Appendix a Summary of Available Water Supplies
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4.3 Water Resources 4.3 Water Resources
4.3 WATER RESOURCES 4.3 WATER RESOURCES This section describes the existing hydrological setting for the County, including a discussion of water quality, based on published and unpublished reports and data compiled by regional agencies. Agencies contacted include the United States Geological Survey, the California Department of Water Resources, and the Central Valley Regional Water Quality Control Board. This section also identifies impacts that may result from the project. SETTING CLIMATE The local climate is considered warm desert receiving approximately six to eight inches of rainfall per year (U.S. Department of Agriculture, 1986). Rainfall occurs primarily in the winter months, with lesser amounts falling in late summer and fall. Kings County would also be considered a dry climate since evaporation greatly exceeds precipitation.1 A common characteristic of dry climates, other than relatively small amounts of precipitation, is that the amount of precipitation received each year is highly variable. Generally, the lower the mean annual rainfall, the greater the year-to-year variability (Lutgens and Tarbuck, 1979). SURFACE WATER HYDROLOGY The County is part of a hydrologic system referred to as the Tulare Lake Basin (Figure 4.3- 1). The management of water resources within the Tulare Lake Basin is a complex activity and is critical to the region’s agricultural operations. The County can be divided into three main hydrologic subareas: the northern alluvial fan and basin area (in the vicinity of the Kings, Kaweah, and Tule rivers and their distributaries), the Tulare Lake Zone, and the southwestern uplands (including the areas west of the California Aqueduct and Highway 5) (Figure 4.3-2). -
Page 78 TITLE 16—CONSERVATION § 45A–1 Kaweah River and The
§ 45a–1 TITLE 16—CONSERVATION Page 78 Kaweah River and the headwaters of that branch Fork Kaweah River to its junction with Cactus of Little Kern River known as Pecks Canyon; Creek; thence easterly along the first hydro- thence southerly and easterly along the crest of graphic divide south of Cactus Creek to its the hydrographic divide between Pecks Canyon intersection with the present west boundary of and Soda Creek to its intersection with a lateral Sequoia National Park, being the west line of divide at approximately the east line of section township 16 south, range 29 east; thence south- 2, township 19 south, range 31 east; thence erly along said west boundary to the southwest northeasterly along said lateral divide to its corner of said township; thence easterly along intersection with the township line near the the present boundary of Sequoia National Park, southeast corner of township 18 south, range 31 being the north line of township 17 south, range east of the Mount Diablo base and meridian; 29 east, to the northeast corner of said township; thence north approximately thirty-five degrees thence southerly along the present boundary of west to the summit of the butte next north of Sequoia National Park, being the west lines of Soda Creek (United States Geological Survey al- townships 17 and 18 south, range 30 east, to the titude eight thousand eight hundred and eighty- place of beginning; and all of those lands lying eight feet); thence northerly and northwesterly within the boundary line above described are in- along the crest of the hydrographic divide to a cluded in and made a part of the Roosevelt-Se- junction with the crest of the main hydro- quoia National Park; and all of those lands ex- graphic divide between the headwaters of the cluded from the present Sequoia National Park South Fork of the Kaweah River and the head- are included in and made a part of the Sequoia waters of Little Kern River; thence northerly National Forest, subject to all laws and regula- along said divide now between Horse and Cow tions applicable to the national forests. -
KINGS RIVER SPECIAL MANAGEMENT AREA High Sierra Ranger District
PACIFIC SOUTHWEST REGION Restoring, Enhancing and Sustaining Forests in California, Hawaii and the Pacific Islands Sierra National Forest KINGS RIVER SPECIAL MANAGEMENT AREA High Sierra Ranger District Welcome to the Kings River Special Manage- Kings River at the end of Garnet Dike Road. It ment Area. Congress has given special designa- follows the river east for three miles to Spring tion to this area to enhance its recreational oppor- Creek, ascends northeast to Garlic Meadow tunities. It is located two hours east of Fresno in Creek, and continues to Rough Creek. the upper Kings River canyon. The Special Man- agement Area (SMA) includes 49,000 acres Bear Wallow interpretive trail is also located on within the Sierra and Sequoia National Forests. It the north side of the Kings River. Interpretive is the third such area nationwide to be given spe- signs provide information on: Cultural heritage, cial recognition and protection. The other two wildflowers, grasses, California Mule Deer mi- special management areas are Lake Tahoe Basin gration, Blue Oak Woodland and a description of and Mono Lake. Noteworthy characteristics of the scenic overlook. The trail is approximately 2 the SMA include a wild trout fishery, Garlic miles long and gradually climbs the foothill Falls, and the Boole Tree, which is the largest slopes. John Muir Wilderness, Monarch Wilder- Sequoia tree found in any National Forest in the ness, Kings Canyon National Park and the Kings United States. River area all on display at the beautiful scenic overlook. RECREATIONAL OPPORTUNITIES The SMA offers a wide variety of recreational On the south side of the river, another trail be- opportunities: gins at Mill Flat Creek and follows the Kings Camping: There are four developed camp- River upstream 5 miles to Converse Creek. -
Salinity Impared Water Bodies and Numerical Limits
Surface Water Bodies Listed as Impaired by Salinity or Electrical Conductivity on the 303(d) List1 Salinity Del Puerto Creek Hospital Creek Ingram Creek Kellogg Creek Knights Landing Ridge Cut Mountain House Creek Newman Wasteway Old River Pit River, South Fork Ramona Lake Salado Creek Sand Creek Spring Creek Tom Paine Slough Tule Canal Electrical Conductivity Delta Waterways (export area) Delta Waterways (northwestern portion) Delta Waterways (southern portion) Delta Waterways (western portion) Grassland Marshes Lower Kings River Mud Slough North Salt Slough San Joaquin River Temple Creek 1 List adopted by the Central Valley Water Board in June 2009. This list has not been approved by the State Water Board or U.S. EPA. Central Valley Water Bodies With Numerical Objectives for Electrical Conductivity or Total Dissolved Solids SURFACE WATERS GROUNDWATER Sacramento River Basin Tulare Lake Basin Hydrographic Units Sacramento River Westside Feather River Kings River American River Tulare Lake and Kaweah River Folsom Lake Tule River and Poso Goose Lake Kern River San Joaquin River Basin San Joaquin River Tulare Lake Basin Kings River Kaweah River Tule River Kern River Sacramento-San Joaquin Delta Sacramento River San Joaquin River So. Fork Mokelumne River Old River West Canal All surface waters and groundwaters Delta-Mendota Canal designated as municipal and domestic Montezuma Slough (MUN) water supplies must meet the Chadbourne Slough numerical secondary maximum Cordelia Slough contaminant levels for salinity in Title Goodyear Slough 22 of the California Code of Intakes on Van Sickle and Chipps Regulations. Islands . -
Appendix A: Description of Contractors and Exchange Partners
Final EA-15-022 Appendix A Description of Contractors and Exchange Partners Summary of Cross Valley Contractors The following description characterizes each Cross Valley Contractor and associated subcontractor: County of Fresno The County of Fresno has a water service contract (Contract No. 14-06-200-8292A-IR15) for up to 3,000 acre-feet per year (AFY) that is provided for municipal and industrial (M&I) uses to specific developments within its CVP service area. The County draws its water directly from Millerton Lake after its Delta supply has been exchanged for Friant supplies with Arvin-Edison Water Storage District (Arvin-Edison). The County’s CVP water supplies have been administered by Arvin-Edison for the last 20 years pursuant to an agreement between the County and Arvin-Edison. County of Tulare The County of Tulare has a water service contract (Contract No. 14-06-200-8293A-IR15) for up to 5,308 AFY of water. The County of Tulare is comprised of 10 subcontractors (both agricultural and M&I) and all are located in the same geographical area as the Friant Division Contractors. Of the 10 subcontractors, only five have routinely taken water deliveries via the County of Tulare’s contract in recent years. The County of Tulare’s CVP contract supply is divided among the 10 subcontractors as shown below: Alpaugh Irrigation District (Alpaugh) – up to 100 AFY (agricultural) Atwell Island Water District (Atwell Island) – up to 50 AFY (agricultural) City of Lindsay – up to 50 AFY (M&I) City of Visalia – up to 300 AFY (M&I) Fransinetto Farms LLC – up to 400 AFY (agricultural) Hills Valley Irrigation District (Hills Valley) – up to 2,913 AFY (agricultural) Saucelito Irrigation District (Saucelito) – up to 100 AFY (agricultural) Stone Corral Irrigation District (Stone Corral) – up to 950 AFY (agricultural) Strathmore Public Utility District (Strathmore) – up to 400 AFY (M&I) Styro-Tek, Inc. -
Westlands Water District – Warren Act Contract for Conveyance of Kings River Flood Flows in the San Luis Canal
Final Environmental Assessment Westlands Water District – Warren Act Contract for Conveyance of Kings River Flood Flows in the San Luis Canal EA-11-002 U.S. Department of the Interior Bureau of Reclamation Mid-Pacific Region South-Central California Area Office Fresno, California January 2012 Mission Statements The mission of the Department of the Interior is to protect and provide access to our Nation’s natural and cultural heritage and honor our trust responsibilities to Indian Tribes and our commitments to island communities. The mission of the Bureau of Reclamation is to manage, develop, and protect water and related resources in an environmentally and economically sound manner in the interest of the American public. Table of Contents Page Section 1 Purpose and Need for Action ....................................................... 1 1.1 Background ........................................................................................... 1 1.2 Purpose and Need ................................................................................. 1 1.3 Scope ..................................................................................................... 1 1.4 Reclamation’s Legal and Statutory Authorities and Jurisdiction Relevant to the Proposed Federal Action.............................................. 2 1.5 Potential Issues...................................................................................... 3 Section 2 Alternatives Including the Proposed Action............................... 5 2.1 No Action Alternative .......................................................................... -
San Joaquin Valley Groundwater Basin Kings Subbasin
Tulare Lake Hydrologic Region California’s Groundwater San Joaquin Valley Groundwater Basin Bulletin 118 San Joaquin Valley Groundwater Basin Kings Subbasin • Groundwater Subbasin Number: 5-22.08 • County: Fresno, Kings, and Tulare • Surface Area: 976,000 acres (1,530 square miles) Subbasin Boundaries and Hydrology The San Joaquin Valley is surrounded on the west by the Coast Ranges, on the south by the San Emigdio and Tehachapi Mountains, on the east by the Sierra Nevada and on the north by the Sacramento-San Joaquin Delta and Sacramento Valley. The northern portion of the San Joaquin Valley drains toward the Delta by the San Joaquin River and its tributaries, the Fresno, Merced, Tuolumne, and Stanislaus Rivers. The southern portion of the valley is internally drained by the Kings, Kaweah, Tule, and Kern Rivers that flow into the Tulare drainage basin including the beds of the former Tulare, Buena Vista, and Kern Lakes. The Kings Subbasin is bounded on the north by the San Joaquin River. The northwest corner of the subbasin is formed by the intersection of the east line of the Farmers Water District with the San Joaquin River. The west boundary of the Kings Subbasin is the eastern boundaries of the Delta- Mendota and Westside Subbasins. The southern boundary runs easterly along the northern boundary of the Empire West Side Irrigation District, the southern fork of the Kings River, the southern boundary of Laguna Irrigation District, the northern boundary of the Kings County Water District, the southern boundaries of Consolidated and Alta Irrigation Districts, and the western boundary of Stone Corral Irrigation District. -
Floods of December 1966 in the Kern-Kaweah Area, Kern and Tulare Counties, California
Floods of December 1966 in the Kern-Kaweah Area, Kern and Tulare Counties, California GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1870-C Floods of December 1966 in the Kern-Kaweah Area, Kern and Tulare Counties, California By WILLARD W. DEAN fPith a section on GEOMORPHIC EFFECTS IN THE KERN RIVER BASIN By KEVIN M. SCOTT FLOODS OF 1966 IN THE UNITED STATES GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1870-C UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1971 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY W. A. Radlinski, Acting Director Library of Congress catalog-card No. 73-610922 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 45 cents (paper cover) CONTENTS Page Abstract_____________________________________________________ Cl Introduction.____________ _ ________________________________________ 1 Acknowledgments. ________________________________________________ 3 Precipitation__ ____________________________________________________ 5 General description of the floods___________________________________ 9 Kern River basin______________________________________________ 12 Tule River basin______________________________________________ 16 Kaweah River basin____________________________--_-____-_---_- 18 Miscellaneous basins___________________________________________ 22 Storage regulation _________________________________________________ 22 Flood damage.__________________________________________________ 23 Comparison to previous floods___________-_____________--___------_ -
Proposed John Muir-Kings Canyon National Park
JOHN MUIR-KINGS CANYON NATIONAL PARK PLATE IX. Part of South Wall of Tehipitee Valley PLATE VIII. Tehipitee Dome, Upper End of Tehipitee Valley (Middle Fork of the Kings River) PROPOSED John Muir-Kings Canyon National Park Including a Summary oj A RIVAL OE THE YOSEMITE THE CANYON OF THE SOUTH FORK OF THE KING'S RIVER, CALIFORNIA By JOHN MUIR WITH PLATES OF ORIGINAL DRAWINGS BY CHARLES D. ROBINSON WHICH APPEARED IN THE CENTURY MAGAZINE November, 1891 Reproduced by permission of D. Applcton-Century Co. Reprinted from Planning and Civic Comment January -\farcb, 19 39 AMERICAN PLANNING AND CIVIC ASSOCIATION 901 UNION TRUST BUILDING WASHINGTON, D. C. John Muir-Kings Canyon National Park Commands Wide Support The proposed John Muir-Kings Canyon National Park would preserve for all time in the National Park System the superlative canyons ol the Kings River, described by John Muir in the accompanying Century article, lirst published in 1891, together with the Evolution Basin and the high peaks of the finest part of the Sierra Nevada, including Mt. Clarence King, Mt. Hatchings, the Sphinx, Tehipite Dome, Paradise Peak, Glacier Monu ment, Avalanche Peak, Grand Sentinel and scores of others. The park would encompass Muir, Cartridge, Mather and Granite Passes, and, along the boundary would touch Alts. Darwin, Haeckel, Pinchot, and the Pali sades as well as Bishop, Taboose, Sawmill, Kearsarge and Forester Passes. General Grant National Park would become General Grant Grove in the new park and the Big Trees of Redwood Canyon, now unprotected, would form another grove in the park. The project has commanded wide support in the State of California and has been approved by the following organizations: Sierra Club. -
Jockusch Et Al in 2012
Zootaxa 3190: 1–30 (2012) ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ Article ZOOTAXA Copyright © 2012 · Magnolia Press ISSN 1175-5334 (online edition) Morphological and molecular diversification of slender salamanders (Caudata: Plethodontidae: Batrachoseps) in the southern Sierra Nevada of California with descriptions of two new species ELIZABETH L. JOCKUSCH1, IÑIGO MARTÍNEZ-SOLANO1,2, ROBERT W. HANSEN3, & DAVID B. WAKE4 1Department of Ecology and Evolutionary Biology, 75 N. Eagleville Rd., U-3043, University of Connecticut, Storrs, CT 06269, USA. E-mail: [email protected] 2Instituto de Investigación en Recursos Cinegéticos (IREC) (CSIC-UCLM-JCCM), Ronda de Toledo, s/n 13005 Ciudad Real, Spain. E-mail: [email protected] 316333 Deer Path Lane, Clovis, CA 93619-9735, USA. E-mail: [email protected] 4Museum of Vertebrate Zoology, 3101 Valley Life Sciences Building, University of California, Berkeley, CA 94720-3160, USA. E-mail: [email protected] Abstract Slender salamanders of the genus Batrachoseps achieve relatively high diversity in the Kern Canyon region at the southern end of the Sierra Nevada of California through high turnover of species with small geographic ranges. The status of several populations of Batrachoseps in this region is enigmatic, and both morphological and molecular data have suggested that some populations do not belong to any of the currently recognized species. Identification of species in this region is com- plicated by the apparent extinction of Batrachoseps relictus in the vicinity of its type locality in the Lower Kern River Canyon. Here we analyze a comprehensive morphological dataset to evaluate diversity in the Kern River Canyon region. -
Terminus Reservoir: Geology, Paleontology, Flora & Fauna
Terminus Reservoir: Geology, Paleontology, Flora & Fauna, Archeology, History Terminus Reservoir Geology, Paleontology, Flora & Fauna, Archeology, History TERMINUS RESERVOIR Geology, Paleontology, Flora & Fauna, Archeology, History By Lorin E. Berryman, Reports Control Officer U.S. Army Corps of Engineers, Sacramento District Dr. Albert B. Elasser, Research Anthropologist Robert H. Lowie, Museum University of California, Berkeley August 1966 Prepared under the Inter-Agency Archeological Salvage Program by the U.S. Army Corps of Engineers in cooperation with the National Park Service TABLE OF CONTENTS index.htm Last Updated: 08-Sep-2008 http://www.nps.gov/history/history/online_books/smithsonian/terminus-reservoir/index.htm[7/11/2012 2:55:36 PM] Terminus Reservoir: Geology, Paleontology, Flora & Fauna, Archeology, History (Table of Contents) Terminus Reservoir Geology, Paleontology, Flora & Fauna, Archeology, History TABLE OF CONTENTS Cover Terminus Dam and Reservoir — Kaweah River, California Geology and Paleontology Geologic History Physiography Stratigraphy Regional Structure Paleontology Flora and Fauna Native Occupation of the Terminus Reservoir Region Archeological Investigations Historical Sketch Linguistic and Cultural Boundaries Pattern of Occupation — Primary Foods The Pictographs Summary of Excavations Greasy Creek Site Slick Rock Village Site Cobble Lodge Site Conclusions Spanish Exploration of the Kaweah River Basin American Exploration and Settlement The Inter-Agency Archeological Salvage Program Notes List of Common and Scientific -
Kings River Canyon
Kings River Canyon Clarence Quigley Fresno Bee, March 2, 1961 The Ghost of the Kings Clarence Quigley and the Kings River On the Kings River, in the Sierra National Forest, there’s a place called Hermit Hole. Hermit Hole is a flat spot on the river bank, shaded by large oak trees, used as a rafting launch and picnic site. Its unusual name derives from an unusual man: Clarence Quigley. Quigley was a lumberman, miner, trapper, and hermit who lived most of his life in the steep canyons of the Kings River. Clarence Quigley received the appellation “Ghost of the Kings” probably in the 1950s by a newspaper writer. He was described as a hermit of a man with an ability to vanish before one’s eyes by ducking into one of his many passages in the brush. He was often glimpsed by hikers or fishermen who frequented the Kings River canyon, but few knew much about him. Once encountered, he was friendly and affable, neighborly offering fishing advice or inquiring about the visitor. A 1961 article about him in the Fresno Bee newspaper entitled ‘Ghost of the Kings’ Proves Friendly Flume Riding, Bear Clubbing Man1 told his story, and the nickname stuck, even in his obituary in 1975.2 ***** Clarence Quigley was born in 1892 as the middle child of five to parents who had moved to California from the Midwest. In 1900, eight-year-old Clarence was living with his father and mother William and Victoria Quigley in Sutter Township in Sutter County in northern California. He had a sister, Ione, and four brothers, George, Warren, Orvil, and Raymond.3 What brought the family members to Fresno County is unknown.