Near-surface hydrothermal regime of the Lassen known geothermal resources area, California

Publisher: U.S. Dept. of the Interior, Geological Survey in Menlo Park, Calif

Written in English
Published: Downloads: 434
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  • Earth temperature -- California.

Edition Notes

Statementby C.W. Mase, J.H. Sass, and Arthur H. Lachenbruch.
SeriesOpen-file report / U.S. Geological Survey -- 80-1230., Open-file report (Geological Survey (U.S.)) -- 80-1230.
ContributionsSass, J. H. 1937-, Lachenbruch, Arthur H., Geological Survey (U.S.)
The Physical Object
Pagination1 v.
ID Numbers
Open LibraryOL18021633M

Hydrothermal Areas: We hike the trails of Lassen National Park and Caribou Wilderness. Our maps are free to you, the hiker. member: Sacramento Valley Hiking Conference: Boiling Springs Lake--see Boiling Springs Lake & Terminal Geyser Bumpass Hell--see. The surface manifestations of a geothermal system in a volcanic area are generally the features that first stimulate exploration. Consequently, the recognition, mapping, and evaluation of these features are important in the second stage or prefeasibilitystudy, during which the geothermal potential is prefeasibility stage also involves sampling fluids and gases to be studied by.   Australia-based firm Controlled Thermal Resources is partnering with Alger Alternative Energy on a plan to construct a utility scale geothermal energy project located within the Salton Sea Known Geothermal Resource Area in California’s Imperial Valley. The plan also includes development of a mining operation. Hydrothermal circulation in its most general sense is the circulation of hot water (Ancient Greek ὕδωρ, water, and θέρμη, heat).Hydrothermal circulation occurs most often in the vicinity of sources of heat within the Earth's general, this occurs near volcanic activity, but can occur in the deep crust related to the intrusion of granite, or as the result of orogeny or.

Stanford Libraries' official online search tool for books, media, journals, databases, government documents and more. The Raft River geothermal system is located 90 miles southwest of Pocatello, near the Utah-Idaho state boarder in the Raft River Valley (Figure 1). The valley lies at approximately ft MSL. The geothermal resource was discovered when two agricultural wells, the Bridge and Crank wells encountered boiling water sometime prior to In most geothermal systems associated with volcanic fields, ~95% of the thermal resource is hot dry rock; exceptions are geothermal systems in carbonate rocks where the permeability is high. The world's very substantive hot dry rock resource can be developed if attempts to create man-made hydrothermal circulation systems are successful. PSGeochemical Modeling of the Near-Surface Hydrothermal System Beneath the Southern Moat of Long Valley Caldera, California* Regina Tempel1 and Daniel Sturmer2 Search and Discovery Article # () Posted Aug *Adapted from poster presentation at AAPG Annual Convention and Exhibition, Houston, Texas, USA, April ,

Paulson, K.M., and Ingebritsen, S.E., , Sodium and chloride data from selected streams in the Lassen area, north-central California, and their relation to thermal-fluid discharge from the Lassen hydrothermal system: U.S. Geological Survey Water-Resources Investigations Report , 29 p. Table 2 USGS Estimates of Potential Energy Recoverable from U.S. Geothermal Resources with Current or Near-Current Technologies Development Category Geothermal reserves (developable at competitive costs) Type of Geothermal Resource Hydrothermal Convection 3, MW-c* Hot Igneous recovery technology undeveloped Conduction- Dominated Marginal. 42 Temperature gradient map showing Known Geothermal Resource Area (KGRA) locations in Imperial Valley, California 56 Modified Stiff diagrams for characteristic ^ Imperial Valley ground waters 57 Schematic surface of specific conductance values for Imperial Valley ground water. Unfortunately, this book can't be printed from the OpenBook. If you need to print pages from this book, we recommend downloading it as a PDF. Visit to get more information about this book, to buy it in print, or to download it as a free PDF.

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Near-surface hydrothermal regime of the Lassen known geothermal resources area, California (U.S. Geological Survey open-file report) [C.

W Mase] on. Near-surface hydrothermal regime of the Lassen Known Geothermal Resource Area, California Open-File Report By: C.W. Mase, J.H. Sass, and Arthur H. Lachenbruch. Geological Survey NEAR-SURFACE HYDROTHERMAL REGIME OF THE LASSEN "KNOWN GEOTHERMAL RESOURCES AREA", CALIFORNIA by C.

Mase, J. Sass, and Arthur H. Lachenbruch U.S. Geological Survey, Menlo Park, California U.S. Geological Survey Open-File Report Cited by: 3. The data relate to a geothermal anomaly known as the Mesa anomaly.

It is concluded that the thermal feature forming the Mesa anomaly is a manifestation of a sizable convective hydrothermal system embracing an area of about 19 square miles and a considerable volume of saturated sediment in the Salton trough.

The Calabozos hydrothermal system would be an attractive geothermal prospect were its location not so remote. Introduction Hot springs and steam vents occur along faults associated with collapse and resurgence of the Calabozos caldera, a late Pleistocene structure on the crest of the central Chilean by: The remarkable hydrothermal features in Lassen Volcanic National Park include roaring fumaroles (steam and volcanic-gas vents), thumping mud pots, boiling pools, and steaming ground.

Water from rain and snow that falls on the highlands of the park feed the hydrothermal system. United States Department of California book Interior Geological Survey SHALLOW HYDROTHERMAL REGIME OF THE EAST BRAWLEY AND GLAMIS KNOWN GEOTHERMAL RESOURCE AREAS, SALTON TROUGH, CALIFORNIA by C.W.

Mase, J.H. Sass, by: 4. Helium surveys over known geothermal resource areas in the Imperial Valley, California Open-File Report By: Alan A. Roberts. of hydrothermal metamorphic origin from the Salton Sea geothermal system was first described by White, Anderson, and Grubbs ().

Gnor,ocrc SBrrrwc The Salton Sea geothermal system is entirely within pliocene and Quaternary sediments of the colorado River delta at the north end of the Gulf of Size: KB.

A geothermal resource requires fluid, heat, and permeability to generate electricity. Conventional hydrothermal resources contain all three components naturally. These geothermal systems can occur in widely diverse geologic settings, sometimes without clear surface manifestations of the underlying resource.

The lack. a geothermal heat pump is drilled into the ground which will extract heat from beneath the earth's surface.

this is done at a power plant or "hot spots" that coverts water to steam by lowering the pressure. to steam is used to turn turbines to make electricity. how geothermal energy is captured: hydrothermal convection.

Buy Near-surface hydrothermal regime of the Lassen " known geothermal resources area ", California (U.S. Geological Survey open-file report) by C. W Mase (ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible : C. W Mase. SPECIAL COLLECTION: GEOLOGY AND GEOBIOLOGY OF LASSEN VOLCANIC NATIONAL PARK The Lassen hydrothermal systemk Steven e.

IngebrItSen1,*, Deborah bergfelD1, laura 1e. Clor, anD WIllIam C. evanS1 1U.S. Geological Survey, Menlo Park, CaliforniaU.S.A.

abStraCt The active Lassen hydrothermal system includes a central vapor-dominated zone or zones beneath. The hydrothermal system in the vicinity of Lassen Volcanic National Park contains a central region of fluid upflow in which steam and liquid phases separate, with steam rising through a parasitic.

Buy Near Surface Hydrothermal Regime of the Lasser 'known Geothermal Resources Area' California by Geological Survey U.S. (ISBN:) from Amazon's Book Store.

Everyday low prices and free delivery on eligible : Geological Survey U.S. The active Lassen hydrothermal system includes a central vapor-dominated zone or zones beneath the Lassen highlands underlain by ~ °C high-chloride waters that discharge at lower elevations.

It is the best-exposed and largest hydrothermal system in the Cascade Range, discharging 41 ± 10 kg/s of steam (~ MW) and 23 ± 2 kg/s of high Cited by: 4. COVID Resources. Reliable information about the coronavirus (COVID) is available from the World Health Organization (current situation, international travel).Numerous and frequently-updated resource results are available from this ’s WebJunction has pulled together information and resources to assist library staff as they consider how to handle coronavirus.

The barbed straight line is a railroad and the rectangle is the location of the power plant Cerro Prieto I, 2~ Hydrothermal Flow Regime and Magmatic Heat Source 33 ,~ I w o SW ~_~ o ~ ~ ~"C -~--~C NE by: Fundamental Characteristics of Hydrothermal Submarine Systems energy in Mexico embraces both near-surface reservoirs and deep geothermal resources at more than meters depth.

Both types of resources exist in the Gulf of California and in the Pacific Ocean (Fig.1). This condensed,Author: Nadia E.

Suárez-Bosche, Mario-César Suárez-Arriaga, V Fernando Samaniego, Víctor Delgado. The currently active hydrothermal system is > km 2 in area, while the associated inactive area is ∼ 10 km 2 (Rose et al., ).

The active hydrothermal features in LVNP contain a vapor. Sponsored by: DOE, CEC, and GRC Organized by: NREL. Building on the successful announcements by the President at the Lake Tahoe Summit to catalyze collaboration and action between the State of California and the Federal Government for conservation and renewable energy development in the Salton Sea, the U.S.

Because geothermal understanding is incomplete and rapidly evolving, the USGS complements its assessments with a broad program of geothermal research that includes (1) study of geothermal processes on crustal and local scales, (2) regional evaluations, (3) intensive study of type systems before and during exploitation, (4) improvement of Cited by: 9.

THIRD EAST AFRICAN RIFT GEOTHERMAL CONFERENCE Djibouti, 22 – 25 November 27 27 GEOTHERMAL RESOURCE INDICATIONS OF THE GEOLOGIC DEVELOPMENT AND HYDROTHERMAL ACTIVITIES OF D.R.C. Getahun Demissie Addis Abeba, Ethiopia, [email protected] ABSTRACT Published sources report the occurrence of more than thermal.

Goals of past geothermal monitoring efforts include: (1) determining if the production of water from wells was measurably affecting the flow of a hot spring (Spencer, ; Jarvis, ); (2) determining if the development of adjacent Known Geothermal Resource Areas might affect an entire hydrothermal area (Sorey, ); and (3) evaluating.

THE GEOTHERMAL MAP OF CALIFORNIA Susan F. Hodgson California Department of Conservation Division of Oil, Gas and Geothermal Resources Sacramento, CA The new “Geothermal Map of California,” drawn at a scale of , is the most comprehensive geothermal map every made of the state. Digitally produced with a PC.

Amedee geothermal plant near Honey Lake has contributed an average MW of electricity to the California grid since October Another MW is produced at the nearby Wineagle geo-thermal power plant.

The Geysers The Geysers Geothermal Field has been the world’s largest producer of geothermal electrical power since the s. It reachedFile Size: KB. Conventional hydrothermal resources naturally contain the permeability, fluid, and heat (over °C) needed to generate electricity.

This constitutes the majority of current global geothermal resource developments. Low-temperature resources are hydrothermal resources with temperatures below ° Size: KB. Geothermal Energy Geothermal energy comes from the heat within the earth. People around the world use geothermal energy to produce electricity, to heat buildings and for other purposes.

Geothermal Energy Geothermal pumps collect hot water and from inside the earth and return the. Technical Report: Quantitative analysis of the hydrothermal system in Lassen Volcanic National Park and Lassen Known Geothermal Resource Area.

Quantitative analysis of the hydrothermal system in Lassen Volcanic National Park and Lassen Known Geothermal Resource Area. California Geothermal Forum: A Path to Increasing Geothermal Development in California Hydrothermal Program Manager.

Geothermal Technologies Office Denver West Blvd. Golden, CO California Energy Commission and the Geothermal Resources Council. The occurrence of hydrothermally altered zones is a commonly observed phenomenon in brittle rock.

The dissolution and transformation of primary minerals and the precipitation of secondary minerals affect rocks in terms of mechanics, stress conditions, and induced seismicity.

The present study investigates commonly observed phenomena of hydrothermal alteration and observations at the geothermal Cited by: Get this from a library!

Quantitative analysis of the hydrothermal system in Lassen Volcanic National Park and Lassen Known Geothermal Resource Area. [M L Sorey; S E Ingebritsen] -- The Lassen hydrothermal system is in the southern Cascade Range, approximately 70 kilometers east-southeast of Redding, California.

The conceptual model of the Lassen system is termed a.Truesdell, A. H., and Fournier, R. O. (a): Calculation of deep temperatures in geothermal systems from the chemistry of boiling spring water of mixed origin, U.N.

Symposium on Development and Use of Geothermal Resources, Proceedings, v. 2, –Cited by: