Lassen Volcanic National Park California
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Area Adventure Hat Creek Ranger District Lassen National Forest
Area Adventure Hat Creek Ranger District Lassen National Forest Welcome The following list of recreation activities are avail- able in the Hat Creek Recreation Area. For more detailed information please stop by the Old Station Visitor Information Center, open April - December, or our District Office located in Fall River Mills. Give Hat Creek Rim Overlook - Nearly 1 million years us a call year-around Mon.- Fri. at (530) 336-5521. ago, active faulting gradually dropped a block of Enjoy your visit to this very interesting country. the Earth’s crust (now Hat Creek Valley) 1,000 feet below the top of the Hat Creek Rim, leaving behind Subway Cave - See an underground cave formed this large fault scarp. This fault system is still “alive by flowing lava. Located just off Highway 89, 1/4 and cracking”. mile north of Old Station junction with Highway 44. The lava tube tour is self guided and the walk is A heritage of the Hat Creek area’s past, it offers mag- 1/3 mile long. Bring a lantern or strong flashlight nificent views of Hat Creek Valley, Lassen Peak, as the cave is not lighted. Sturdy Shoes and a light Burney Mountain, and, further away, Mt. Shasta. jacket are advisable. Subway Cave is closed during the winter months. Fault Hat Creek Rim Fault Scarp Vertical movement Hat Creek V Cross Section of a Lava Tube along this fault system alley dropped this block of earth into its present position Spattercone Trail - Walk a nature trail where volca- nic spattercones and other interesting geologic fea- tures may be seen. -
Geologic Gems of California's State Parks
STATE OF CALIFORNIA – EDMUND G. BROWN JR., GOVERNOR NATURAL RESOURCES AGENCY – JOHN LAIRD, SECRETARY CALIFORNIA GEOLOGICAL SURVEY DEPARTMENT OF PARKS AND RECREATION – LISA MANGAT, DIRECTOR JOHN D. PARRISH, Ph.D., STATE GEOLOGIST DEPARTMENT OF CONSERVATION – DAVID BUNN, DIRECTOR PLATE 1 The rugged cliffs of Del Norte Coast Redwoods State Park are composed of some of California’s Bio-regions the most tortured, twisted, and mobile rocks of the North American continent. The California’s Geomorphic Provinces rocks are mostly buried beneath soils and covered by vigorous redwood forests, which thrive in a climate famous for summer fog and powerful winter storms. The rocks only reveal themselves in steep stream banks, along road and trail cut banks, along the precipitous coastal cliffs and offshore in the form of towering rock monuments or sea stacks. (Photograph by CalTrans staff.) Few of California’s State parks display impressive monoliths adorned like a Patrick’s Point State Park displays a snapshot of geologic processes that have castle with towering spires and few permit rock climbing. Castle Crags State shaped the face of western North America, and that continue today. The rocks Park is an exception. The scenic beauty is best enjoyed from a distant exposed in the seacliffs and offshore represent dynamic interplay between the vantage point where one can see the range of surrounding landforms. The The Klamath Mountains consist of several rugged ranges and deep canyons. Klamath/North Coast Bioregion San Joaquin Valley Colorado Desert subducting oceanic tectonic plate (Gorda Plate) and the continental North American monolith and its surroundings are a microcosm of the Klamath Mountains The mountains reach elevations of 6,000 to 8,000 feet. -
Volcanic Legacy
United States Department of Agriculture Forest Service Pacifi c Southwest Region VOLCANIC LEGACY March 2012 SCENIC BYWAY ALL AMERICAN ROAD Interpretive Plan For portions through Lassen National Forest, Lassen Volcanic National Park, Klamath Basin National Wildlife Refuge Complex, Tule Lake, Lava Beds National Monument and World War II Valor in the Pacific National Monument 2 Table of Contents INTRODUCTION ........................................................................................................................................4 Background Information ........................................................................................................................4 Management Opportunities ....................................................................................................................5 Planning Assumptions .............................................................................................................................6 BYWAY GOALS AND OBJECTIVES ......................................................................................................7 Management Goals ..................................................................................................................................7 Management Objectives ..........................................................................................................................7 Visitor Experience Goals ........................................................................................................................7 Visitor -
Lassen Volcanic National Park
LASSEN VOLCANIC NATIONAL PARK • CALIFORNIA • UNITED STATES DEPARTMENT OF THE INTERIOR RATIONAL PARK SERVICE UNITED STATES DEPARTMENT OF THE INTERIOR HAROLD L. ICKES, Secretary NATIONAL PARK SERVICE ARNO B. CAMMERER, Director LASSEN VOLCANIC NATIONAL PARK CALIFORNIA SEASON FROM JUNE 1 TO SEPTEMBER IS UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1934 RULES AND REGULATIONS The park regulations are designed for the protection of the natural beauties as well as for the comfort and convenience of visitors. The com plete regulations may be seen at the office of the superintendent of the park. The following synopsis is for the general guidance of visitors, who are requested to assist in the administration of the park by observing CONTENTS the rules. PAGE Automobiles.—Many sharp unexpected curves exist on the Lassen Peak Loop Highway, and fast driving—over 25 miles per hour in most places—is GEOLOGIC HISTORY 2 dangerous. Drive slowly, keeping always well to the right, and enjoy the THE ANCIENT BROKEOFF CRATER 5 scenery. Specimens and souvenirs.—In order that future visitors may enjoy the SOLFATARAS 6 park unimpaired and unmolested, it is strictly prohibited to break any THE CINDER CONE 8 formation; to take any minerals, lava, pumace, sulphur, or other rock MOUNTAINS 9 specimens; to injure or molest or disturb any animal, bird, tree, flower, or shrub in the park. Driving nails in trees or cutting the bark of trees in OTHER INTERESTING FEATURES I0 camp grounds is likewise prohibited and strictly enforced. Dead wood WILD ANIMALS :: may be gathered for camp fires. Trash.—Scraps of paper, lunch refuse, orange peelings, kodak cartons, FISHING :4 chewing-gum wrappers, and similar trash scattered along the roads and CAMPING r5 trails and camp grounds and parking areas are most objectionable and unsightly. -
51 SEVEN LAKES BASIN Here's The
Castle Lake and Mount Shasta from near Heart Lake (Photo by John R. Soares) mostly level as you continue, bringing you to Peak, Magee Peak, and numerous other Cascade the spine of Mount Bradley Ridge at 3 miles. A volcanoes lead to Mount Shasta, with Mount Eddy 0.2-mile scamper northeast (left) brings you to a to the west of the largest California volcano. knob with the best views. If you want more hiking, continue farther Look south at the immediate prospect of serrated toward Mount Bradley or hike the 0.5 mile path granite crests of Castle Crags. Eastward Lassen that skirts the east side of Castle Lake. SEVEN LAKES BASIN 51 Length: 6 miles round-trip Hiking time: 5 hours or 2 days High point: 6,825 feet Total elevation gain: 1,400 feet Difficulty: moderate Season: early June through late October Water: available only at Seven Lakes Basin (purify first); bring your own Maps: USGS 7.5’ Mumbo Basin, USGS 7.5’ Seven Lakes Basin Information: Mount Shasta Ranger Station, Shasta–Trinity National Forest 122 Seven Lakes Basin • 123 6850' One-way spires of the Trinity Alps to the west, with for- 6800' 6750' ested mountains filling in the northerly and 6700' southerly views. 6650' Travel south, undulating gently along the 6600' 6550' spine of the ridge, occasionally shaded by a Jef- 6500' frey pine, western white pine, red fir, or white fir. 6450' 6400' Note the various flowers, including blue lupines 6350' and yellow sulfur flowers. 6300' 6250' The first decent campsite appears on the left at 6200' 0.3 mile, followed by the inaugural view of Mount 0 mile 1.5 3.0 Shasta, with Mount Eddy and Gumboot Lake com- ThisHike 51. -
Location Option Details
Student Page Location Option Details 1. Florida k Florida has the smallest number of earthquakes in the United States. k Florida is the U.S. location where hurricanes are most frequent. k Of the six deadliest hurricanes to hit the continental U.S., three have hit Florida. k Between 1900 and 1995, Florida experienced both the most major (24) and the most overall (57) hurricanes of any state in the United States. k About half the hurricanes to strike southern Florida are major ones. k No point in Florida is more than 100 miles from the coast; therefore, all areas are at risk of hurricane damage. k From July 1995 through June 1996, Florida experienced 35 tornadoes, 32 floods, and three hurricanes. k In February 1998, devastating tornadoes swept through central Florida, killing at least 43 people and destroying many homes and other buildings. k In 2004, four hurricanes and one tropical storm hit Florida. This was the first time Florida encountered four hurricanes in one season since 1851. The pre-Hurricane Charley aerial photo on the left was taken several days following the passage of 2001’s Tropi- cal Storm Gabrielle. Note the two relatively small breaches in the central part of the island. On August 13, 2004, Hurricane Charley carved the 450-m-wide breach that is shown in the right photo. From U.S. Geological Survey. continues on next page ©Sustainable Forestry Initiative Inc. Decision Making 129 Student Page Location Option Details continued 2. California k California is the state with the most damaging earthquakes. k Giant earthquakes on faults, such as the San Andreas, tend to occur every few hundred years; therefore, an earthquake like the one in 1906 (magnitude 7.8) is not likely to occur in northern California for at least 100 years. -
High-Elevation Five Needle Pine Cone Collections in California and Nevada
High-elevation white pine cone collections from the Great Basin of Nevada, California, & Utah on National Forest, Bureau of Land Management, National Park, and State lands, 2009 – 2013. Collected 40-50 cones/tree. 2009 (all on NFS land): 3 sites # trees Schell Creek Range, Cave Mtn., NV Pinus longaeva 100 Spring Mtns., Lee Canyon, NV Pinus longaeva 100 White Mtns., Boundary Peak, NV Pinus longaeva 100 2010 (all on NFS land except as noted): 7 sites Carson Range, Mt. Rose, NV Pinus albicaulis 23 Hawkins Peak, CA Pinus albicaulis 26 Luther Creek, CA Pinus lambertiana 15 Monitor Pass, CA Pinus lambertiana 25 Pine Forest Range, NV [BLM] Pinus albicaulis 20 Sweetwater Mtns., NV Pinus albicaulis 20 Wassuk Range, Corey Pk., NV [BLM] Pinus albicaulis 25 2011 (all on NFS land except as noted): 13 sites Fish Creek Range, NV [BLM] Pinus flexilis 25 Fish Creek Range, NV [BLM] Pinus longaeva 25 Grant Range, NV Pinus flexilis 25 Highland Range, NV [BLM] Pinus longaeva 25 Independence Mtns., NV Pinus albicaulis 17 Jarbidge Mtns., NV Pinus albicaulis 25 Pequop Mtns., NV [BLM] Pinus longaeva 25 Ruby Mtns., Lamoille Canyon, NV Pinus albicaulis 25 Ruby Mtns., Lamoille Canyon, NV Pinus flexilis 20 Schell Creek Range, Cave Mtn., NV Pinus flexilis 25 Sweetwater Mtns., NV Pinus flexilis 25 White Pine Range, Mt. Hamilton, NV Pinus flexilis 25 White Pine Range, Mt. Hamilton, NV Pinus longaeva 25 2012 (all on NFS land except as noted): 9 sites Black Mountain, Inyo NF, CA Pinus longaeva 23 Carson Range, LTBMU, NV Pinus albicaulis 25 Egan Range, Toiyabe NF, NV Pinus longaeva 25 Emma Lake, Toiyabe NF, CA Pinus albicaulis 25 Happy Valley, Fishlake NF, UT Pinus longaeva 25 Inyo Mtns., Tamarack Canyon, CA Pinus longaeva 25 Leavitt Lake, Toiyabe NF, CA Pinus albicaulis 25 Mt. -
Buy This Book
Excerpted from buy this book © by the Regents of the University of California. Not to be reproduced without publisher’s written permission. INTRODUCTION This book is an attempt to present to general readers not Panamint Range, because for the most part the wildflower trained in taxonomic botany, but interested in nature and seeker does not travel in the desert in summer. their surroundings, some of the wildflowers of the California mountains in such a way that they can be identified without technical knowledge. Naturally, these are mostly summer The California Mountains wildflowers, together with a few of the more striking species that bloom in spring and fall. They are roughly those from the In general, the mountains of California consist of two great yellow pine belt upward through the red fir and subalpine series of ranges: an outer, the Coast Ranges; and an inner, the forests to the peaks above timberline. Obviously, the 286 Sierra Nevada and the southern end of the Cascade Range, in- plants presented cannot begin to cover all that occur in so cluding Lassen Peak and Mount Shasta.The Sierra Nevada,an great an altitudinal range, especially when the geographical immense granitic block 400 miles long and 50 to 80 miles limits of the pine belt are considered. wide, extends from Plumas County to Kern County. It is no- Mention of the pine belt in California mountains will nat- table for its display of cirques, moraines, lakes, and glacial val- urally cause you to think of the Sierra Nevada, but of course leys and has its highest point at Mount Whitney at 14,495 feet this belt also extends into the southern Cascade Range (Mount above sea level. -
The Historical Range of Beaver in the Sierra Nevada: a Review of the Evidence
Spring 2012 65 California Fish and Game 98(2):65-80; 2012 The historical range of beaver in the Sierra Nevada: a review of the evidence RICHARD B. LANMAN*, HEIDI PERRYMAN, BROCK DOLMAN, AND CHARLES D. JAMES Institute for Historical Ecology, 556 Van Buren Street, Los Altos, CA 94022, USA (RBL) Worth a Dam, 3704 Mt. Diablo Road, Lafayette, CA 94549, USA (HP) OAEC WATER Institute, 15290 Coleman Valley Road, Occidental, CA 95465, USA (BD) Bureau of Indian Affairs, Northwest Region, Branch of Environmental and Cultural Resources Management, Portland, OR 97232, USA (CDJ) *Correspondent: [email protected] The North American beaver (Castor canadensis) has not been considered native to the mid- or high-elevations of the western Sierra Nevada or along its eastern slope, although this mountain range is adjacent to the mammal’s historical range in the Pit, Sacramento and San Joaquin rivers and their tributaries. Current California and Nevada beaver management policies appear to rest on assertions that date from the first half of the twentieth century. This review challenges those long-held assumptions. Novel physical evidence of ancient beaver dams in the north central Sierra (James and Lanman 2012) is here supported by a contemporary and expanded re-evaluation of historical records of occurrence by additional reliable observers, as well as new sources of indirect evidence including newspaper accounts, geographical place names, Native American ethnographic information, and assessments of habitat suitability. Understanding that beaver are native to the Sierra Nevada is important to contemporary management of rapidly expanding beaver populations. These populations were established by translocation, and have been shown to have beneficial effects on fish abundance and diversity in the Sierra Nevada, to stabilize stream incision in montane meadows, and to reduce discharge of nitrogen, phosphorus and sediment loads into fragile water bodies such as Lake Tahoe. -
Time-Scale and Mechanism of Subsidence at Lassen Volcanic Center, CA, from Insar
Journal of Volcanology and Geothermal Research 320 (2016) 117–127 Contents lists available at ScienceDirect Journal of Volcanology and Geothermal Research journal homepage: www.elsevier.com/locate/jvolgeores Time-scale and mechanism of subsidence at Lassen Volcanic Center, CA, from InSAR Amy L. Parker a,⁎,1,2,JulietBiggsa,1,ZhongLub a School of Earth Sciences, University of Bristol, Bristol, UK b Roy M. Huffington Department of Earth Sciences, Southern Methodist University, Dallas, TX, United States article info abstract Article history: Observations of volcanic subsidence have contributed to our understanding of the eruption cycle, hydrothermal Received 2 November 2015 systems and the formation of continental crust. Lassen Volcanic Center is one of two volcanoes in the southern Received in revised form 1 April 2016 Cascades known to have subsided in recent decades, but the onset, temporal evolution, and cause of subsidence Accepted 11 April 2016 remain unconstrained. Here we use multiple sets of InSAR data, each corrected using the North American Region- Available online 16 April 2016 al Reanalysis atmospheric model, to determine the temporal and spatial characteristics of deformation between 1992 and 2010. Throughout this period all datasets reveal subsidence of a broad, 30–40 km wide region at rates of ~10 mm/yr. Evaluating past geodetic studies we suggest that subsidence may have been ongoing since the 1980s, before which it is unlikely that significant ground deformation occurred. By combining multiple tracks of InSAR data we find that the ratio of horizontal to vertical displacements is high (up to 3:1), and source inversions favour a point source located at ~8 km depth. -
CURRICULUM VITAE, Francisco L. Pérez (Revised August, 2011)
CURRICULUM VITAE, Francisco L. Pérez (revised August, 2011) Professor, and Director, Soils Laboratory, Department of Geography and the Environment, University of Texas at Austin Austin, Texas 78712, USA. (512) 471-5116, FAX: (512) 471-5049. E-mail: [email protected] Place of Birth: Jumilla (Murcia), Spain. Citizenship and Residence: USA resident (Immigrant Visa), July 1978 - June 2008. American citizen since June 2008. Education: - B. Architecture, Universidad Central de Venezuela, Caracas, July 1973. - M.L.A. in Environmental Design and Planning, University of California (Berkeley), June 1976. - Ph.D. student, University of Oregon (Eugene), Sept 1978-June 1979 (no degree earned). - Ph.D. Wildland Resource Science (focus on Plant Ecology and Geomorphology), University of California (Berkeley), July 1985. Academic and Professional Work Experience: 1. Independent Architect and City Planner, Caracas (Venezuela), August 1973-July 1974. 2. Environmental Planner, Stoddart & Tábora Co., Caracas (Venezuela) July 1976-Dec. 1978. 3. Environmental Impact Division, Venezuelan Ministry of Environment and Renewable Natural Resources (MARNR), Caracas (Venezuela), January 1978-July 1978. 4. Assistant Professor, School of Architecture and City Planning, Department of Environmental Science, Universidad Central de Venezuela (Caracas), Venezuela, August 1976 -July 1978. 5. Graduate Teaching Fellow, Department of Geography, University of Oregon (Eugene), Spring 1979 6. Graduate Teaching Assistant, Department of Forestry and Resource Management, University of California (Berkeley), Winter 1980. 7. Graduate Teaching Assistant, Department of Landscape Architecture, University of California (Berkeley), Spring 1981 and 1983. 8. Except those quarters listed above, I was Research Assistant for Prof. Joe R. McBride, at the Department of Forestry and Resource Management, University of California (Berkeley), between August 1979 and July 1985. -
Geologyofeaglelake.Pdf
OCCASIONAL PAPERS OF THE CALIFORNIA ACADEMY OF SCIENCES No. 34, 29 pages, 4 figures, 1 plate August 31, k/)j THE GEOLOGICAL HISTORY OF EAGLE LAKE LASSEN COUNTY, CALIFORNIA G. C. GESTER Research Associate (Deceased) Department of Geology California Academy of Sciences Introduction, Previous Work and Acknowledgments The principal objective of this paper is to attempt to portray the geo- logical history of Eagle Lake. My first interest in the geology of Eagle Lake stemmed from an exam- ination of the obsidian deposits in California. The Sixth Annual Report of the State Mineralogist(Hanks, 1886, part I, page 125) states that in Lassen Coun- ty "obsidian is found in great abundance on the east side of Eagle Lake, a mile more or less from Clark's Ranch." No obsidian was found, in place, there. Evidently, however, considerable obsidian was carried there by the Indians and used for making arrowheads, a great many of which have been gathered from the shores of the lake. Another statement that attracted my attention was to the effect that Eagle Lake was classed as a "landslide lake," (Davis, 1933, p. 201; Hinds, 1952, p. 86). "The barrier forming it appears to be a landslide on the south- east side." The examination of the shores of the lake clearly suggested that the lake was barred on its southeastern side by the ancient rocks and flows of basaltic lavas rather than by a landslide. A further search of the literature revealed that there are very few pub- lished data regarding the geology of the lake and the surrounding landscape.