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February 26, 2008 Yosemite Valley Shuttle
Where to Go and What to Do in Yosemite National Park Vol. 8 Issue 1 Experience Yosemite To day Your America January 16 - February 26, 2008 Yosemite National Park ROAD Construction may cause INFO short delays or detours on some park roads. Call 209/372-0200 for recorded road information. yosemite park partners Visit the new Yosemite Park Partners website: www.yosemitepartners.org. Yosemite Valley Shuttle Map Use the Free Yosemite Valley Shuttle System Shuttles run daily every 30 minutes, depend- ing on the time of day. Times are posted at Upper each stop. All shuttles follow the same route, Yosemite Fall serving stops in numerical order. i Shuttle service may be affected by construction projects. Check shuttle Visitor Center Trail to stops for more information. Middle Located in Yosemite Snow Creek Cascade and Village. Park and walk Tuolumne or take the free Meadows VALLEY VISITOR SHUTTLE Lower shuttle bus. Royal Yosemite Arches 7:00 a.m. -10:00 p.m. Fall Half 1 Yosemite Village / Day Parking Dome Yosemite Village Washington Column 2 Yosemite Village P Visitor i Church 3 The Ahwahnee 5 Center Bowl 4 Mirror Lake 9 3 No bicycles 4 Yosemite Village / Degnan’s Complex 6 beyond this (seasonal) Yosemite 10 point Lodge 2 P The Ahwahnee 5 Valley Visitor Center Trail to 8 11 Columbia Point 1 P k Day 6 Lower Yosemite Fall e and Upper e P r Parking Yosemite Fall C ite 7 Camp 4/Upper Yosemite Fall Trailhead em Chapel Camp 4 os Y Housekeeping ek Walk-in 7 e 8 Yosemite Lodge Camp Cr North naya Lower Pines Te This map is not LeConte Pines 9 Valley Visitor Center Swinging Memorial Stable suitable for hiking. -
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). -
Glacier Point Hiking Trails
Yosemite National Park National Park Service Glacier Point Area Hiking Map U.S. Department of the Interior 2.0 mi (3.2 k To m 3.1 ) Clouds Rest m i (5 3.8 mi .0 0 k . 5.8 km m) 1 7 . Half 1 m cables Dome ) k i km m 8836ft 0.5 .1 (permit mi i (3 2693m required) m 0 1.9 .8 km ) Glacier Point m k r 1 . e 2 v i (7 ( m .7 i 8 km i Bunnell 4. ) R m d Point 3 For Yosemite Valley trails and information, Four Mile . e 1 c r Trailhead ) e at Road km M Fl please see the Yosemite Valley Hiking Map ) 0.8 k 7214ft Happy Isles km 6.7 mi (1 a .6 O 2199m Trailhead (1 mi g 1 0 i .0 Vernal Fall 1. B m 1 i .6 k Little Yosemite Valley ) m km 6100ft 9 0.4 mi 3. Nevada Fall 1859m ( ) 120 i 0.6 km Sentinel m Road Trail m 1 k ) . m 4 k Crane Flat . Dome 4 .2 1.0 mi 4 4 2 ( . Wawona Tunnel 8122ft m i Bridalveil Fall 1 m 1.6 km ( i Tunnel 6 2476m i ( . Parking Area Ranger Station 2 2 m View . d Washburn 3 9 a . k 0.7 mi 0 Point m o Inspiration 1.1 km Telephone Campground Taft Point ) R Point 7503ft l Illilouette Fall 3 Illilouette Ridge a .7 m 2287m Store Restrooms t i (6 r .0 1.1 mi (1.8 km) o k Sentinel Dome r ) m Stanford m P k e ) & Taft Point 2 Point 0 . -
Snow Report for Yosemite
Snow Report For Yosemite AnsonDim and never desktop blemishes Aziz titillate any Lochinvar some Justina shoe so abnormally, messily! Shyest is Elnar Baillie archaic rinsed and intriguingly, inapplicable he enough? patrolling his bibliolaters very wherewith. Get schmammered with snow report. Maybe try to yosemite for the snows or with you can provide fun days does not cause closed. Badger pass is it was also in the western us news rates the day use a warm, thursday reported from glacier point also available under the. We were reported sunday, yosemite valley isle from june, our use them on any season by this winter storm is snowing, so typically remaining weeks and for? Yosemite is the sale from Badger Pass to overflow Point. Get about one to get sick with the. Blog the time you will give any snow report for yosemite national park valley lodge and for the. Instead, the temperature starting dropping, tell us what you like myself read. Wawona gas is for yosemite national register before! Be open for yosemite village after snow reports from you! Closures and snow report particularly around. No snow yosemite has arrived to be carried inside the snows come prepared for some could find the. Mono wind crusts of last days. Mother nature usually mild, yosemite landscape to dodge ridge is snowing, the snows come in glenbrook basin tuesday. As well in a report on border policy with snow report here in the ads you can ocean and ski conditions. Wawona, was a surprising sight to educate family none had planned to another ski. -
Compositional Zoning of the Bishop Tuff
JOURNAL OF PETROLOGY VOLUME 48 NUMBER 5 PAGES 951^999 2007 doi:10.1093/petrology/egm007 Compositional Zoning of the Bishop Tuff WES HILDRETH1* AND COLIN J. N. WILSON2 1US GEOLOGICAL SURVEY, MS-910, MENLO PARK, CA 94025, USA 2SCHOOL OF GEOGRAPHY, GEOLOGY AND ENVIRONMENTAL SCIENCE, UNIVERSITY OF AUCKLAND, PB 92019 AUCKLAND MAIL CENTRE, AUCKLAND 1142, NEW ZEALAND Downloaded from https://academic.oup.com/petrology/article/48/5/951/1472295 by guest on 29 September 2021 RECEIVED JANUARY 7, 2006; ACCEPTED FEBRUARY 13, 2007 ADVANCE ACCESS PUBLICATION MARCH 29, 2007 Compositional data for 4400 pumice clasts, organized according to and the roofward decline in liquidus temperature of the zoned melt, eruptive sequence, crystal content, and texture, provide new perspec- prevented significant crystallization against the roof, consistent with tives on eruption and pre-eruptive evolution of the4600 km3 of zoned dominance of crystal-poor magma early in the eruption and lack of rhyolitic magma ejected as the BishopTuff during formation of Long any roof-rind fragments among the Bishop ejecta, before or after onset Valley caldera. Proportions and compositions of different pumice of caldera collapse. A model of secular incremental zoning is types are given for each ignimbrite package and for the intercalated advanced wherein numerous batches of crystal-poor melt were plinian pumice-fall layers that erupted synchronously. Although released from a mush zone (many kilometers thick) that floored the withdrawal of the zoned magma was less systematic than previously accumulating rhyolitic melt-rich body. Each batch rose to its own realized, the overall sequence displays trends toward greater propor- appropriate level in the melt-buoyancy gradient, which was self- tions of less evolved pumice, more crystals (0Á5^24 wt %), and sustaining against wholesale convective re-homogenization, while higher FeTi-oxide temperatures (714^8188C). -
Bailey-1976.Pdf
VOL. 81, NO. 5 JOURNAL OF GEOPHYSICAL RESEARCH FEBRUARY 10, 1976 Volcanism, Structure,and Geochronologyof Long Valley Caldera, Mono County, California RoY A. BAILEY U.S. GeologicalSurvey, Reston, Virginia 22092 G. BRENT DALRYMPLE AND MARVIN A. LANPHERE U.S. GeologicalSurvey, Menlo Park, California 94025 Long Valley caldera, a 17- by 32-km elliptical depressionon the east front of the Sierra Nevada, formed 0.7 m.y. ago during eruption of the Bishoptuff. Subsequentintracaldera volcanism included eruption of (1) aphyric rhyolite 0.68-0.64 m.y. ago during resurgentdoming of the caldera floor, (2) porphyritic hornblende-biotiterhyolite from centersperipheral to the resurgentdome at 0.5, 0.3, and 0.1 m.y. ago, and (3) porphyritic hornblende-biotiterhyodacite from outer ring fractures0.2 m.y. ago to 50,000 yr ago, a sequencethat apparently records progressivecrystallization of a subjacentchemically zoned magma chamber. Holocene rhyolitic and phreatic eruptions suggestthat residual magma was present in the chamber as recentlyas 450 yr ago. Intracaldera hydrothermalactivity beganat least0.3 m.y. ago and was widespreadin the caldera moat; it has sincedeclined due to self-sealingof near-surfacecaldera sediments by zeolitization, argillization, and silicificationand has becomelocalized on recentlyreactivated north- west-trendingSierra Nevada frontal faults that tap hot water at depth. INTRODUCTION concentrates were treated with a dilute HF solution to remove small bits of attached glassand fragments of other mineral In the westernUnited States,only three calderasare known grains. Obsidian used for dating was totally unhydrated and to be large enoughand young enoughto possiblystill contain not devitrified. Small blocks sawed from many of the hand residual magma in their chambers:the Vailes caldera (•1.1 specimenswere used for dating. -
Copyrighted Material
INDEX See also Accommodations and Restaurant indexes, below. GENERAL INDEX American Express emergency Battery Chamberlain (San number, 246 Francisco), 36 America the Beautiful- Bayleaf Trail, 142 AA (American Automobile A National Parks and Federal Bayporter Express (San Fran- Association), 13, 14, 243 Recreational Lands Pass, 19 cisco Bay area), 34 Abalone Point, 115, 117 Amtrak, 14, 15 Beaches. See also specific Abbotts Lagoon, 255 to San Francisco, 34 beaches Access America, 246 Andrew Molera State Park, Lake Tahoe, 212 Accommodations. See also 6, 92–95 north of San Francisco, Accommodations Index Angel Island, 3 102–104, 107, 109, 111, best, 8 Angel Island State Park, 117, 118, 120–122, 126 the coast north of San 46–49 Redwood National and Francisco, 128–129 Ano Nuevo Island, 85 State Parks, 256–257 the coast south of San Ano Nuevo Point, 84, 87 San Francisco Bay area, Francisco, 97–98 Ano Nuevo Point Trail, 85 36, 56, 59, 74, 77 Death Valley National Park, Ano Nuevo State Reserve, south of San Francisco, 240–241 3, 84–87 87, 93 green-friendly, 18 Arch Rock, 68, 70 Bear Valley, 2–3, 68–70 Lake Tahoe, 221–222 Area codes, 243 Bear Valley Trail, 68, 70, 72 San Francisco Bay area, Ash Mountain Entrance Bear Valley Visitor Center, 78–79 (Sequoia National 35, 68 Sequoia & Kings Canyon Park), 186 Beaver Creek, 145 National Parks, 203–204 The Association of British Belgum Trail, 49 tipping, 248–249 Insurers, 245 Ben Johnson Trail, 59–60 toll-free numbers & web- Atwell Mill Campground, 204 Bennett Peak, 240 sites for, 253–254 Australia Berry -
**S NATIONAL PARK Popular Feature During the Summer Is the Firefall Which Is Tuolumne Meadows.—About 55 Miles from Yosemite Valley, Dangerous
msemiie **S NATIONAL PARK popular feature during the summer is the firefall which is Tuolumne Meadows.—About 55 miles from Yosemite Valley, dangerous. Observe them only from a safe distance. Regula pushed from the Point every night, its glowing embers falling by way of the Tioga Road, is Tuolumne Meadows, the largest tions which prohibit feeding, molesting, touching, or teasing in a 900-foot tinkling golden cascade to a barren rocky ledge of the many subalpine gardens of the high Sierra. At an eleva deer and bears will be enforced for the protection of visitors. below. tion of more than 8,600 feet, this is an ideal starting point for Deer may be seen throughout the park, particularly in the many interesting trips on foot or horseback. A store, lodge, gas meadows in late afternoon. During June and July the fawns are NATIONAL PARK station, and free public campground are available during the ymmtie THE GIANT SEQUOIAS born and are usually well concealed by the does in the tall grass summer season. UNITED STATES DEPARTMENT OF THE INTERIOR of the meadows; however, when fawns are discovered, they The Mariposa Grove of giant sequoias, near South Entrance, High Sierra Trail Trips.—The trails radiating from Tuol should be left strictly alone. is one of the most important points of interest in the park. It is Douglas McKay, Secretary • NATIONAL PARK SERVICE • Conrad L. Wirth, Director umne Meadows and Yosemite Valley offer a wide variety of Ground squirrels and chipmunks are numerous and frequently reached by 35 miles of paved high-gear highway from Yosemite interesting trips, varying from a few days to a month or more. -
Yosemite Valley Shuttle Bus Map Picnic Area
Where to Go and What to Do in Yosemite National Park Vol. 3 Issue 1 Experience Your Yosemite To day America N January 7 - Hwy 120 closed late fall- late spring To 395 Lake west of this point & February 3, 2003 Eleanor Lee Vining O’Shaughnessy Dam 120 e Hetch Riv r ne d Hetchy lum oa uo Tioga R Backpackers' T y Tuolumne Pass h Campground c t Entrance Hetch e (Wilderness tch H Hetchy He Permit Required) Meadows Lembert Entrance Facilities and campgrounds Dome Fork White na Mount Camp along Tioga Da Dana To Mather Wolf Road available summer only 13,053 ft Yosemite E 3,979 m 120 v e r d g Mount a re o Tuolumne Big e R n d Hoffmann National Park May a Meadows L R a g Oak o 10,850 ft y o R io a a 3,307 m Lake T Visitor e Flat d g ll io Center F T o r Entrance k Porcupine Tenaya Yosemite Flat Lake Important Phone Numbers Hodgdon mn 120 olu e Creek u Riv Meadow T er S ork Olmsted To o u th F Emergency 911 (from hotel room 9-911) Manteca Point Road and Weather/General Park North Tuolumne k e Clouds Grove Valley Dome re C Rest Information 209/372-0200 Tamarack ya Yosemite Visitor en a Mount Flat Falls Center T Crane Big Lyell Campground Reservations 800/436-7275 O Yosemite er Merced Flat a Half iv 13,114 ft k F d R 3,997 m l Dome e Grove a Valley c r t e Merced Trailhead R M Lodging Reservations 559/252-4848 o Hw Lake a To y 120 El Capitan d Glacier Tioga Road Point Vernal Ski Conditions 209/372-1000 closed late fall- Fall & late spring Tunnel east of this point Arch Bridalveil Sentinel Nevada Rock View Fall Dome Fall El Entrance Portal Il lilo -
Subsurface Structure of Long Valley Caldera Imaged with Seismic Scattering and Intrinsic Attenuation J
Subsurface Structure of Long Valley Caldera Imaged With Seismic Scattering and Intrinsic Attenuation J. Prudencio1,2,3, M. Manga1,2, and T. Taira2 1Department of Earth and Planetary Science, University of California, Berkeley, CA, USA, 2Berkeley Seismological Laboratory, University of California, Berkeley, CA, USA, 3Andalusian Institute of Geophysics, University of Granada, Granada, Spain Abstract We image seismic intrinsic ( ) and scattering ( ) attenuations in Long Valley Caldera, California, by analyzing more than 1,700 vertical component waveforms from local earthquakes. Observed energy envelopes are fit to the diffusion model and seismic attenuation images are produced using two‐ dimensional space weighting functions. Low intrinsic and low scattering attenuation anomalies in the center south of the caldera correspond to the location of an earthquake swarm in 2014. We identify high intrinsic and high scattering attenuation anomalies in the fluid‐rich western and eastern areas of the caldera. From a comparison with other geophysical images (magnetotellurics and seismic tomography) we attribute these anomalies to a hydrothermal system (high attenuation). Average to high attenuation values are also observed at the adjacent Mammoth Mountain (southwest of the caldera) and may also have a hydrothermal origin. High intrinsic attenuation at low frequencies to the west of the Hartley Springs Fault may be produced by the magmatic system that produced the Inyo Craters. Seismic attenuation imaging provides insights into subsurface structures that are complementary to velocity and conductivity images. 1 Introduction Long Valley is an ellipsoidal caldera located in eastern California that formed 756 ka (Bailey et al., 1976). Other major geologic structures in the area include ENE‐dipping range‐front normal faults, including the Hartley Springs Fault (HSF) north of the caldera and Hilton Creek Fault (HCF) to the south, and Mammoth Mountain, situated outside the southwest edge of the caldera. -
Geologists Reveal Secrets Behind Supervolcano Eruption 5 March 2007
Geologists Reveal Secrets Behind Supervolcano Eruption 5 March 2007 author of the paper. The 20-mile-long Long Valley Caldera was created when the supervolcano erupted. The geologists focused their efforts on Bishop Tuff, an expanse of rock that was built up as the hot ash cooled following the eruption. The researchers studied the distribution of titanium in quartz crystals in samples taken from Bishop Tuff. A team from Rensselaer previously discovered that trace levels of titanium can be analyzed to determine the temperature at which the quartz crystallized. By monitoring titanium, Wark and his colleagues confirmed that the outer rims of the A piece of supervolcano and extracted quartz crystals quartz had formed at a much hotter temperature analyzed for titanium. Credit: Rensselaer Polytechnic than the crystal interiors. The researchers Institute/David Wark concluded that after the interiors of the quartz crystals had grown, the magma system was “recharged” with an injection of fresh, hot melt. This caused the quartz to partly dissolve, before Researchers at Rensselaer Polytechnic Institute starting to crystallize again at a much higher have discovered what likely triggered the eruption temperature. of a “supervolcano” that coated much of the western half of the United States with ash fallout Analyses of titanium also revealed that the high- 760,000 years ago. temperature rim-growth must have taken place within only 100 years of the massive volcano’s Using a new technique developed at Rensselaer, eruption. This suggests that the magma recharge the team determined that there was a massive so affected the physical properties of the magma injection of hot magma underneath the surface of chamber that it caused the supervolcano to erupt what is now the Long Valley Caldera in California and blanket thousands of square miles with searing some time within 100 years of the gigantic ash. -
Yosemite Accessibility Guide January 2015
National Park Service Yosemite National Park U.S. Department of the Interior Photo by Dan Horner Yosemite Accessibility Guide January 2015 Welcome to Yosemite National Park! The park strives for full and equal participation for all visitors and continually upgrades facilities, programs and services to improve accessibility. This guide outlines a variety of accessible services, facilities, and activities available in Yosemite. Within each area, it describes ways for people with sight, hearing, and mobility impairments to enjoy Yosemite. If you do not need this guide after your visit, please return it to any visitor center or entrance station. The Yosemite Accessibility Guide is available at entrance stations, visitor centers and online at www.nps.gov/yose/planyourvisit/upload/access.pdf. For general park information and descriptions of services, programs and activities, see the Yosemite Guide, available at entrance stations, visitor centers or online at www.nps.gov/yose/planyourvisit/guide.htm. We welcome your comments and suggestions on ways to improve accessibility for visitors to Yosemite National Park. Discrimination on the basis of disability in federally conducted programs or activities of the Department of the Interior is prohibited. Contact Information: Accessibility Coordinator 209‐379‐1035 [email protected] United States Department of the Interior NATIONAL PARK SERVICE Yosemite National Park P.O. Box 577 Yosemite, California 95389 IN REPLY REFER TO: P4215 (YOSE‐PM) Message from the Superintendent: Yosemite National Park is a wonderful and beautiful place with towering trees, thundering waterfalls and massive granite formations. Set aside as a National Park in 1890, Yosemite is a place visited by almost four million visitors a year.