Yosemite, Lake Tahoe & the Eastern Sierra
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Geologic Map of the Long Valley Caldera, Mono-Inyo Craters
DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP 1-1933 US. GEOLOGICAL SURVEY GEOLOGIC MAP OF LONG VALLEY CALDERA, MONO-INYO CRATERS VOLCANIC CHAIN, AND VICINITY, EASTERN CALIFORNIA By Roy A. Bailey GEOLOGIC SETTING VOLCANISM Long Valley caldera and the Mono-Inyo Craters Long Valley caldera volcanic chain compose a late Tertiary to Quaternary Volcanism in the Long Valley area (Bailey and others, volcanic complex on the west edge of the Basin and 1976; Bailey, 1982b) began about 3.6 Ma with Range Province at the base of the Sierra Nevada frontal widespread eruption of trachybasaltic-trachyandesitic fault escarpment. The caldera, an east-west-elongate, lavas on a moderately well dissected upland surface oval depression 17 by 32 km, is located just northwest (Huber, 1981).Erosional remnants of these mafic lavas of the northern end of the Owens Valley rift and forms are scattered over a 4,000-km2 area extending from the a reentrant or offset in the Sierran escarpment, Adobe Hills (5-10 km notheast of the map area), commonly referred to as the "Mammoth embayment.'? around the periphery of Long Valley caldera, and The Mono-Inyo Craters volcanic chain forms a north- southwestward into the High Sierra. Although these trending zone of volcanic vents extending 45 km from lavas never formed a continuous cover over this region, the west moat of the caldera to Mono Lake. The their wide distribution suggests an extensive mantle prevolcanic basement in the area is mainly Mesozoic source for these initial mafic eruptions. Between 3.0 granitic rock of the Sierra Nevada batholith and and 2.5 Ma quartz-latite domes and flows erupted near Paleozoic metasedimentary and Mesozoic metavolcanic the north and northwest rims of the present caldera, at rocks of the Mount Morrisen, Gull Lake, and Ritter and near Bald Mountain and on San Joaquin Ridge Range roof pendants (map A). -
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. -
State of Sierra Frogs
State of Sierra Frogs A report on the status of frogs & toads in the Sierra Nevada & California Cascade Mountains State of Sierra Frogs A report on the status of frogs & toads in the Sierra Nevada & California Cascade Mountains By Marion Gee, Sara Stansfield, & Joan Clayburgh July 2008 www.sierranevadaalliance.org State of Sierra Frogs 1 Acknowledgements The impetus for this report was the invaluable research on pesticides by Carlos Davidson, professor at San Francisco State University. Davidson, along with Amy Lind (US Forest Service), Curtis Milliron (California Department of Fish and Game), David Bradford (United States Environmental Protection Agency) and Kim Vincent (Graduate Student, San Francisco State University), generously donated their time and expertise to speak at two public workshops on the topics of Sierra frogs and toads as well as to provide comments for this document. Our thanks to the other reviewers of this manuscripts including Bob Stack (Jumping Frog Research Institute), Katie Buelterman, Dan Keenan, and Genevieve Jessop Marsh. This project was fortunate to receive contributions of photography and artwork from John Muir Laws, Elena DeLacy, Bob Stack, Ralph & Lisa Cutter and Vance Vredenburg. Photo credits are found with each caption. This work was made possible by generous grants from the Rose Foundation for Communities and the Environment and the State Water Resources Control Board. Funding for this project has been provided in part through an Agreement with the State Water Resources Control Board (SWRCB) pursuant to the Costa-Machado Water Act of 2000 (Proposition 13) and any amendments thereto for the implementation of California’s Non-point Source Pollution Control Program. -
City of South Lake Tahoe Municipal Services Review and Sphere of Influence Update
Agenda Item #4E Page 1 of 99 PUBLIC REVIEW DRAFT EL DORADO LOCAL AGENCY FORMATION COMMISSION (LAFCO) CITY OF SOUTH LAKE TAHOE MUNICIPAL SERVICES REVIEW AND SPHERE OF INFLUENCE UPDATE MAY 2016 Agenda Item #4E Page 2 of 99 PUBLIC REVIEW DRAFT CITY OF SOUTH LAKE TAHOE MUNICIPAL SERVICES REVIEW AND SPHERE OF INFLUENCE UPDATE Prepared for: El Dorado Local Agency Formation Commission 550 Main Street Placerville, CA 95667 Contact Person: Jose Henriquez, Executive Officer Phone: (530) 295-2707 Consultant: 6051 N. Fresno Street, Suite 200 Contact: Steve Brandt, Project Manager Phone: (559) 733-0440 Fax: (559) 733-7821 May 2016 © Copyright by Quad Knopf, Inc. Unauthorized use prohibited. Cover Photo: City of South Lake Tahoe 150245 Agenda Item #4E Page 3 of 99 EL DORADO LOCAL AGENCY FORMATION COMMISSION Commissioners Shiva Frentzen, El Dorado County Representative Brian Veerkamp, El Dorado County Representative Mark Acuna, City Representative Austin Sass, City Representative Dale Coco, MD, Special District Representative Ken Humphreys, Chair, Special District Representative Dyana Anderly, Public Member Representative Alternate Commissioners John Clerici, City Representative Niles Fleege, Public Member Representative Holly Morrison, Special District Representative Michael Ranalli, El Dorado County Representative Staff Jose Henriquez, Executive Officer Erica Sanchez, Policy Analyst Denise Tebaldi, Interim Commission Clerk Legal Counsel Kara Ueda, LAFCO Counsel Consultant 6051 N. Fresno, Suite 200 Fresno, CA 93710 Copyright by Quad Knopf, Inc. Unauthorized use prohibited. © 150245 Agenda Item #4E Page 4 of 99 TABLE OF CONTENTS SECTION 1 - Introduction ............................................................................................................................... 1-1 1.1 - Role and Responsibility of Local Agency Formation Commission (LAFCo) ...... 1-1 1.2 - Municipal Service Review Purpose ................................................................................... -
Inyo National Forest Visitor Guide
>>> >>> Inyo National Forest >>> >>> >>> >>> >>> >>> >>> >>> >>> >>> >>> Visitor Guide >>> >>> >>> >>> >>> $1.00 Suggested Donation FRED RICHTER Inspiring Destinations © Inyo National Forest Facts “Inyo” is a Paiute xtending 165 miles Bound ary Peak, South Si er ra, lakes and 1,100 miles of streams Indian word meaning along the California/ White Mountain, and Owens River that provide habitat for golden, ENevada border between Headwaters wildernesses. Devils brook, brown and rainbow trout. “Dwelling Place of Los Angeles and Reno, the Inyo Postpile Nation al Mon ument, Mam moth Mountain Ski Area National Forest, established May ad min is tered by the National Park becomes a sum mer destination for the Great Spirit.” 25, 1907, in cludes over two million Ser vice, is also located within the mountain bike en thu si asts as they acres of pris tine lakes, fragile Inyo Na tion al For est in the Reds ride the chal leng ing Ka mi ka ze Contents Trail from the top of the 11,053-foot mead ows, wind ing streams, rugged Mead ow area west of Mam moth Wildlife 2 Sierra Ne va da peaks and arid Great Lakes. In addition, the Inyo is home high Mam moth Moun tain or one of Basin moun tains. El e va tions range to the tallest peak in the low er 48 the many other trails that transect Wildflowers 3 from 3,900 to 14,494 feet, pro vid states, Mt. Whitney (14,494 feet) the front coun try of the forest. Wilderness 4-5 ing diverse habitats that sup port and is adjacent to the lowest point Sixty-five trailheads provide Regional Map - North 6 vegetation patterns ranging from in North America at Badwater in ac cess to over 1,200 miles of trail Mono Lake 7 semiarid deserts to high al pine Death Val ley Nation al Park (282 in the 1.2 million acres of wil der- meadows. -
Snow Hydrology with Dr
Snow Hydrology with Dr. Ned Bair Ologies Podcast January 14, 2019 Oh hey, it’s that blueberry bagel that tastes like onions ‘cause it pressed its face into an everything bagel. Alie Ward, back with another episode of Ologies. It’s the middle of January, and here in the northern hemisphere, lips are chapped, feet are cold, parkas are on. I’m here to give you a snow job. But first, thank you to everyone who supports on Patreon, and who gets merch, including the new black t-shirts (yes!) at OlogiesMerch.com. Of course, thanks to everyone who rates and subscribes, who leaves reviews on iTunes, you know I read them. You know I read them. For example, this week, thank you to Evie, who said, In the hopes of Alie noticing me [heeyyy], I gotta say that this podcast just recently got me through some pretty bad flying anxiety. So thank you. Thank you for taking me into the sky with you, Evie. Also, EvanDK, I hope you and your pops are feeling okay. Okay, so: snow. Snow! Not just snow, but big cold crumbly scary dangerous avalanches. What the hell are they? I searched far and wide for a snow expert, and I connected with a dude who got his Ph.D. in Environmental Science and Management from University of California, Santa Barbara, a place Steven Ray Morris and I both attended, but this guy is primarily based up near Mammoth Mountain, which is technically a giant lava dome complex. Freakin’ volcano, near Yosemite. It’s chill. -
The History of Valentine Camp by Mary Farrell
History of Valentine Camp Mary M. Farrell Trans-Sierran Archaeological Research P.O. Box 840 Lone Pine, CA 93545 November 7, 2015 Prepared for Valentine Eastern Sierra Reserve University of California, Santa Barbara, Natural Reserve System Sierra Nevada Aquatic Research Laboratory 1016 Mt. Morrison Road Mammoth Lakes, CA 93546 Abstract Located in Mammoth Lakes, California, Valentine Camp and the nearby Sierra Nevada Aquatic Research Laboratory form the Valentine Eastern Sierra Reserve, a field research station in the University of California's Natural Reserve System. The University’s tenure at Valentine Camp began over 40 years ago, but the area’s history goes back thousands of years. Before the arrival of Euroamericans in the nineteenth century, the region was home to Paiutes and other Native American tribes. Land just east of Valentine Camp was surveyed under contract with the United States government in 1856, and mineral deposits in the mountains just west of Valentine Camp brought hundreds of miners to the vicinity in the last decades of the nineteenth century. Even as mining in the region waned, grazing increased. The land that became Valentine Camp was patented in 1897 by Thomas Williams, a rancher and capitalist who lived in Owens Valley. It was Williams’s son, also Thomas, who sold the 160 acres to Valentine Camp’s founders. Those founders were very wealthy, very influential men in southern California who could have, and did, vacation wherever they wanted. Anyone familiar with the natural beauty of Mammoth Lakes would not be surprised that they chose to spend time at Valentine Camp. Valentine Camp was donated to the University of California Natural Land and Water Reserve System (now the Natural Reserve System) in 1972 to ensure the land’s continued protection. -
Consequences of Drying Lake Systems Around the World
Consequences of Drying Lake Systems around the World Prepared for: State of Utah Great Salt Lake Advisory Council Prepared by: AECOM February 15, 2019 Consequences of Drying Lake Systems around the World Table of Contents EXECUTIVE SUMMARY ..................................................................... 5 I. INTRODUCTION ...................................................................... 13 II. CONTEXT ................................................................................. 13 III. APPROACH ............................................................................. 16 IV. CASE STUDIES OF DRYING LAKE SYSTEMS ...................... 17 1. LAKE URMIA ..................................................................................................... 17 a) Overview of Lake Characteristics .................................................................... 18 b) Economic Consequences ............................................................................... 19 c) Social Consequences ..................................................................................... 20 d) Environmental Consequences ........................................................................ 21 e) Relevance to Great Salt Lake ......................................................................... 21 2. ARAL SEA ........................................................................................................ 22 a) Overview of Lake Characteristics .................................................................... 22 b) Economic -
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. -
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. -
Chapter 8 Manzanar
CHAPTER 8 MANZANAR Introduction The Manzanar Relocation Center, initially referred to as the “Owens Valley Reception Center”, was located at about 36oo44' N latitude and 118 09'W longitude, and at about 3,900 feet elevation in east-central California’s Inyo County (Figure 8.1). Independence lay about six miles north and Lone Pine approximately ten miles south along U.S. highway 395. Los Angeles is about 225 miles to the south and Las Vegas approximately 230 miles to the southeast. The relocation center was named after Manzanar, a turn-of-the-century fruit town at the site that disappeared after the City of Los Angeles purchased its land and water. The Los Angeles Aqueduct lies about a mile to the east. The Works Progress Administration (1939, p. 517-518), on the eve of World War II, described this area as: This section of US 395 penetrates a land of contrasts–cool crests and burning lowlands, fertile agricultural regions and untamed deserts. It is a land where Indians made a last stand against the invading white man, where bandits sought refuge from early vigilante retribution; a land of fortunes–past and present–in gold, silver, tungsten, marble, soda, and borax; and a land esteemed by sportsmen because of scores of lakes and streams abounding with trout and forests alive with game. The highway follows the irregular base of the towering Sierra Nevada, past the highest peak in any of the States–Mount Whitney–at the western approach to Death Valley, the Nation’s lowest, and hottest, area. The following pages address: 1) the physical and human setting in which Manzanar was located; 2) why east central California was selected for a relocation center; 3) the structural layout of Manzanar; 4) the origins of Manzanar’s evacuees; 5) how Manzanar’s evacuees interacted with the physical and human environments of east central California; 6) relocation patterns of Manzanar’s evacuees; 7) the fate of Manzanar after closing; and 8) the impact of Manzanar on east central California some 60 years after closing. -
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.