ACTIVE FAULTING and QUATERNARY PALEOHYDROLOGY of the TRUCKEE FAULT ZONE NORTH of TRUCKEE, CALIFORNIA by Aaron Dwight Melody a Th
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Washington Division of Geology and Earth Resources Open File Report
l 122 EARTHQUAKES AND SEISMOLOGY - LEGAL ASPECTS OPEN FILE REPORT 92-2 EARTHQUAKES AND Ludwin, R. S.; Malone, S. D.; Crosson, R. EARTHQUAKES AND SEISMOLOGY - LEGAL S.; Qamar, A. I., 1991, Washington SEISMOLOGY - 1946 EVENT ASPECTS eanhquak:es, 1985. Clague, J. J., 1989, Research on eanh- Ludwin, R. S.; Qamar, A. I., 1991, Reeval Perkins, J. B.; Moy, Kenneth, 1989, Llabil quak:e-induced ground failures in south uation of the 19th century Washington ity of local government for earthquake western British Columbia [abstract). and Oregon eanhquake catalog using hazards and losses-A guide to the law Evans, S. G., 1989, The 1946 Mount Colo original accounts-The moderate sized and its impacts in the States of Califor nel Foster rock avalanches and auoci earthquake of May l, 1882 [abstract). nia, Alaska, Utah, and Washington; ated displacement wave, Vancouver Is Final repon. Maley, Richard, 1986, Strong motion accel land, British Columbia. erograph stations in Oregon and Wash Hasegawa, H. S.; Rogers, G. C., 1978, EARTHQUAKES AND ington (April 1986). Appendix C Quantification of the magnitude 7.3, SEISMOLOGY - NETWORKS Malone, S. D., 1991, The HAWK seismic British Columbia earthquake of June 23, AND CATALOGS data acquisition and analysis system 1946. [abstract). Berg, J. W., Jr.; Baker, C. D., 1963, Oregon Hodgson, E. A., 1946, British Columbia eanhquak:es, 1841 through 1958 [ab Milne, W. G., 1953, Seismological investi earthquake, June 23, 1946. gations in British Columbia (abstract). stract). Hodgson, J. H.; Milne, W. G., 1951, Direc Chan, W.W., 1988, Network and array anal Munro, P. S.; Halliday, R. J.; Shannon, W. -
Cottonwood Lakes / New Army Pass Trail
Inyo National Forest Cottonwood Lakes / New Army Pass Trail Named for the cottonwood trees which were located at the original trailhead in the Owens Valley, the Cottonwood Lakes are home to California's state fish, the Golden Trout (Oncorhynchus mykiss aguabonita). The lakes are located in an alpine basin at the southern end of the John Muir Wilder- ness. They are surrounded by high peaks of the Sierra Nevada, including Cirque Peak and Mt. Lang- ley. The New Army Pass Trail provides access to Sequoia National Park and the Pacific Crest Trail. Trailhead Facilities: Water: Yes Bear Resistant Food Storage Lockers: Yes Campgrounds: Cottonwood Lakes Trailhead Campground is located at the trailhead. Visitors with stock may use Horseshoe Meadow Equestrian Camp, located nearby. On The Trail: Food Storage: Food, trash and scented items must be stored in bear-resistant containers. Camping: Use existing campsites. Camping is prohibited within 25 feet of the trail, and within 100 feet of water. Human Waste: Bury human waste 6”-8” deep in soil, at least 100 feet from campsites, trails, and water. Access: Campfires: Campfires are prohibited above 10,400 ft. The trailhead is located approximately 24 miles southwest of Lone Pine, CA. From Highway Pets: Pets must be under control at all times. 395 in Lone Pine, turn west onto Whitney Portal Additional Regulations: Information about Kings Road. Drive 3.5 miles and turn south (left) onto Canyon National Park regulations is available at Horseshoe Meadow Road. Travel approximately www.nps.gov/seki, www.fs.usda.gov/goto/inyo/ 20 miles, turn right and follow signs to the cottonwoodlakestrail or at Inyo National Forest Cottonwood LAKES Trailhead. -
Distribution List
Revised DEIS/EIR Truckee River Operating Agreement DISTRIBUTION LIST CONGRESSIONAL DELEGATIONS Nevada Senators John Ensign Harry Reid Representatives Shelly Berkley (District 1) James A. Gibbons (District 2) Jon C. Porter (District 3) California Senators Barbara Boxer Dianne Feinstein Representatives John T. Doolittle (District 4) Robert T. Matsui (District 5) Doug Ose (District 3) NEVADA STATE SENATE Mark E. Amodei, Carson City Bernice Mathews, Reno Mike McGinness, Fallon William J. Raggio, Reno Randolph Townsend, Reno Maurice E. Washington, Sparks NEVADA STATE ASSEMBLY Bernie Anderson, Sparks Sharron Angle, Reno Jason Geddes, Reno Dawn Gibbons, Reno Tom Grady,Yerington Ron Knecht, Carson City Distribution List-1 Revised DEIS/EIR Truckee River Operating Agreement CALIFORNIA STATE SENATE Samuel Aanestad (District 4) Michael Machado (District 5) Thomas "Rico" Oller (District 1) Deborah Ortiz (District 6) CALIFORNIA STATE ASSEMBLY David Cox (District 5) Tim Leslie (District 4) Darrell Steinberg (District 9) FEDERAL GOVERNMENT AGENCIES Advisory Council on Historic Preservation, Washington, DC Army Corps of Engineers, Reno, NV Army Corps of Engineers, Washington, DC Army Corps of Engineers, Real Estate Division, Sacramento, CA Army Corps of Engineers, Planning Division, Sacramento, CA Bureau of Indian Affairs, Office of Trust and Economic Development, Washington, DC Bureau of Indian Affairs, Washington, DC Bureau of Indian Affairs, Western Regional Office, Phoenix, AZ Bureau of Land Management, Carson City District Office, Carson City, NV -
Cambridge University Press 978-1-108-44568-9 — Active Faults of the World Robert Yeats Index More Information
Cambridge University Press 978-1-108-44568-9 — Active Faults of the World Robert Yeats Index More Information Index Abancay Deflection, 201, 204–206, 223 Allmendinger, R. W., 206 Abant, Turkey, earthquake of 1957 Ms 7.0, 286 allochthonous terranes, 26 Abdrakhmatov, K. Y., 381, 383 Alpine fault, New Zealand, 482, 486, 489–490, 493 Abercrombie, R. E., 461, 464 Alps, 245, 249 Abers, G. A., 475–477 Alquist-Priolo Act, California, 75 Abidin, H. Z., 464 Altay Range, 384–387 Abiz, Iran, fault, 318 Alteriis, G., 251 Acambay graben, Mexico, 182 Altiplano Plateau, 190, 191, 200, 204, 205, 222 Acambay, Mexico, earthquake of 1912 Ms 6.7, 181 Altunel, E., 305, 322 Accra, Ghana, earthquake of 1939 M 6.4, 235 Altyn Tagh fault, 336, 355, 358, 360, 362, 364–366, accreted terrane, 3 378 Acocella, V., 234 Alvarado, P., 210, 214 active fault front, 408 Álvarez-Marrón, J. M., 219 Adamek, S., 170 Amaziahu, Dead Sea, fault, 297 Adams, J., 52, 66, 71–73, 87, 494 Ambraseys, N. N., 226, 229–231, 234, 259, 264, 275, Adria, 249, 250 277, 286, 288–290, 292, 296, 300, 301, 311, 321, Afar Triangle and triple junction, 226, 227, 231–233, 328, 334, 339, 341, 352, 353 237 Ammon, C. J., 464 Afghan (Helmand) block, 318 Amuri, New Zealand, earthquake of 1888 Mw 7–7.3, 486 Agadir, Morocco, earthquake of 1960 Ms 5.9, 243 Amurian Plate, 389, 399 Age of Enlightenment, 239 Anatolia Plate, 263, 268, 292, 293 Agua Blanca fault, Baja California, 107 Ancash, Peru, earthquake of 1946 M 6.3 to 6.9, 201 Aguilera, J., vii, 79, 138, 189 Ancón fault, Venezuela, 166 Airy, G. -
California State Lands Commission
STAFF REPORT 69 A 56 10/24/19 AD 671 W 503.2094 S 28 W. Crunk CONSIDER BOUNDARY LINE AND EASEMENT AGREEMENTS BETWEEN THE STATE, ACTING BY AND THROUGH THE STATE LANDS COMMISSION AND CERTAIN PROPERTY OWNERS AT DONNER LAKE PARTIES: State of California, acting by and through the State Lands Commission All those property owners along the shore of Donner Lake listed in Exhibit A, attached (collectively known as the “Property Owners”) INTRODUCTION: In November 2016, a group of Donner Lake property owners filed suit against the Commission through a recently formed corporation known as SOS Donner Lake. The Nevada County Superior Court case, SOS Donner v. California State Lands Commission, challenged the Commission’s jurisdiction over Donner Lake and the boundary between State-owned sovereign land and the privately owned uplands. The proposed Boundary Line and Easement Agreements (Agreements) will settle this litigation, settle the underlying boundary disputes, and bring finality and certainty to an area that has been in contention since the 1970s. The proposed Agreements will fix the elevation of the low-water mark that serves as the boundary between State-owned fee land in the bed of Donner Lake and the privately owned adjoining uplands. The Agreements will also fix the elevation of the high-water mark that delineates the landward extent of the Public Trust easement. The upland owners will also acknowledge the navigability of Donner Lake, thus confirming the State’s ownership of the lakebed. To effectuate the Agreements, the Commission and Property Owners will mutually grant quitclaim deeds that will confirm the parties’ respective ownership. -
Yosemite, Lake Tahoe & the Eastern Sierra
Emerald Bay, Lake Tahoe PCC EXTENSION YOSEMITE, LAKE TAHOE & THE EASTERN SIERRA FEATURING THE ALABAMA HILLS - MAMMOTH LAKES - MONO LAKE - TIOGA PASS - TUOLUMNE MEADOWS - YOSEMITE VALLEY AUGUST 8-12, 2021 ~ 5 DAY TOUR TOUR HIGHLIGHTS w Travel the length of geologic-rich Highway 395 in the shadow of the Sierra Nevada with sightseeing to include the Alabama Hills, the June Lake Loop, and the Museum of Lone Pine Film History w Visit the Mono Lake Visitors Center and Alabama Hills Mono Lake enjoy an included picnic and time to admire the tufa towers on the shores of Mono Lake w Stay two nights in South Lake Tahoe in an upscale, all- suites hotel within walking distance of the casino hotels, with sightseeing to include a driving tour around the north side of Lake Tahoe and a narrated lunch cruise on Lake Tahoe to the spectacular Emerald Bay w Travel over Tioga Pass and into Yosemite Yosemite Valley Tuolumne Meadows National Park with sightseeing to include Tuolumne Meadows, Tenaya Lake, Olmstead ITINERARY Point and sights in the Yosemite Valley including El Capitan, Half Dome and Embark on a unique adventure to discover the majesty of the Sierra Nevada. Born of fire and ice, the Yosemite Village granite peaks, valleys and lakes of the High Sierra have been sculpted by glaciers, wind and weather into some of nature’s most glorious works. From the eroded rocks of the Alabama Hills, to the glacier-formed w Enjoy an overnight stay at a Yosemite-area June Lake Loop, to the incredible beauty of Lake Tahoe and Yosemite National Park, this tour features lodge with a private balcony overlooking the Mother Nature at her best. -
Volume 30, Fall 2006
TRUCKEE DONNER LAND TRUST Preserving and protecting important historic, recreational and scenic open Fall Newsletter spaces in the greater Truckee region. Volume 30 ❖ Fall 2006 Fall 2006 Newsletter Page 2 WHEN IT RAINS, IT POURS Maybe it’s a sign of the times The Truckee Donner Land Trust was or just plain dumb luck, but founded in 1990 in order to preserve whatever the reason, there sure and protect important historic, seems to be a lot of important recreational and scenic open spaces acreage for sale right now. in the greater Truckee region. Properties the Land Trust has eyed for years are now suddenly P.O. Box 8816, Truckee, CA 96162 for sale. So many in fact, we 10069 West River Street, Old Tonini House questioned our capacity to fund I can however, talk in Tel. 530.582.4711 them all. But in the end, Board generalities. The lands we are Fax 530.582.5528 and staff concluded that all pursuing and “have not gone email: [email protected] of these lands are simply too website: www.tdlandtrust.org public with” have a combined important not to protect. We’d be value of over $40,000,000. They remiss of our mission not to try; The Truckee Donner Land Trust is a total over 6,000 acres. 501 (c)(3) nonprofit organization. All future generations will not easily donations to the Land Trust are tax- forgive us if these lands are lost Most of these properties are of deductible under the Internal Revenue to development. To paraphrase significant acreage with names Service Code. -
Yosemite National Park Foundation Overview
NATIONAL PARK SERVICE • U.S. DEPARTMENT OF THE INTERIOR Foundation Document Overview Yosemite National Park California Contact Information For more information about Yosemite National Park, Call (209) 372-0200 (then dial 3 then 5) or write to: Public Information Office, P.O. Box 577, Yosemite, CA 95389 Park Description Through a rich history of conservation, the spectacular The geology of the Yosemite area is characterized by granitic natural and cultural features of Yosemite National Park rocks and remnants of older rock. About 10 million years have been protected over time. The conservation ethics and ago, the Sierra Nevada was uplifted and then tilted to form its policies rooted at Yosemite National Park were central to the relatively gentle western slopes and the more dramatic eastern development of the national park idea. First, Galen Clark and slopes. The uplift increased the steepness of stream and river others lobbied to protect Yosemite Valley from development, beds, resulting in formation of deep, narrow canyons. About ultimately leading to President Abraham Lincoln’s signing 1 million years ago, snow and ice accumulated, forming glaciers the Yosemite Grant in 1864. The Yosemite Grant granted the at the high elevations that moved down the river valleys. Ice Yosemite Valley and Mariposa Grove of Big Trees to the State thickness in Yosemite Valley may have reached 4,000 feet during of California stipulating that these lands “be held for public the early glacial episode. The downslope movement of the ice use, resort, and recreation… inalienable for all time.” Later, masses cut and sculpted the U-shaped valley that attracts so John Muir led a successful movement to establish a larger many visitors to its scenic vistas today. -
This Report Is Preliminary and Has Not Bee Reviewed for Conformity with US
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Northeast-trending subcrustal fault transects western Washington by Kenneth F. Fox, Jr.* Open-File Report 83-398 This report is preliminary and has not bee reviewed for conformity with U.S Geological Survey editorial standards and stratigraphic nomenclature. *U.S. Geological Survey 3^5 Middlefield Road Menlo Park, California 9^025 Page Table of Contents Tectonic setting......................................................... 1 Seisraicity............................................................... 4 Discussion............................................................... 4 References cited......................................................... 6 Figures Figure 1. Magnetic anomalies in the northeastern Pacific................ 8 Figure 2. Bathymetry at intersection of Columbia lineament and Blanco fracture zone................................................. 9 Figure 3. Plane vector representation of movement of Gorda plate........ 10 Figure 4. Reconstruction of Pacific-Juan de Fuca plate geometry 2 m.y. before present................................................ 11 Figure 5. Epicenters of historical earthquakes with intensity greater than V........................................................ 12 TECTONIC SETTING The north-trending magnetic anomalies of the Juan de Fuca plate are off set along two conspicuous northeast-trending lineaments (fig. 1), named the Columbia offset and the Destruction offset by Carlson (1981). The northeast ward projections of these lineaments intersect the continental area of western Washington, hence are of potential significance to the tectonics of the Pacific Northwest region. Pavoni (1966) suggested that these lineaments were left-lateral faults, and that the Columbia, 280 km in length, had 52 km of offset, and the Destruction, with a length of 370 km, had 75 km of offset. Based on Vine's (1968) correlation of the magnetic anomalies mapped in this area by Raff and Mason (1961), with the magnetic reversal time scale, Silver (1971b, p. -
Matthew Greene Were Starting to Understand the Grave the Following Day
VANISHED An account of the mysterious disappearance of a climber in the Sierra Nevada BY MONICA PRELLE ILLUSTRATIONS BY BRETT AFFRUNTI CLIMBING.COM — 61 VANISHED Three months earlier in July, the 39-year-old high school feasted on their arms. They went hiking together often, N THE SMALL SKI TOWN of Mammoth Lakes in math teacher dropped his car off at a Mammoth auto shop even in the really cold winters common to the Northeast. California’s Eastern Sierra, the first snowfall of the for repairs. He was visiting the area for a summer climb- “The ice didn’t slow him down one bit,” Minto said. “I strug- ing vacation when the car blew a head gasket. The friends gled to keep up.” Greene loved to run, competing on the track year is usually a beautiful and joyous celebration. Greene was traveling with headed home as scheduled, and team in high school and running the Boston Marathon a few Greene planned to drive to Colorado to join other friends times as an adult. As the student speaker for his high school But for the family and friends of a missing for more climbing as soon as his car was ready. graduation, Greene urged his classmates to take chances. IPennsylvania man, the falling flakes in early October “I may have to spend the rest of my life here in Mam- “The time has come to fulfill our current goals and to set moth,” he texted to a friend as he got more and more frus- new ones to be conquered later,” he said in his speech. -
Mountain Whitefish Chances for Survival: Better 4 Prosopium Williamsoni
Mountain Whitefish chances for survival: better 4 Prosopium williamsoni ountain whitefish are silvery in color and coarse-scaled with a large and the mackenzie and hudson bay drainages in the arctic. to sustain whatever harvest exists today. mountain whitefish in California and Nevada, they are present in the truckee, should be managed as a native salmonid that is still persisting 1 2 3 4 5 WHITEFISH adipose fin, a small mouth on the underside of the head, a short Carson, and Walker river drainages on the east side of in some numbers. they also are a good indicator of the dorsal fin, and a slender, cylindrical body. they are found the sierra Nevada, but are absent from susan river and “health” of the Carson, Walker, and truckee rivers, as well as eagle lake. lake tahoe and other lakes where they still exist. Whitefish m Mountain Whitefish Distribution throughout western North america. While mountain whitefish are regarded aBundanCe: mountain whitefish are still common in populations in sierra Nevada rivers and tributaries have California, but they are now divided into isolated popula- been fragmented by dams and reservoirs, and are generally as a single species throughout their wide range, a thorough genetic analysis tions. they were once harvested in large numbers by Native scarce in reservoirs. a severe decline in the abundance of americans and commercially harvested in lake tahoe. mountain whitefish in sagehen and prosser Creeks followed would probably reveal distinct population segments. the lahontan population there are still mountain whitefish in lake tahoe, but they the construction of dams on each creek. -
Central Nevada
University of Nevada Reno LATE CENOZOIC GEOLOGY AND TECTONICS OF STEWART AND MONTE CRISTO VALLEYS, WEST - CENTRAL NEVADA A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science .I by Mark Philip Molinari fit ; December, 1984 ii ABSTRACT Discontinuous right-normal-slip faults comprise the N30 0W trending, 45 kilometer long Stewart - Monte Cristo fault zone (SMCFZ). Initiation of the SMCFZ postdates the 15.5 to 11.0 m.y. Esmeralda Formation. Right-normal-slip >1 meter occurred on the southern segment of the SMCFZ during the 1932 Cedar Mountain earthquake (Ms= 7.2-7.3). Geomor- phic evidence supports at least three and possibly five or six surface faulting events on the southern segment during the latest Pleistocene and Holocene. Gentle folds in the Esmeralda Formation east of and sub-parallel to the SMCFZ are coeval with and genetically related to faulting. Structural development of the SMCFZ is similar to other right-lateral wrench faults and is consistent with labora- tory wrench fault models. The SMCFZ is the youngest and southeasternmost fault of a system of major late Cenozoic, left-stepping, en echelon right-slip faults in the central Walker Lane. - .~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ iii TABLE OF CONTENTS page ABSTRACT .................. S S ii INTRODUCTION . 0 0 1 0 * I Location and Extent of Study Area . S S S S 1 Regional Tectonic and Geologic Setting. S. S a * 0 1 Purpose and Scope ...... a a * a 5 Methodology . 6 Previous Work . 8 Physiography. 10 MESOZOIC STRATIGRAPHY. 13 Sedimentary Rocks . & 13 Mina Formation . 13 Luning Formation . 13 Plutonic Rocks .