Copyright 2019 Office of the Secretary of State Rules effective as of January 01, 2019 DIVISION 1 PROCEDURAL RULES 736-001-0000 Notice of Proposed Rules 736-001-0005 Model Rules of Procedure 736-001-0030 Fees for Public Records DIVISION 2 ADMINISTRATIVE ACTIVITIES 736-002-0010 State Park Cooperating Associations 736-002-0015 Working with Donor Organizations 736-002-0020 Criminal Records Checks 736-002-0030 Definitions 736-002-0038 Designated Positions: Authorized Designee and Contact Person 736-002-0042 Criminal Records Check Process 736-002-0050 Preliminary Fitness Determination. 736-002-0052 Hiring or Appointing on a Preliminary Basis 736-002-0058 Final Fitness Determination 736-002-0070 Crimes Considered 736-002-0102 Appealing a Fitness Determination 736-002-0150 Recordkeeping, Confidentiality, and Retention 736-002-0160 Fees DIVISION 3 WILLAMETTE RIVER GREENWAY PLAN 736-003-0005 Willamette River Greenway Plan DIVISION 4 DISTRIBUTION OF ALL-TERRAIN VEHICLE FUNDSTO PUBLIC AND PRIVATELY OWNED LANDMANAGERS, ATV CLUBS AND ORGANIZATIONS 736-004-0005 Purpose of Rule 736-004-0010 Statutory Authority 736-004-0015 Definitions 736-004-0020 ATV Grant Program: Apportionment of Monies 736-004-0025 Grant Application Eligibility and Requirements 736-004-0030 Project Administration 736-004-0035 Establishment of the ATV Advisory Committee 736-004-0045 ATV Operating Permit Agent Application and Privileges 736-004-0060 -
A History of the Kokanee in Detroit Reservoir J. J
A HISTORY OF THE KOKANEE IN DETROIT RESERVOIR By J. J. Wetherbee, District Fishery Biologist Data on trapping and spawning by: W. C. Wingfield, Superintendent, Roaring River Hatchery Scale analysis by: F. H. Sumner, Scale analyst, Oregon Game Commission 1965 TABLE OF CONTENTS Page I. Introduction 1 II. Environment and Food Habits 1 III. Stocking 4 IV. Sport Fishery 5 V. Spawning Runs 7 VI. Egg-Take Operation 10 VII. Spawning Habits and Propagation 16 VIII. Age and Growth 19 IX. Future Outlook for Kokanee Populations in Detroit Reservoir 21 X. Considerations for Future Management of Kokanee 22 I INTRODUCTION Kokanee were originally stocked in Detroit Reservoir in 11959. This species was introduced in hopes that it would utilize pelagiczoo plankton and provide a more varied sport fishery. The trout fishery in the reservoir depends primarily on heavy plants of legal-sized rainbow trout, supplemented by stocking fingerling rainbow. As the introduction of the kokanee has been somewhat successful in this fluctuating impoundment, a compilation of all known biologi- cal data would be of interest and aid in the future management of this species. II ENVIRONMENT AND FOOD HABITS Detroit is a multi-purpose reservoir maintained by the Corps of Engineers and contains 3,580 surfaceacres at full pool and 1,250 acres at minimum pool. Elevation is 1,569 feet at full pool. An annual drawdown of about 1)40 feet is usually accomplished by December 1. The reservoir is normally maintained at full pool from May to SepteMber. As Detroit is subjected to extreme fluctuations and is character- ized by a steeply sloping shoreline, it cannot be classedas a productive water. -
Willamette Basin Review Feasibility Study
US Army Corps of Engineers Portland District Willamette Basin Review Feasibility Study DRAFT Integrated Feasibility Report and Environmental Assessment November 2017 Willamette Basin Review Feasibility Study Executive Summary The Willamette River basin is located entirely within the state of Oregon, beginning south of Cottage Grove, and extending approximately 187 miles to the north where the Willamette River flows into the Columbia River. The basin is more than 11,200 square miles, averages 75 miles in width, and encompasses approximately 12 percent of the total area of the state (Figure ES-1). Within the watershed are most of the state’s population (nearly 70 percent), larger cities, and major industries. The basin also contains some of Oregon’s most productive agricultural lands and supports nationally and regionally important fish and wildlife species. Thirteen of Oregon’s thirty-six counties intersect or lie within the boundary of the Willamette River basin. Through a series of Flood Control Acts the U.S. Congress authorized the U.S. Army Corps of Engineers (Corps) to construct, operate, and maintain thirteen major dams1 in the Willamette River basin. Collectively, these dams, reservoirs and associated infrastructure are known as the Willamette Valley Project (WVP). With a combined conservation storage capacity of approximately 1,590,000 acre-feet, the WVP is capable of providing important benefits for flood damage reduction, navigation, hydropower, irrigation, municipal and industrial water supply, flow augmentation for pollution abatement and improved conditions for fish and wildlife, and recreation. Feasibility Study History The Willamette Basin Review Feasibility Study began in 1996 to investigate future Willamette River basin water demand. -
WIN Quarterly: Summer 2020
WIN Quarterly: Summer 2020 Greetings, friends and colleagues, I hope you all had a relaxing weekend. It sure felt a little different, this year! The relative calm of the holiday gave me a chance to think about what Independence Day means to me, how that may differ from others and a chance to finish working through my thoughts about Juneteenth. We just declared Juneteenth a holiday at CPRCD and, considering current events, it felt weird to take a day off for the holiday. Ultimately, I did what many privileged white folk do and I donated some money to a charity and went about my day (HBCU Foundation). I instantly felt guilty and knew I needed to do better, so I'm working on that. When congress passed the Lee Resolution on July 2nd, 1776 I would bet that few foresaw another seven years of war with the British. Similarly, I can only imagine that people of color in the United States did not anticipate their fight to continue for another 155 years after Major General Gordon Granger read General Order No. 3 in Galveston on June 19th, 1865. For my whole life, I've celebrated an independence from a "tyranny" I never experienced. What I've really celebrated was my privilege. In fact, I would've been on the other side as my great grandfathers and great uncles were generals for the British Army; one of the former leading numerous decimations of the Americans during the Revolutionary War until being crushed at Yorktown; one of the latter leading the British to victory at the Battle of Alexandria. -
An Evaluation of Spring Chinook Salmon Reintroductions Above Detroit Dam, North Santiam River, Using Genetic Pedigree Analysis P
AN EVALUATION OF SPRING CHINOOK SALMON REINTRODUCTIONS ABOVE DETROIT DAM, NORTH SANTIAM RIVER, USING GENETIC PEDIGREE ANALYSIS Prepared for: U. S. ARMY CORPS OF ENGINEERS PORTLAND DISTRICT – WILLAMETTE VALLEY PROJECT 333 SW First Ave. Portland, Oregon 97204 Prepared by: Kathleen G. O’Malley1, Melissa L. Evans1, Marc A. Johnson1,2, Dave Jacobson1, and Michael Hogansen2 1Oregon State University Department of Fisheries and Wildlife Coastal Oregon Marine Experiment Station Hatfield Marine Science Center 2030 SE Marine Science Drive Newport, Oregon 97365 2Oregon Department of Fish and Wildlife Upper Willamette Research, Monitoring, and Evaluation Corvallis Research Laboratory 28655 Highway 34 Corvallis, Oregon 97333 SUMMARY For approximately two decades, hatchery-origin (HOR) spring Chinook salmon have been released (“outplanted”) above Detroit Dam on the North Santiam River. Here we used genetic parentage analysis to evaluate the contribution of salmon outplants to subsequent natural-origin (NOR) salmon recruitment to the river. Despite sampling limitations encountered during several years of the study, we were able to determine that most NOR salmon sampled in 2013 (59%) and 2014 (66%) were progeny of outplanted salmon. We were also able to estimate fitness, a cohort replacement rate (CRR), and the effective number of breeders (Nb) for salmon outplanted above Detroit Dam in 2009. On average, female fitness was ~5× (2.72:0.52 progeny) that of males and fitness was highly variable among individuals (range: 0-20 progeny). It is likely that the highly skewed male:female sex ratio (~6:1) among outplanted salmon limited reproductive opportunities for males in 2009. The CRR was 1.07, as estimated from female replacement. -
Analyzing Dam Feasibility in the Willamette River Watershed
Portland State University PDXScholar Dissertations and Theses Dissertations and Theses Spring 6-8-2017 Analyzing Dam Feasibility in the Willamette River Watershed Alexander Cameron Nagel Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Part of the Geography Commons, Hydrology Commons, and the Water Resource Management Commons Let us know how access to this document benefits ou.y Recommended Citation Nagel, Alexander Cameron, "Analyzing Dam Feasibility in the Willamette River Watershed" (2017). Dissertations and Theses. Paper 4012. https://doi.org/10.15760/etd.5896 This Thesis is brought to you for free and open access. It has been accepted for inclusion in Dissertations and Theses by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. Analyzing Dam Feasibility in the Willamette River Watershed by Alexander Cameron Nagel A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geography Thesis Committee: Heejun Chang, Chair Geoffrey Duh Paul Loikith Portland State University 2017 i Abstract This study conducts a dam-scale cost versus benefit analysis in order to explore the feasibility of each the 13 U.S. Army Corps of Engineers (USACE) commissioned dams in Oregon’s Willamette River network. Constructed between 1941 and 1969, these structures function in collaboration to comprise the Willamette River Basin Reservoir System (WRBRS). The motivation for this project derives from a growing awareness of the biophysical impacts that dam structures can have on riparian habitats. This project compares each of the 13 dams being assessed, to prioritize their level of utility within the system. -
Willamette Basin Review Feasibility Study
US Army Corps of Engineers Portland District Willamette Basin Review Feasibility Study DRAFT Integrated Feasibility Report and Environmental Assessment November 2017 Willamette Basin Review Feasibility Study Executive Summary The Willamette River basin is located entirely within the state of Oregon, beginning south of Cottage Grove, and extending approximately 187 miles to the north where the Willamette River flows into the Columbia River. The basin is more than 11,200 square miles, averages 75 miles in width, and encompasses approximately 12 percent of the total area of the state (Figure ES-1). Within the watershed are most of the state’s population (nearly 70 percent), larger cities, and major industries. The basin also contains some of Oregon’s most productive agricultural lands and supports nationally and regionally important fish and wildlife species. Thirteen of Oregon’s thirty-six counties intersect or lie within the boundary of the Willamette River basin. Through a series of Flood Control Acts the U.S. Congress authorized the U.S. Army Corps of Engineers (Corps) to construct, operate, and maintain thirteen major dams1 in the Willamette River basin. Collectively, these dams, reservoirs and associated infrastructure are known as the Willamette Valley Project (WVP). With a combined conservation storage capacity of approximately 1,590,000 acre-feet, the WVP is capable of providing important benefits for flood damage reduction, navigation, hydropower, irrigation, municipal and industrial water supply, flow augmentation for pollution abatement and improved conditions for fish and wildlife, and recreation. Feasibility Study History The Willamette Basin Review Feasibility Study began in 1996 to investigate future Willamette River basin water demand. -
Simulations of a Hypothetical Temperature Control Structure at Detroit Dam on the North Santiam River, Northwestern Oregon
Prepared in cooperation with the U.S. Army Corps of Engineers Simulations of a Hypothetical Temperature Control Structure at Detroit Dam on the North Santiam River, Northwestern Oregon Open-File Report 2015–1012 U.S. Department of the Interior U.S. Geological Survey Simulations of a Hypothetical Temperature Control Structure at Detroit Dam on the North Santiam River, Northwestern Oregon By Norman L. Buccola, Adam J. Stonewall, and Stewart A. Rounds Prepared in cooperation with the U.S. Army Corps of Engineers Open-File Report 2015–1012 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2015 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov or call 1–888–ASK–USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. Suggested citation: Buccola, N.L., Stonewall, A.J., and Rounds, S.A., 2015, Simulations of a hypothetical temperature control structure at Detroit Dam on the North Santiam River, northwestern Oregon: U.S. -
Lake Wise 2009
November LAKE WISE 2009 Editor: Roger Edwards A Voice for Quiet Waters The Oregon Lakes Association Newsletter Some Highlights from the Lincoln City Conference Rotating the site of OLA’s annual conference to different regions of Oregon each year provides attendees the chance to move beyond areas of their normal travels. Wherever the destination happens to be, the meeting produces serious discussions of lake topics, and the opportunity to greet old friends and meet new ones in a low key setting. This expectation was achieved again at Lincoln City last September. We were made to feel very welcome in Lincoln City, on the very first time OLA has met there. The resources we needed were conveniently near-by and handily served our purpose. Holding a lake meeting just steps away from a lake was a real bonus. Some of the vendors were demonstrating their instruments outside of the exhibit hall, where views of Devils Lake diverted attention from the sound of pounding surf from across Hwy 101. Inside, the full agenda of posters and presentations was divided between lake researchers, regulators, and enthusiasts, more-or-less paralleling the makeup of those in attendance. Everyone likely had a different impression of the day’s events, but the Board was universally pleased with this year’s Conference. It attracted well over a dozen new members, who will take our viewpoints to new locations, and who may seek a future position on the OLA Board. Some of these new members have affiliations with Oregon State University and extending our membership network there is a welcome development. -
Modeling Hydrodynamics, Water Temperature, and Suspended Sediment in Detroit Lake, Oregon
Prepared in cooperation with the City of Salem, Oregon Modeling Hydrodynamics, Water Temperature, and Suspended Sediment in Detroit Lake, Oregon Scientific Investigations Report 2007-5008 U.S. Department of the Interior U.S. Geological Survey Front Cover: Photograph of Detroit Lake and Piety Island, looking east. (Photograph by Mark Uhrich, U.S. Geological Survey, September 29, 2004.) Insets from left to right: Inset 1: Photograph showing aerial view of Detroit Dam, taken from just west of the dam. (Photograph from U.S. Army Corps of Engineers, July 11, 1990.) Inset 2: Photograph showing Breitenbush River storm inflow to Detroit Lake, looking west. (Photograph by Heather Bragg, U.S. Geological Survey, April 14, 2002.) Inset 3: Photograph showing Breitenbush River inflow to Detroit Lake, looking west. (Photograph by Heather Bragg, U.S. Geological Survey, November 7, 2006.) Back Cover: View of Mt. Jefferson over Detroit Lake, looking east. (Photograph by David Piatt, U.S. Geological Survey, July 4, 2004.) Modeling Hydrodynamics, Water Temperature, and Suspended Sediment in Detroit Lake, Oregon By Annett B. Sullivan, Stewart A. Rounds, Steven Sobieszczyk, and Heather M. Bragg Prepared in cooperation with the City of Salem, Oregon Scientific Investigations Report 2007–5008 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Reston, Virginia: 2007 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS--the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. -
Monitoring and Evaluation Report Willamette National Forest Fiscal Year 2011
AUGUST 2011 United States Department of Agriculture Monitoring and Forest Service Evaluation Report Pacific Northwest Region Willamette National Forest Fiscal Year 2011 Ames Creek, Sweet Home, Oregon i AUGUST 2011 ii AUGUST 2011 Welcome to the 2011 Willamette National Forest annual Monitoring and Evaluation report. This is our 23th year implementing the 1990 Willamette National Forest Plan, and this report is intended to give you an update on the services and products we provide. Our professionals monitor a wide variety of forest resources and have summarized their findings for your review. As I reviewed the Forest Plan Monitoring Report I got an opportunity to see the work our specialists are doing in one place and I can’t help but share my appreciation with what the Willamette’s resource specialists are accomplishing. I am overwhelmed by the effort our professionals are doing to get the work done and complete necessary monitoring under declining budgets. Our specialists have entered into partnerships, written grants, and managed volunteers in addition to working with numerous local and federal agencies. We are in the community and hope you enjoying the forests. I invite you to read this year’s report and contact myself or my staff with any questions, ideas, or concerns you may have. I appreciate your continued interest in the Willamette National Forest. Sincerely, MEG MITCHELL Forest Supervisor Willamette National Forest r6-will-009-11 The U.S. Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, age, disability, and where applicable, sex, marital status, familial status, parental status, religion, sexual orientation, genetic information, political beliefs, reprisal, or because all or part of an individual's income is derived from any public assistance program. -
DOGAMI Open-File Report O-76-05, Preliminary Report on The
PRELIMINARY REPORT ON THE RECONNAISSANCE GEOLOGY OF THE UPPER CLACKAMAS AND NORTH SANTIAM RIVERS AREA, CASCADE RANGE, OREGON by Paul E. Hammond Geologist Portland, Oregon July 1976 DRAFT COpy TABLE OF CONTENT S Summary of Main Geologic Findings . i" ~o~ s~, t- ,'j > <:},. Preliminary Evaluation of Geothermal Resource~ti~ ~ Introdul:tion Objectlves Accessibility Method of Mapping Rock Nomenclature Rock Units Introduction Western Cascade Group Beds at Detroit (Td) Breitenbush Tuff (Tbt) Nohorn Formation (Tnh) Bull Creek Beds (Tbc) Outerson Formation (To) Cub Point Formation (Tcp) Gordan Peak Formation (Tgp) Columbia River Basalt (Ter) Rhododendron Formation (Tr) Cheat Creek Beds (Tee) Scar Mountain Beds (sm) Miscellaneous Lava Flows: Vitrophyric Basalt of Lost Creek (TIc) Vitrophyric Andesite of Coopers and Boulder Ridges (Tcbr) Intrusive Rocks Trout Creek Vitrophyre (Titc) Basalt Dikes and Plugs (Tib) Hornblende Andesite (Tiha) Pyroxene Andesite (Tipa) Pyroxene Diorite (Tlpd) Possible Ouaternary Intrusions (Ql) High Cascade Group Older High Cascade Volcanic Rocks (OTb) Younger High Cascade Volcanic Rocks (Qb) Mount Jefferson Volcanic Deposits (OJ) Surficial Depo.its Glacial Deposits (f(jt, Qjo; Qst I Qso) Landslides (Qls) Talus (Qts) Alluvium (Qal) Structure Introduction Folds Faults Some General Observations High Cascade Graben or Volcano-Tectonic Depression Arching of the Cascade Range References - 1 - SUMMARY OF MAIN GEOLOGIC FINDINGS The upper Clackamas and North Santiam River area, covering about 635 square miles (1645 sq. km.) lies in the northwestern part of the Cascade Range, just west of Mount Jefferson. The area is underlain by over 20,000 feet (6100 m.) of volcanic strata of the probable upper part of the western Cascade Volcanic Group.