Banks Lake Fish Survey, September 2000.WPD
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Washington Division of Geology and Earth Resources Open File Report
RECONNAISSANCE SURFICIAL GEOLOGIC MAPPING OF THE LATE CENOZOIC SEDIMENTS OF THE COLUMBIA BASIN, WASHINGTON by James G. Rigby and Kurt Othberg with contributions from Newell Campbell Larry Hanson Eugene Kiver Dale Stradling Gary Webster Open File Report 79-3 September 1979 State of Washington Department of Natural Resources Division of Geology and Earth Resources Olympia, Washington CONTENTS Introduction Objectives Study Area Regional Setting 1 Mapping Procedure 4 Sample Collection 8 Description of Map Units 8 Pre-Miocene Rocks 8 Columbia River Basalt, Yakima Basalt Subgroup 9 Ellensburg Formation 9 Gravels of the Ancestral Columbia River 13 Ringold Formation 15 Thorp Gravel 17 Gravel of Terrace Remnants 19 Tieton Andesite 23 Palouse Formation and Other Loess Deposits 23 Glacial Deposits 25 Catastrophic Flood Deposits 28 Background and previous work 30 Description and interpretation of flood deposits 35 Distinctive geomorphic features 38 Terraces and other features of undetermined origin 40 Post-Pleistocene Deposits 43 Landslide Deposits 44 Alluvium 45 Alluvial Fan Deposits 45 Older Alluvial Fan Deposits 45 Colluvium 46 Sand Dunes 46 Mirna Mounds and Other Periglacial(?) Patterned Ground 47 Structural Geology 48 Southwest Quadrant 48 Toppenish Ridge 49 Ah tanum Ridge 52 Horse Heaven Hills 52 East Selah Fault 53 Northern Saddle Mountains and Smyrna Bench 54 Selah Butte Area 57 Miscellaneous Areas 58 Northwest Quadrant 58 Kittitas Valley 58 Beebe Terrace Disturbance 59 Winesap Lineament 60 Northeast Quadrant 60 Southeast Quadrant 61 Recommendations 62 Stratigraphy 62 Structure 63 Summary 64 References Cited 66 Appendix A - Tephrochronology and identification of collected datable materials 82 Appendix B - Description of field mapping units 88 Northeast Quadrant 89 Northwest Quadrant 90 Southwest Quadrant 91 Southeast Quadrant 92 ii ILLUSTRATIONS Figure 1. -
Dry Falls Visitor Center Due to the Fact That Many Travelers Saw These Unusual Landforms in the Landscape As They Drove the Coulee Corridor
Interactive Design Approach IMMERSIVE Theater Topo Model The design approach for the exhibits is closely integrated with the Seating architecture. The layering of massive, linear building walls pro- for 50-60 EXHIBIT vides a direction for the design and layout of exhibit components. Gallery Real ‘Today’ erratic OUTDOOR Terrace Building walls are cut open at strategic points to accommodate WITH EXhibits specific exhibits and to allow for circulation. Smaller, wall-panel exhibits are used for supports and dividers. Equipment ‘Volcanic ‘Ice Age Floods’ Room Period’ Approaching the center, visitors are forced to walk around a mas- sive erratic – these huge boulders are seemingly deposited directly Gallery Animal Modelled erratic Lava flow overhead Freestanding time line animal cutouts on the path to the front door. The displaced rock serves as a strong Welcome in floor icon of the violent events that occurred during the Ice Age Floods. Through the Visitor Center’s front doors, visitors are startled to see another massive erratic precariously wedged overhead between W M Retail / cafe the two parallel building walls. Just out of reach it makes an un- usual photo opportunity for visitors who puzzle over how the rock terrace stays in place. From an interpretive standpoint, it is important to Outdoor Classroom realize no actual erratics are present in the Sun Lakes-Dry Falls with Amphitheater State Park landscape. During the floods, water was moving too quickly for erratics to be deposited at Dry Falls - they were car- ried downstream and deposited in the Quincy and Pasco basins many miles away. However, the results of the visioning workshop determined that erratics are an important and exciting flood fea- ture to display at the Dry Falls Visitor Center due to the fact that many travelers saw these unusual landforms in the landscape as they drove the Coulee Corridor. -
Millersylvania State Park
STEAMBOAT ROCK STATE PARK MANAGEMENT PLAN November 2010 Washington State Parks’ Mission: The Washington State Parks and Recreation Commission acquires, operates, enhances, and protects a diverse system of recreational, cultural, and natural sites. The Commission fosters outdoor recreation and education statewide to provide enjoyment and enrichment for all and a valued legacy to future generations. Steamboat Rock State Park Management Plan Page 1 ACKNOWLEDGMENTS AND CONTACTS The Washington State Parks and Recreation Commission gratefully acknowledges the many stakeholders and the staff of Steamboat Rock State Park who participated in public meetings, reviewed voluminous materials, and made this a better plan because of it. Plan Author Andrew Fielding, Environmental Planner, Eastern Region Steamboat Rock State Park Area Management Planning Team Tom Poplawski, Steamboat Rock State Park Manager Jim Harris, Eastern Region Director Tom Ernsberger, Eastern Region Operations Manager Brian Hovis, Administrator, Policy and Governmental Affairs, Olympia Headquarters Bill Fraser, Parks Planner, Eastern Region Andrew Fielding, Environmental Planner, Eastern Region Washington State Park and Recreation Commission 1111 Israel Road SW, Olympia, WA 98504 Tel: (360) 902-8500 Fax: (360) 753-1591 TDD: (360) 664-3133 Commissioners (at time of land classification adoption): Fred Olson, Chair Joe Taller, Vice Chair Rodger Schmitt, Secretary Eliot Scull Lucinda S. Whaley Patricia T. Lantz Cecilia Vogt Rex Derr, Director Steamboat Rock State Park Management Plan -
Top 35 Fishing Waters of Grant County
TOP35 FISHING WATERS In Grant County, Washington For more information, please contact: Grant County Tourism Commission P.O. Box 37, Ephrata, WA 98823 509.765.7888 • 800.992.6234 TourGrantCounty.com CONTENTS Grant County Tourism Commission The Top 35 Fishing Waters In Grant County, Washington PO Box 37 1. Potholes Reservoir (28,000 acres) .................................................1 Ephrata, Washington 98837 2. Banks Lake (24,900 acres) .......................................................2 TOP 3. Moses Lake (6,800 acres) .......................................................3 No part of this book may be reproduced in any 4. Blue Lake (534 acres) ...........................................................4 3 form, or by any electronic, mechanical, or other 5. Park Lake (338 acres) ...........................................................5 5 means, without permission in writing from the 6. Burke Lake (69 acres) ...........................................................6 Grant County Tourism Commission. 7. Martha Lake (15 acres) ..........................................................7 FISHING 8. Corral Lake (70 acres) ...........................................................8 © 2019, Grant County Tourism Commission Fifth printing, 10m 9. Priest Lake Pool (below Wanapum Dam) ...........................................8 WATERS 10. Hanford Reach (below Priest Rapids Dam) .........................................10 11. Rocky Ford Creek .............................................................11 In Grant County, Washington -
The Missoula Flood
THE MISSOULA FLOOD Dry Falls in Grand Coulee, Washington, was the largest waterfall in the world during the Missoula Flood. Height of falls is 385 ft [117 m]. Flood waters were actually about 260 ft deep [80 m] above the top of the falls, so a more appropriate name might be Dry Cataract. KEENAN LEE DEPARTMENT OF GEOLOGY AND GEOLOGICAL ENGINEERING COLORADO SCHOOL OF MINES GOLDEN COLORADO 80401 2009 The Missoula Flood 2 CONTENTS Page OVERVIEW 2 THE GLACIAL DAM 3 LAKE MISSOULA 5 THE DAM FAILURE 6 THE MISSOULA FLOOD ABOVE THE ICE DAM 6 Catastrophic Flood Features in Eddy Narrows 6 Catastrophic Flood Features in Perma Narrows 7 Catastrophic Flood Features at Camas Prairie 9 THE MISSOULA FLOOD BELOW THE ICE DAM 13 Rathdrum Prairie and Spokane 13 Cheny – Palouse Scablands 14 Grand Coulee 15 Wallula Gap and Columbia River Gorge 15 Portland to the Pacific Ocean 16 MULTIPLE MISSOULA FLOODS 17 AGE OF MISSOULA FLOODS 18 SOME REFERENCES 19 OVERVIEW About 15 000 years ago in latest Pleistocene time, glaciers from the Cordilleran ice sheet in Canada advanced southward and dammed two rivers, the Columbia River and one of its major tributaries, the Clark Fork River [Fig. 1]. One lobe of the ice sheet dammed the Columbia River, creating Lake Columbia and diverting the Columbia River into the Grand Coulee. Another lobe of the ice sheet advanced southward down the Purcell Trench to the present Lake Pend Oreille in Idaho and dammed the Clark Fork River. This created an enormous Lake Missoula, with a volume of water greater than that of Lake Erie and Lake Ontario combined [530 mi3 or 2200 km3]. -
John W. Keys III Pump-Generating Plant
U.S. Department of the Interior Bureau of Reclamation John W. Keys III Pump-Generating Plant The John W. Keys III Pump-Generating Plant pumps for irrigation and also provides important recreational water uphill 280 feet from Franklin D. Roosevelt Lake benefits to the region. to Banks Lake. This water is used to irrigate approxi- The pump-generating plant began operation in 1951. mately 670,000 acres of farmland in the Columbia Basin From 1951 to 1953, six pumping units, each rated at Project. More than 60 crops are grown in the basin and 65,000 horsepower and with a capacity to pump 1,600 distributed across the nation. cubic feet per second, were installed in the plant. Congress authorized Grand Coulee Dam in 1935, with In the early 1960s, investigations revealed the potential its primary purpose to provide water for irrigation. for power generation. Reversible pumps were installed to When the United States entered World War II in 1941, allow water from Banks Lake to flow back through the the focus of the dam shifted from irrigation to power units to generate power during periods of peak demand. production. It was not until 1943 that Congress autho- The first three generating pumps came online in 1973. rized the Columbia Basin Project to deliver water to the Two more generating pumps were installed in 1983; the farmers of central Washington State. final generating pump was installed in January 1984. Construction of the irrigation facilities began in 1948. The total generating capacity of the plant is now Components of the project include the pump-generating 314,000 kilowatts. -
Wvter Action
WVTER TO ACTION GRAND COULEE DAM AND LAKE ROOSEVELT U.S. BUREAU OF RECLAMATION- BONNEVILLE POWER ADMINISTRATION -U.S. NATIONAL PARK SERVICE ake Roosevelt has steadily gained in popularity as a summer tourist attraction. t High reservoir levels most years provide visitors with a rich variety of recreational opportunities. But many people are not aware of the full story behind Grand Coulee Dam and the great lake it created. This brochure explains the origin of Lake Roosevelt, why it was built and how it serves the people of the Pacific Northwest. It represents a unified effort on the part of the three federal agencies most involved in management and oversight of Lake Roosevelt and Grand Coulee Dam: the U. S. Bureau of Reclamation, the Bonneville Power Administration, and the U.S. National Park Service. Who's responsible for what? The U.S. Bureau of Reclamation built and operates the Columbia Basin Project including Grand Coulee Dam. While many parties with diverse needs and interests provide input in the pro ject's operation, Reclamation makes the final decisions. To contact a repre sentative of Reclamation, call (509) 638-1360 or write to Grand Coulee Project Office, Attention: Code 140, Grand Coulee, Washington 99133. The Bonneville Power Administration markets and distributes power gener ated at federal dams on the Columbia River and its tributaries. In 1980, a new federal law charged BPA with ensuring that the Northwest has an adequate sup ply of power, whether from hydroelectric dams or other generating resources. BPA schedules power generation at Grand Coulee Dam within constraints established by Reclamation that provide for the project's multipurpose benefits. -
Lake Missoula and Its Floods by Kendall L
Society for Range Management Lake Missoula and Its Floods By Kendall L. Johnson he city of Spokane lies astride the Spokane River, out of the earth over previous untold centuries. The winds some 40 miles from its origination near Coeur created dune-like deposits of variable orientation and depth d’Alene, Idaho. The convention center and that today make up fertile farmland in southeastern hotel, site of the 65th annual meeting of SRM, are Washington and adjacent Idaho. Bretz’s Flood followed the Tlocated right along the river, creating a beautiful and even path of the many earlier fl oods and recreated the effects over idyllic setting. These qualities make it even harder to imagine thousands of square miles in the Columbia Basin. These can a long-ago day when a miles-wide wall of water, measuring briefl y be considered in four major categories: 1) the chan- as much as 500 feet high, bore down on this site. Hours neled scablands, 2) the river canyon, 3) the Grand Coulee, before, a great ice dam on glacial Lake Missoula (present-day and 4) Lake Lewis. Clark Fork River) had failed. The dam was as much as 2,500 feet in height, impounded a lake up to 2,000 feet deep, The Channeled Scablands extended east in the intermontane valleys for 200 miles, and The enormous depth of the advancing front of water, covered some 3,000 square miles. It probably contained over 500 cubic miles of water, approximating half the volume of measured in the several hundreds of feet, moving at speeds Lake Michigan. -
Banks Lake Drawdown Environmental Impact Statement
Banks Lake Drawdown Final Environmental Impact Statement U.S. Department of the Interior Upper Columbia Area Office Bureau of Reclamation Ephrata Field Office Pacific Northwest Region Ephrata, Washington Boise, Idaho May 2004 MISSION STATEMENTS The mission of the Department of the Interior is to protect and provide access to our Nation’s natural and cultural heritage and honor our trust responsibilities to Indian tribes and our commitments to island communities. The mission of the Bureau of Reclamation is to manage, develop, and protect water and related resources in an environmentally and economically sound manner in the interest of the American public. Final Environmental Impact Statement Banks Lake Drawdown Douglas and Grant Counties, Washington Lead Agency: U.S. Department of the Interior Bureau of Reclamation For further information contact: Jim Blanchard Special Projects Officer Ephrata Field Office Bureau of Reclamation Box 815 Ephrata, WA 98823 (509) 754-0226 The Action Alternative describes the resource conditions that would occur with Banks Lake water surface elevations between 1570 feet and 1560 feet, while the No Action Alternative describes the conditions that would occur without the action, with water surface elevation between 1570 feet and 1565 feet. Both the No Action and Action Alternatives include four potential operational scenarios that could occur annually within their respective ranges, depending upon the hydrology of any given year. Both alternatives include refilling the reservoir to elevation 1570 feet by September 22. The No Action Alternative is the preferred alternative. The draft environmental impact statement provided Reclamation’s determination that the Action Alternative “may affect but is not likely to adversely affect” the federally listed bald eagle (Haliaeetus leucocephalus) and would have no effect on the federally listed pygmy rabbit (Brachylagus idahoensis) or Ute ladies’-tresses (Spiranthes diluvialis). -
This File Was Created by Scanning the Printed Publication
This file was created by scanning the printed publication. Text errors identified by the software have been corrected; however, some errors may remain. Editors SHARON E. CLARKE is a geographer and GIS analyst, Department of Forest Science, Oregon State University, Corvallis, OR 97331; and SANDRA A. BRYCE is a biogeographer, Dynamac Corporation, Environmental Protection Agency, National Health and Environmental Effects Research Laboratory, Western Ecology Division, Corvallis, OR 97333. This document is a product of cooperative research between the U.S. Department of Agriculture, Forest Service; the Forest Science De- partment, Oregon State University; and the U.S. Environmental Protection Agency. Cover Artwork Cover artwork was designed and produced by John Ivie. Abstract Clarke, Sharon E.; Bryce, Sandra A., eds. 1997. Hierarchical subdivisions of the Columbia Plateau and Blue Mountains ecoregions, Oregon and Washington. Gen. Tech. Rep. PNW-GTR-395. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station. 114 p. This document presents two spatial scales of a hierarchical, ecoregional framework and provides a connection to both larger and smaller scale ecological classifications. The two spatial scales are subregions (1:250,000) and landscape-level ecoregions (1:100,000), or Level IV and Level V ecoregions. Level IV ecoregions were developed by the Environmental Protection Agency because the resolution of national-scale ecoregions provided insufficient detail to meet the needs of state agencies for estab- lishing biocriteria, reference sites, and attainability goals for water-quality regulation. For this project, two ecoregions—the Columbia Plateau and the Blue Mountains— were subdivided into more detailed Level IV ecoregions. -
Carlson-Duncan-Johnson Grand Coulee 2004
PNNL-14998 Characterization of Pump Flow at the Grand Coulee Dam Pumping Station for Fish Passage, 2004 TJ Carlson JP Duncan RL Johnson FINAL REPORT March 31, 2005 Prepared for the Bonneville Power Administration under a Related Services Agreement with the U.S. Department of Energy Contract DE-AC05-76RL01830 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 Battelle Memorial Institute, 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, or Battelle Memorial Institute. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. PACIFIC NORTHWEST NATIONAL LABORATORY operated by BATTELLE for the UNITED STATES DEPARTMENT OF ENERGY under Contract DE-AC05-76RL01830 Printed in the United States of America Available to DOE and DOE contractors from the Office of Scientific and Technical Information, P.O. Box 62, Oak Ridge, TN 37831-0062; ph: (865) 576-8401 fax: (865) 576-5728 email: [email protected] Available to the public from the National Technical Information Service, U.S. -
Field-Trip Guide to the Vents, Dikes, Stratigraphy, and Structure of the Columbia River Basalt Group, Eastern Oregon and Southeastern Washington
Field-Trip Guide to the Vents, Dikes, Stratigraphy, and Structure of the Columbia River Basalt Group, Eastern Oregon and Southeastern Washington Scientific Investigations Report 2017–5022–N U.S. Department of the Interior U.S. Geological Survey Cover. Palouse Falls, Washington. The Palouse River originates in Idaho and flows westward before it enters the Snake River near Lyons Ferry, Washington. About 10 kilometers north of this confluence, the river has eroded through the Wanapum Basalt and upper portion of the Grande Ronde Basalt to produce Palouse Falls, where the river drops 60 meters (198 feet) into the plunge pool below. The river’s course was created during the cataclysmic Missoula floods of the Pleistocene as ice dams along the Clark Fork River in Idaho periodically broke and reformed. These events released water from Glacial Lake Missoula, with the resulting floods into Washington creating the Channeled Scablands and Glacial Lake Lewis. Palouse Falls was created by headward erosion of these floodwaters as they spilled over the basalt into the Snake River. After the last of the floodwaters receded, the Palouse River began to follow the scabland channel it resides in today. Photograph by Stephen P. Reidel. Field-Trip Guide to the Vents, Dikes, Stratigraphy, and Structure of the Columbia River Basalt Group, Eastern Oregon and Southeastern Washington By Victor E. Camp, Stephen P. Reidel, Martin E. Ross, Richard J. Brown, and Stephen Self Scientific Investigations Report 2017–5022–N U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior RYAN K. ZINKE, Secretary U.S.