2 edition of Surface-water hydrology of coastal basins of northern California. found in the catalog.
Surface-water hydrology of coastal basins of northern California.
S. E. Rantz
|Series||Geological Survey (U.S.). Water-supply paper, 1758, Water-supply paper (Washington, D.C.) ;, 1758.|
|LC Classifications||TC801 .U2 no. 1758|
|The Physical Object|
|Pagination||v, 77 p.|
|Number of Pages||77|
|LC Control Number||gs 64000279|
The Pacific coastal temperate rainforest (PCTR) ecosystem extends kilometers (km) along the west coast of North America from northern California to Kodiak Island, Alaska (Kellogg ). The northern portion of this ecosystem is one of the least anthropogenically modified ecosystems on Earth, home to intact old-growth forests, extensive. Mann MP, Rizzardo J, Satkowski R () Evaluation of methods used for estimating selected streamflow statistics, and flood frequency and magnitude, for small basins in north coastal California: U.S. Geological Survey Scientific Investigations Report –, 92 p.
Product Description. This study describes the complex geology of the northern Sacramento Valley, focusing on the Late Cenozoic geologic formations and structures that compose or influence the valley’s fresh groundwater aquifer formations. Laguna-San Diego Coastal - HUC ; Southern California Coastal - HUC ; California - HUC Online USGS Watershed Information For: Links to Projects, Publications and Information for Cataloging Unit - San Diego Optimum Management in a Basin With Changing Water-supply and Water-quality Problems -.
This study seeks to quantify water availability in the California Coastal Basins (CCBs). The CCBs vary greatly in their geologic, hydrologic, and climatic conditions; predominant water uses (agricultural, urban, or environmental); and how water availability changes in response to natural and anthropogenic stresses. Upper Klamath Lake (UKL) is the source of the Klamath river that flows through southern Oregon and northern California. The UKL basin is home to two endangered species and provides water + ha (,+ acres) of irrigation on the United States Bureau of Reclamation (USBR) Klamath Project located downstream of the UKL basin.
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Additional Physical Format: Online version: Rantz, S.E. (Saul Edward), Surface-water hydrology of coastal basins of northern California. Washington, D.C.: U.S.
Surface-water hydrology of coastal basins of Northern California,U.S. Geological Survey, Water-Supply Paper, W [United States Geological. SURFACE-WATER HYDROLOGY OF COASTAL BASINS OF NORTHERN CALIFORNIA BY S. RANTZ ABSTRACT This report presents an analysis of the surface-water hydrology of those coastal basins of California that are north of the south boundary of the Eel River basin.
Its purpose is to provide hydrologic information in convenient form for use inCited by: Get this from a library. Surface-water hydrology of coastal basins of northern California. [S E Rantz; Geological Survey (U.S.),; California. Department of Water Resources.].
Surface-Water Hydrology of Coastal Basins of Northern California By S. RANTZ GEOLOGICAL SURVEY WATER-SUPPLY PAPER Prepared in cooperation with the Cali fornia Department of Water Resources UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: SURFACE-WATER HYDROLOGY OF CALIFORNIA COASTAL BASINS BETWEEN SAN FRANCISCO BAY AND EEL RIVER By S.
Product Description. Section of the Water Code directs that the California Department of Public Works, acting by and through the State Engineer, shall “investigate conditions of the quality of all the waters within the State, including saline waters, coastal and inland, as related to all sources of pollution of whatever nature and shall report thereon to the Legislature and to the.
most California regions, the water table is between 10 and feet below the land surface (in some Southern California desert basins it is as deep as feet).
It is in California’s numerous valleys and intermontane basins that ground water exists in the greatest quantity (California and Nevada groundwater basins are shown in Figure 1). Bulletin is California’s official publication on the occurrence and nature of groundwater statewide. Bulletin defines the boundaries and describes the hydrologic characteristics of California’s groundwater basins and provides information on groundwater management and recommendations for.
Surface-water hydrology of coastal basins of northern California() The Publications Warehouse does not have links to digital versions of this publication at this time. Northern California coastal plains with abundant shallow groundwater likely will see significant and widespread groundwater emergence, while impacts along the much drier central and southern California coast may be less severe due to the absence of shallow groundwater in many areas.
The USGS Watershed Boundary Dataset (WBD) defines the areal extent of surface water drainage to a point, accounting for all land and surface areas. Watershed Boundaries are determined solely upon science-based hydrologic principles, not favoring any administrative boundaries or special projects, nor particular program or agency.
Hydrology Report: Guthrie, C. G., and Q. Coastal Hydrology for the Guadalupe Estuary: Updated Hydrology with Emphasis on Diversion and Return Flow Data for November Texas Water Development Board, Austin, Texas. 28 pp. Along the coast, most groundwater is developed from shallow wells installed in the sand and gravel beds of several of the region’s rivers.
Under California law, the water produced in these areas is considered surface water underflow. Water from Ranney collectors installed in. Surface water and groundwater are connected in a system of watersheds and groundwater basins. The State Water Plan notes surface water and groundwater are a single resource, “In California, winter precipitation and spring snowmelt are captured in surface water reservoirs to provide both flood protection and water supply to the state.
Water Resource Availability, Maumee River Basin Surface-water Hydrology, Water Resources 61 History of basin wetlands The Maumee River basin in Indiana historically contained a section of the ancient Lake Maumee, a predecessor to modern Lake Erie.
As the lake reced-ed, it left an area of poorly drained soils which early. metamorphic and igneous rocks, these are mostly surface water, while in the semi-arid less watered northern lowlands th ey are mostly groundwater, owing to the permeability of the sedimentary rocks.
Surface Water Hydrology Three major surface water bodies are located within one mile from the 36 lots (Brown and Caldwell, ). The distance and direction of each surface water body is summarized below in Table 4.H Storm Drainage The PDR lots are located on the Westchester Bluffs that drain northward on Falmouth Street to.
HYDROLOGY AND WATER QUALITY Environmental Setting Regional The proposed project would be located in an area subject to the jurisdiction of the NCRWQCB.
The NCRWQCB is separated into two natural drainage basins: the Klamath River Basin and the North Coastal Basin. From Rantz, S.E.
(), Surface-Water Hydrology of Coastal Basins of Northern California: USGS Water-Supply Paper Northern California rainfall frequency maps Maps of rainfall intensity and frequency from the USWB Precipitation Frequency Atlas of the Western U.S., v.
XI: California. SURFACE WATER HYDROLOGY Andrew J. Draper Octo INTRODUCTION CALVIN models California’s inter-connected water supply system. In Northern California, this consists of all inflows to the Central Valley originating from the Trinity-Cascade, Sierra Nevada and Coastal Mountain ranges.The coastal springs in Pasco, Hernando, and Citrus Counties, Florida consist of three first-order magnitude springs and numerous smaller springs, which are points of substantial ground-water discharge from the Upper Floridan aquifer.
Spring flow is proportional to the water-level altitude in the aquifer and is affected primarily by the magnitude and timing of rainfall.