LAKE WISE Editor: Roger Edwards a Voice for Quiet Waters the Newsletter of the Oregon Lakes Association
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Timing of In-Water Work to Protect Fish and Wildlife Resources
OREGON GUIDELINES FOR TIMING OF IN-WATER WORK TO PROTECT FISH AND WILDLIFE RESOURCES June, 2008 Purpose of Guidelines - The Oregon Department of Fish and Wildlife, (ODFW), “The guidelines are to assist under its authority to manage Oregon’s fish and wildlife resources has updated the following guidelines for timing of in-water work. The guidelines are to assist the the public in minimizing public in minimizing potential impacts to important fish, wildlife and habitat potential impacts...”. resources. Developing the Guidelines - The guidelines are based on ODFW district fish “The guidelines are based biologists’ recommendations. Primary considerations were given to important fish species including anadromous and other game fish and threatened, endangered, or on ODFW district fish sensitive species (coded list of species included in the guidelines). Time periods were biologists’ established to avoid the vulnerable life stages of these fish including migration, recommendations”. spawning and rearing. The preferred work period applies to the listed streams, unlisted upstream tributaries, and associated reservoirs and lakes. Using the Guidelines - These guidelines provide the public a way of planning in-water “These guidelines provide work during periods of time that would have the least impact on important fish, wildlife, and habitat resources. ODFW will use the guidelines as a basis for the public a way of planning commenting on planning and regulatory processes. There are some circumstances where in-water work during it may be appropriate to perform in-water work outside of the preferred work period periods of time that would indicated in the guidelines. ODFW, on a project by project basis, may consider variations in climate, location, and category of work that would allow more specific have the least impact on in-water work timing recommendations. -
Yachats River Basin Fish Management Plan
( YACHATS RIVER BASIN FISH MANAGEMENT PLAN Oregon Department of Fish and Wildlife November 1997 l TABLE OF CONTENTS Introduction . .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. 3 Overview.............................................................................................. 5 Habitat................................................................................................ 9 Fall Chinook Salmon............................................................................ 27 Chum Salmon....................................................................................... 31 Coho Salmon........................................................................................ 33 Winter Steelhead .................... .............. ....... ......... ............ ............. ... .. .. 42 Cutthroat Trout.................................................................................... 4 7 Pacific Lamprey........................... .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. 51 Crayfish................................................................................................ 53 Angler Access ... ... .. .. ... .. .. .. .. .. .. .. ... .. .. .. .. .. .. .. .. .. .. .. .. 56 Priorities............................................................................................... 58 Implementation and Review.................................................................. 64 References........................................................................................... -
Upper Lake Creek SRMA Proposed Recreation Opportunity Spectrum 1
1792A 8320C UPPER LAKE CREEK SPECIAL RECREATION MANAGEMENT AREA RECREATION AREA MANAGEMENT PLAN ENVIRONMENTAL ASSESSMENT NO. OR095-04-08 January, 2005 ENVIRONMENAL ANALYSIS CONTENTS 1.0 INTRODUCTION 1.1 Background...................................................................................................................................... 1 1.2 Purpose and Need of the RAMP ..................................................................................................... 1 1.3 Management Objectives for the SRMA ........................................................................................... 1 1.3.1 Objective # 1 .......................................................................................................................... 1 1.3.2 Objective # 2 .......................................................................................................................... 1 1.3.3 Objective # 3 .......................................................................................................................... 2 1.3.4 Objective # 4 .......................................................................................................................... 2 1.4 Conformance with the Land Use Plans ........................................................................................... 2 2.0 ISSUES AND PUBLIC Scoping 2.1 Scoping............................................................................................................................................ 2 2.2 Issues Selected for Analysis........................................................................................................... -
Triangle Lake
Triangle Lake Lane County Mid Coast Basin Location Area 279 acres (112.9 hect) Elevation 695 ft (211.8 m) Type natural lake Use recreation Location 25 miles w est of Junction City in the Coast Range Access paved county boat ramp reached from Ore Hw y 36 USGS Quad Triangle Lake (24K), Eugene (100K) Coordinates 44˚ 09' 56" N, 123˚ 34' 14" W USPLSS tow nship 16S, range 07W, section 20 Triangle Lake lies high in the Oregon Coast Range only a few miles west of the divide and in the headwater portion of the Siuslaw River. The name of the lake is obviously taken from its geometric shape; however, in the latter part of the nineteenth century it was variously known as Loon Lake, Echo Lake, and Lake of the Woods. Although there are hundreds of natural lakes on the Oregon Coast, there are very few in the Coast Range. The explanation lies with the geologic and climatic history of the area. The Pleistocene Epoch was a time of high precipitation and this fact combined with tectonic uplift of the mountains produced very steep-walled, narrow valleys throughout the range. Glacial and volcanic processes, Source: Oregon National Guard, 1981-82. View looking southeast. responsible for most of the Cascade Mountain lakes, were virtually non-existent in the Coast Range. However, landslides in the rugged topography are quite common, and the few natural ` lakes that do exist were formed where massive slides blocked a river valley, impounding Drainage Basin Characteristics water behind it. The only two large natural lakes in the Coast Range, Triangle Lake and Loon Area 54.2 sq mi (140.4 sq km) Relief steep Precip 80-100 in (203-254 cm ) Lake, were formed in this manner. -
Assessment of Suspended-Sediment Transport, Bedload, and Dissolved Oxygen During a Short-Term Drawdown of Fall Creek Lake, Oregon, Winter 2012–13
Prepared in cooperation with the U.S. Army Corps of Engineers Assessment of Suspended-Sediment Transport, Bedload, and Dissolved Oxygen during a Short-Term Drawdown of Fall Creek Lake, Oregon, Winter 2012–13 Open-File Report 2014–1114 U.S. Department of the Interior U.S. Geological Survey Cover: Fall Creek Reservoir, Oregon, during drawdown. (Photograph by Liam N. Schenk, U.S. Geological Survey, December 13, 2012.) Inset: A hydrologist collects bedload samples downstream from the reservoir during drawdown. (Photograph by Heather M. Bragg, U.S. Geological Survey, December 3, 2012.) Assessment of Suspended-Sediment Transport, Bedload, and Dissolved Oxygen during a Short-Term Drawdown of Fall Creek Lake, Oregon, Winter 2012–13 By Liam N. Schenk and Heather M. Bragg Prepared in cooperation with the U.S. Army Corps of Engineers Open File Report 2014–1114 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, Director U.S. Geological Survey, Reston, Virginia: 2014 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 Suggested citation: Schenk, L.N., and Bragg, H.M., 2014, Assessment of suspended-sediment transport, bedload, and dissolved oxygen during a short-term drawdown of Fall Creek Lake, Oregon, winter 2012–13: U.S. -
Hult Reservoir Fish Species Composition, Size and Relative Abundance 2017
HULT RESERVOIR FISH SPECIES COMPOSITION, SIZE AND RELATIVE ABUNDANCE 2017 Prepared for BUREAU OF LAND MANAGEMENT SIUSLAW FIELD OFFICE 3106 Pierce Parkway, Suite E Springfield, Oregon 97477 i Prepared by Jeremy D. Romer Fred R. Monzyk Erik J. Suring Thomas A. Friesen Oregon Department of Fish and Wildlife Reservoir Research Project Corvallis Research Lab 28655 Highway 34 Corvallis, Oregon 97333 Cooperative Agreement: L12AC20634 February 2018 ii Table of Contents Summary ...................................................................................................................................................... 1 Background / Introduction ......................................................................................................................... 2 Methods ........................................................................................................................................................ 4 Fish Capture .............................................................................................................................................. 4 Water Chemistry ....................................................................................................................................... 5 Data Analysis ............................................................................................................................................. 5 Species Composition, Size, and Relative Abundance ................................................................................ 5 Coho Salmon and the -
Geologic Interpretation of Floodplain Deposits of the Southwestern
Geologic Interpretation of Floodplain Deposits of the Southwestern Willamette Valley, T17SR4W With Some Implications for Restoration Management Practices Eugene, Oregon Michael James, James Geoenvironmental Services Karin Baitis, Eugene District BLM JULY 2003 TABLE OF CONTENTS Page EXECUTIVE SUMMARY i ACKNOWLEDGEMENTS 1 CHAPTER 1 INTRODUCTION 1 Location 2 CHAPTER 2 WEST EUGENE GEOLOGIC BACKGROUND 9 CHAPTER 3 RESULTS 15 3.1 MAPPING 15 3.1.1Stratigraphic and Soil Investigation 15 3.1.2 Chronology of Lithologic Units: Radiocarbon Dating and Paleopedology 17 3.1.3 Summary 23 3.2 CHARACTERIZATION OF SEDIMENTS 24 3.2.1 Textural and Sedimentological Analysis 24 3.3 MINERALOGY 26 3.3.1 Soil 26 3.3.2 Tephra Analysis 32 3.3.3 Clay XRD 33 3.3.4 Summary 38 3.4 MINERAL CHEMISTRY 40 3.4.1 Microprobe and Neutron Activation Analysis 40 3.4.2 Trace Elements 48 3.4.3 Summary 52 3.5 SURFACE AND SOIL WATER CONDUCTIVITY 53 3.5.1 General Experiment Design 53 3.5.2 Amazon Creek and Area Stream Conductivities 58 3.5.3 Soil/Water Conductivity 60 3.5.4 Ion Chromatography of Soil Profiles--Paul Engelking 60 3.5.5 Summary 61 3.6 RESTORATION TREATMENT SOIL CONDUCTIVITY ANALYSES 62 3.6.1 Conductivity and Ion Chromatography 62 3.6.2 Nutrient Tests 65 3.6.3 Summary 66 CHAPTER 4 CONCLUSIONS AND RECOMMENDATIONS 68 4.1 Conclusions 68 4.2 Recommendations 71 REFERENCES 73 Appendix A Soil Descriptions Appendix B Soil Photographs with Descriptions Appendix C Stratigraphic Columns Appendix D Textural and Mineralogic Table Appendix E XRD Appendix F Neutron Activation Appendix G Soil and Water Conductivity Appendix H Soil Treatment Conductivity EXECUTIVE SUMMARY A three-and-one-half mile, NW-SE transect of soil auger borings was done in West Eugene from Bailey Hill Rd to Oak Knoll across parcels that make up part of the West Eugene Wetlands. -
Angling Guide Oregon Department of Fish and Wildlife
Angling Guide Oregon Department of Fish and Wildlife Alton Baker Park canoe canal: In Eugene by Autzen Stadium. Stocked in the spring with rainbow trout. A good place to take kids. Big Cliff Reservoir: 150 acres on the North Santiam River. The dam is located several miles below Detroit Dam off of Highway 22. Stocked with trout. Blue River Reservoir and Upper Blue River: 42 miles east of Eugene off Highway 126. Native cutthroat and rainbow. Stocked in spring and early summer with rainbow trout. USFS campground. Bond Butte Pond: 3 miles north of the Harrisburg exit on the east side of I-5 at MP 212 (the Bond Butte overpass). Channel catfish, largemouth bass, white crappie, bluegill. Carmen Reservoir: 65-acre reservoir located on Highway 126 appproximately 70 miles east of Springfield. Rainbow trout, cutthroat trout, brook trout. Clear Lake: 70 miles east of Eugene off Highway 126. Naturally reproducing brook trout and stocked with rainbow trout. Resort with restaurant, boat and cabin rentals. USFS campground. Cottage Grove Ponds: A group of 6 ponds totaling 15 acres. Located 1.5 miles east of Cottage Grove on Row River Road behind the truck scales. Largemouth bass, bluegill, bullhead. Rainbow trout are stocked into one pond in the spring. Cottage Grove Reservoir: Six miles south of Cottage Grove on London Road. Largemouth bass, brown bullhead, bluegill, cutthroat trout. Hatchery rainbow are stocked in the spring. USACE provides campgrounds. There is a health advisory for mercury contamination. Pregnant women, nursing women and children up to six years old should not eat fish other than stocked rainbow trout; children older than 6 and healthy adults should not eat more than 1/2 pound per week. -
Short‐Term Reservoir Draining to Streambed for Juvenile Salmon Passage and Non‐Native Fish Removal
Received: 8 October 2018 Revised: 10 April 2019 Accepted: 10 April 2019 DOI: 10.1002/eco.2096 RESEARCH ARTICLE Short‐term reservoir draining to streambed for juvenile salmon passage and non‐native fish removal Christina A. Murphy1 | Gregory Taylor2 | Todd Pierce2 | Ivan Arismendi1 | Sherri L. Johnson3 1 Department of Fisheries and Wildlife, Oregon State University, Corvallis, OR Abstract 2 Willamette Valley Project, US Army Corps of Fish passage out of reservoirs is a critical issue for downstream movement of juvenile Engineers, Lowell, OR salmonids and other migratory species. Reservoirs can delay downstream migrations 3 Pacific Northwest Research Station, US by juvenile salmon for months or years. Here, we examine whether a novel manage- Forest Service, Corvallis, OR ment activity implementing annual short‐term draining of a reservoir to streambed Correspondence improves timely downstream migration of juvenile salmonids. We analyse 12 years Christina Murphy, Department of Fisheries and Wildlife, Oregon State University, Corvallis, of fish capture data from a screw trap located downstream of Fall Creek Reservoir OR. (Oregon, USA) to examine changes in timing of passage out of the reservoir and to Email: [email protected] compare fish species composition pre‐ and post‐draining. We observed a contraction Funding information in the timing of downstream migration for juvenile Chinook Salmon and reduction of U.S. Environmental Protection Agency, Grant/ Award Number: STAR Fellowship FP‐ yearlings in years following draining. We suggest that briefly draining the reservoir to 91782401‐1 streambed leads to reduced abundance of warm‐water invasive fishes in the reservoir after it refills. These changes could decrease predation and shift competition between invasive and resident riverine‐adapted native fishes in the reservoir. -
Chapter3 Reference and Current Conditions
CHAPTER3 REFERENCE AND CURRENT CONDITIONS PHYSICAL DOMAIN !f31:()L00..,_, Winberry/Lower Fall Creek analysis area is the second largest drainage in the Fall Creek subwatershed. It has 43,890 acres and encompasses the entire Winberry subwatershed as well as the reservoir portion of Fall Creek subwatershed. The analysis area has been subdivided into five drainages (see Mylar Overlay). The largest is South Reservoir with 13,439 acres; Brush Creek is the smallest with 2,620 acres. An east-west trending ridge divides the upper portion into South Fork Winberry Creek and North Fork Winberry Creek. There are two main tributaries on South Fork Winberry Creek: Cabin Creek and Monterica Creek. North Fork Winberry Creek has three main tributaries: Blanket Creek, Traverse Creek and Brush Creek. Just east of the USFS boundary, the North and South Forks of Winberry Creek combine to form mainstem Winberry Creek. Its main tributaries between the national forest boundary and Fall Creek Reservoir are Alder Creek and Nelson Creek. Numerous unnamed tributaries enter Fall Creek Reservoir during full pool. Fall Creek flows from the reservoir, collects a few unnamed tributaries and joins Uttl.e Fall Creek three miles below the reservoir, where the analysis area ends. · Igneous extrusives such as tuffs, lapilli ·tuffs, tuffaceous sedimentary pyroclastics, and lava flows predominate. Igneous intrusive rocks account for less than 1% of the watershed. Distribution estimates of extrusive rock types range from 75-80% pyroclastic origin and 20-25% lava flows (Peck and others, 1964, Sharrod, 1991). Spatially, the older rocks are predominately tuffs and tuffaceous sedimentary rocks and tend to be found at lower to middle elevations. -
Winberry and Lower Fall Creek
J V\Tet""agencyf! - Winberry and Lower Fall Creek Wa-~e~shed Analysis .~ \.Vinberfi'/l~o~er tall Creek \.Valershed Anal-ysis Inleragen(..'{ Core Tea1n Rick Cope Team Leader Geology/Soils Specialist Sue Baker Recrealionall·bresler L-ynn Larson rbresl Ecologist Laurie Bernstein r1sheries Biologist Kirk Lunstrwn \.Vildlife Biologisl Jenn-y Din1Hng Botanist Bob Magne Fisheries Biologist Rand-y Green Fire;1·uels Spedalisl l<.tis \.Vard H-ydrologist George Hill Park Ranger Sonja \.Veber Editor/Graphics Contributors .lon Belcher GIS Mar-y Lee Gra-y Editor Tom Jackson GIS "Val Rogers H-ydrology Technician Larr.y Tennis Transportation Spedalist Larr.y \.Veddle \.Vildlife Technician K.ds \.Vobbe GIS TABLE OF CONTENTS INTRODUCTION 9 CHAPTER 1 12 PHYSICAL DOMAIN ·············································•····························································· 1 2 GEOLcx:J.Y ····································-············································~·-·····································12 EROSION PROCESSES ••••••••••••••••••••••••••••••••••••••••••••••••••••••••••••••••••••••••••••••••••••••••••••••••••••••••• 12 HYDROLcx;Y ••••••.••••••.••••••••••••••••••••••••.•..••••••.•••.•.••••••.••••••••••.••.••.••.••••.••.••••••••.•..••••••...•••••• 13 WA'TER QUAI. .ITY •••••••••••.•••••••••••••••••..•.•.••.•••..•.•.••.•.•.•••..•....•..•.••••••.•..•.••.••••••.•.•.•••••.•.••••••. 13 RO.ADS ···························-·································································································14 BIOLOGICAL DOMAIN······································································································· -
Insights on the Hydrologic Impacts of Large Dams in Oregon.Pdf
Dams in Oregon: impacts, opportunities and future directions Rose Wallick Chauncey Anderson, Stewart Rounds, Mackenzie Keith, Krista Jones USGS Oregon Water Science Center U.S. Department of the Interior U.S. Geological Survey Dams in Oregon Dam Height More than 1,100 dams in state dam inventory 48 dams more than 100ft tall 10 dams more than 300 ft tall Cougar Dam is tallest – 519 ft Overview Purpose and environmental impacts of dams Strategies to address impacts . Removal, infrastructure modifications, operations Science insights from USGS studies Future directions U.S. has more than 87,000 documented dams Source: National Inventory of Dams, ttp://nid.usace.army.mil/ Detroit Dam, completed 1953, 463 ft Dams built perdecade Damsbuilt After Doyle et al. (2003) Cougar Dam, completed 1963, 519 ft Photographs courtesy USACE Purpose of dams Dams provide: . Hydropower . Flood control . Water storage . Navigation Middle Fork Willamette, USGS photo . Recreation . Other benefits Detroit Lake, Photo courtesy: https://www.detroitlakeoregon.org/ Environmental impacts of dams . Alter river flows, water temperature, water quality, trap sediment, carbon, nutrients in reservoirs . Block fish passage . Change ecosystems above and below dams . Support conditions that can lead to harmful algae blooms Cougar Reservoir, South Fork McKenzie, USGS photo Middle Fork Willamette River below Dexter Dam, USGS photo Motivating factors for removing, upgrading or re-operating dams Examples include: • Dams age, expensive to maintain safely • Facilities may not work as