Design of a Ground-Water-Quality Monitoring Network for the Salinas River Basin, California
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The Paso Robles AVA and Its Eleven Viticultural Areas
The Paso Robles AVA and its Eleven Viticultural Areas Located along California's famed Central Coast, the Paso Robles winegrape growing Paso Robles Highlands region's climate is perfect for the production of award‐winning premium wines. A Climate: District Region IV long growing season of warm days and cool evenings give rise to vibrantly ripened Annual Average Rainfall: 12 in (30 cm) fruit with dynamic flavor profiles. The region’s diversity led to the establishment of Diurnal Growing Season Temperature Change: 50°F 11 new viticultural areas within the greater Paso Robles AVA, made official in 2014. Topography: Old Pliocene–Pleistocene erosional surface across the Simmler, This historic announcement concluded a seven‐year process by a dedicated group Monterey and Paso Robles Formations below the La Panza Range; of Paso Robles vintners and winegrape growers who created a unified approach, 1,160‐2,086 ft. (353‐635 m) using science as its standard, to develop a comprehensive master plan for the Soil: Deep, sometimes cemented alluvial soils; old leached alkaline soils common, greater Paso Robles American Viticultural Area. with younger sandy soils along active steams. Paso Robles Paso Robles Willow Creek District Climate: Maritime, becoming more continental to the east, with growing Climate: Region II degree‐day Regions II, III and IV. Annual Average Rainfall: 24‐30 in (61‐76 cm) Annual Average Rainfall: 8‐30 in (20‐76 cm) Diurnal Growing Season Temperature Change: 20°F Diurnal Growing Season Temperature Change: 20‐50°F Topography: High elevation mountainous bedrock slopes across a more erodible Topography: Salinas River and tributary valleys, alluvial terraces, and member of the Monterey Formation; 960‐1,900 ft. -
Late Cenozoic Tectonics of the Central and Southern Coast Ranges of California
OVERVIEW Late Cenozoic tectonics of the central and southern Coast Ranges of California Benjamin M. Page* Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305-2115 George A. Thompson† Department of Geophysics, Stanford University, Stanford, California 94305-2215 Robert G. Coleman Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305-2115 ABSTRACT within the Coast Ranges is ascribed in large Taliaferro (e.g., 1943). A prodigious amount of part to the well-established change in plate mo- geologic mapping by T. W. Dibblee, Jr., pre- The central and southern Coast Ranges tions at about 3.5 Ma. sented the areal geology in a form that made gen- of California coincide with the broad Pa- eral interpretations possible. E. H. Bailey, W. P. cific–North American plate boundary. The INTRODUCTION Irwin, D. L. Jones, M. C. Blake, and R. J. ranges formed during the transform regime, McLaughlin of the U.S. Geological Survey and but show little direct mechanical relation to The California Coast Ranges province encom- W. R. Dickinson are among many who have con- strike-slip faulting. After late Miocene defor- passes a system of elongate mountains and inter- tributed enormously to the present understanding mation, two recent generations of range build- vening valleys collectively extending southeast- of the Coast Ranges. Representative references ing occurred: (1) folding and thrusting, begin- ward from the latitude of Cape Mendocino (or by these and many other individuals were cited in ning ca. 3.5 Ma and increasing at 0.4 Ma, and beyond) to the Transverse Ranges. This paper Page (1981). -
Technical Report
2350 Mission College Blvd., Suite 525 Santa Clara, CA 95054 650-852-2800 Storm Water Resource Plan For the Greater Salinas Area Final February 10, 2017 Prepared for Monterey Regional Water Pollution Control Agency 5 Harris Court, Building D Monterey, CA 93940 K/J Project No. 1668019*00 Table of Contents List of Tables ................................................................................................................................ iii List of Figures............................................................................................................................... iii List of Appendices ........................................................................................................................ iv List of Acronyms ........................................................................................................................... iv Section 1: Introduction and SWRP Objectives .............................................. 6 1.1 Plan Development .................................................................................. 6 1.1 SWRP Plan Objectives........................................................................... 8 1.1.1 GMC IRWM Plan Objectives ..................................................... 11 1.1.1.1 Basin Plan Goals Relevant to Storm Water ............ 11 1.1.2 Greater Salinas Area SWRP Objectives ................................... 11 1.1.2.1 Water Quality Objective .......................................... 12 1.1.2.2 Water Supply Objective ......................................... -
Geologic Map of the Northwestern Caliente Range, San Luis Obispo County, California
USGS L BRARY RESTON 1111 111 1 11 11 II I I II 1 1 111 II 11 3 1818 0001k616 3 DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Geologic map of the northwestern Caliente Range, San Luis Obispo County, California by J. Alan Bartowl Open-File Report 88-691 This map is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. Any use of trade names is for descriptive purposes only and does not imply endorsement by USGS 'Menlo Park, CA 1988 it nedelitil Sow( diSti) DISCUSSION INTRODUCTION The map area lies in the southern Coast Ranges of California, north of the Transverse Ranges and west of the southern San Joaquin Valley. This region is part of the Salinia-Tujunga composite terrane that is bounded on the northeast by the San Andreas fault (fig. 1) and on the southwest by the Nacimiento fault zone (Vedder and others, 1983). The Chimineas fault of this map is inferred to be the boundary between the Salinia and the Tujunga terranes (Ross, 1972; Vedder and others, 1983). Geologic mapping in the region of the California Coast Ranges that includes the area of this map has been largely the work of T.W. Dibblee, Jr. Compilations of geologic mapping at a scale of 1:125,000 (Dibblee, 1962, 1973a) provide the regional setting for this map, the northeast border of which lies about 6 to 7 km southwest of the San Andreas fault. Ross (1972) mapped the crystalline basement rocks in the vicinity of Barrett Creek, along the northeast side of the Chimineas fault ("Barrett Ridge" of Ross, 1972). -
Creek Stewardship Guide for San Luis Obispo County Was Adapted from the Sotoyome Resource Conservation District’S Stewardship Guide for the Russian River
Creek Stewardship Guide San Luis Obispo County 65 South Main Street Suite 107 Templeton, CA 93465 805.434.0396 ext. 5 www.US-LTRCD.org Acknowledgements The Creek Stewardship Guide for San Luis Obispo County was adapted from the Sotoyome Resource Conservation District’s Stewardship Guide for the Russian River. Text & Technical Review Sotoyome Resource Conservation District, Principal Contributor Melissa Sparks, Principal Contributor National Resource Conservation District, Contributor City of Paso Robles, Contributor Terra Verde Environmental Consulting, Reviewer/Editor Coastal San Luis Resource Conservation District, Reviewer/Editor Monterey County Resource Conservation District, Reviewer/Editor San Luis Obispo County Public Works Department, Reviewer/Editor Atascadero Mutual Water Company, Reviewer Photographs Carolyn Berg Terra Verde Environmental Consulting US-LT RCD Design, Editing & Layout Scott Ender Supporting partner: December 2012 Table of Contents 1 INTRODUCTION 2 RESOURCE CONSERVATION DISTRICTS IN SAN LUIS OBISPO COUNTY 3 WATERSHEDS OF SAN LUIS OBISPO COUNTY 3 Climate 4 Unique & Diverse Watersheds & Sub-Watersheds of San Luis Obispo County 7 Agriculture in San Luis Obispo County Watersheds 8 WHAT YOU CAN DO TO HELP SAN LUIS OBISPO’S CREEKS 9 Prevent & Control Soil Erosion 11 Properly Maintain Unsurfaced Roads and Driveways 13 Restore Native Riparian Vegetation 14 Remove Exotic Species 14 Enhance Instream Habitat 15 Avoid Creating Fish Passage Barriers 15 Conserve Water 16 Control Stormwater Runoff 16 Maintain Septic Systems -
Conservation and Open Space Element Appendices
County of San Luis Obispo General Plan Conservation and Open Space Element Appendices May 2010 San Luis Obispo County Department of Planning and Building ® County of San Luis Obispo General Plan Conservation and Open Space Element Appendices Adopted by the San Luis Obispo County Board of Supervisors May 11, 2010 - Resolution 2010-151 San Luis Obispo County Department of Planning and Building ® ® TOC TABLE OF CONTENTS Appendix 1. Air Quality Resources Introduction ......................................................................... A1.1 Local Setting ....................................................................... A1.1 Regulatory Framework ....................................................... A1.9 Climate Change ................................................................ A1.20 References ....................................................................... A1.30 Appendix 2. Community-Wide and County Government Operations 2006 Baseline Greenhouse Gas Emissions Inventory Executive Summary ............................................................ A2.1 Community-Wide GHG Inventory Results ........................... A2.2 County government operations GHG Inventory Results ..... A2.2 Data limitations ................................................................... A2.3 Forecast and Next Steps .................................................... A2.4 1. Introduction ................................................................... A2.6 2. Community and County Government Operations Inventory Methodology .............................................................. -
Lower San Juan Creek Watershed
Lower San Juan Creek Watershed Hydrologic Water Acreage Flows to Groundwater Jurisdictions Unit Name Planning Basin(s) Area Estrella Rafael/ Big 114,329 Salinas River via Paso Robles County of San Luis 17 Spring acres Estrella River – to Obispo WPA 11, Pacific Ocean Shandon (ptn) Salinas/ (Monterey Bay Los Padres National Estrella National Marine Forest Sanctuary) WPA 14 Description: The Lower San Juan Creek watershed is located in the eastern portion of the county to the north- west of the Carrizo Plains. The headwaters are located in the La Panza range with the highest point at approximately 3600-feet. The confluence of San Juan Creek with the Estrella River occurs at Shandon. The dominant land use is agriculture. The San Juan Creek Valley is generally used most intensively for agriculture because of better soils and water availability. Irrigated production has increased during the last 10 years, particularly in vineyards and alfalfa. Dry farming and grazing operations encompass the rest of the agricultural uses. The riparian forest and a portion of the adjacent upland areas associated with the Estrella River and San Juan Creek in the vicinity of Shandon are important wildlife habitat, and serve as important corridors for wildlife movement. San Joaquin kit fox and Western burrowing owl occur in open grasslands. Another important wildlife movement corridor is located near the base of the hillside near the eastern edge of Shandon. Existing Watershed Plans: No existing plans to date Watershed Management Plan Phase 1 Lower San Juan Creek Watershed, Section 3.2.3.6, page 167 Lower San Juan Creek Watershed Characteristics Physical Setting Rainfall Average Annual: 9-13 in. -
1 Collections
A. andersonii A. Gray SANTA CRUZ MANZANITA San Mateo Along Skyline Blvd. between Gulch Road and la Honda Rd. (A. regismontana?) Santa Cruz Along Empire Grade, about 2 miles north of its intersection with Alba Grade. Lat. N. 37° 07', Long. 122° 10' W. Altitude about 2550 feet. Santa Cruz Aong grade (summit) 0.8 mi nw Alba Road junction (2600 ft elev. above and nw of Ben Lomond (town)) - Empire Grade Santa Cruz Near Summit of Opal Creek Rd., Big Basin Redwood State Park. Santa Cruz Near intersection of Empire Grade and Alba Grade. ben Lomond Mountain. Santa Cruz Along China Grade, 0.2 miles NW of its intersection with the Big Basin-Saratoga Summit Rd. Santa Cruz Nisene Marks State Park, Aptos Creek watershed; under PG&E high-voltage transmission line on eastern rim of the creek canyon Santa Cruz Along Redwood Drive 1.5 miles up (north of) from Monte Toyon Santa Cruz Miller's Ranch, summit between Gilroy and Watsonville. Santa Cruz At junction of Alba Road and Empire Road Ben Lomond Ridge summit Santa Cruz Sandy ridges near Bonny Doon - Santa Cruz Mountains Santa Cruz 3 miles NW of Santa Cruz, on upper UC Santa Cruz campus, Marshall Fields Santa Cruz Mt. Madonna Road along summit of the Santa Cruz Mountains. Between Lands End and Manzanitas School. Lat. N. 37° 02', Long. 121° 45' W; elev. 2000 feet Monterey Moro Road, Prunedale (A. pajaroensis?) A. auriculata Eastw. MT. DIABLO MANZANITA Contra Costa Between two major cuts of Cowell Cement Company (w face of ridge) - Mount Diablo, Lime Ridge Contra Costa Immediately south of Nortonville; 37°57'N, 121°53'W Contra Costa Top Pine Canyon Ridge (s-facing slope between the two forks) - Mount Diablo, Emmons Canyon (off Stone Valley) Contra Costa Near fire trail which runs s from large spur (on meridian) heading into Sycamore Canyon - Mount Diablo, Inner Black Hills Contra Costa Off Summit Dr. -
October 3, 2018
Cuyama Valley Groundwater Basin Groundwater Sustainability Plan Hydrogeologic Conceptual Model Draft Prepared by: October 2018 Table of Contents Chapter 2 Basin Setting .......................................................................................................2-2 Acronyms 2-3 2.1 Hydrogeologic Conceptual Model ..........................................................................2-4 2.1.1 Useful Terminology ................................................................................................2-4 2.1.2 Regional Geologic and Structural Setting ..............................................................2-5 2.1.3 Geologic History ....................................................................................................2-5 2.1.4 Geologic Formations/Stratigraphy .........................................................................2-8 2.1.5 Faults and Structural Features ............................................................................. 2-17 2.1.6 Basin Boundaries ................................................................................................ 2-26 2.1.7 Principal Aquifers and Aquitards .......................................................................... 2-26 2.1.8 Natural Water Quality Characterization ................................................................ 2-32 2.1.9 Topography, Surface Water and Recharge .......................................................... 2-36 2.1.10 Hydrogeologic Conceptual Model Data Gaps ..................................................... -
Abies Bracteata Revised 2011 1 Abies Bracteata (D. Don) Poit
Lead Forest: Los Padres National Forest Forest Service Endemic: No Abies bracteata (D. Don) Poit. (bristlecone fir) Known Potential Synonym: Abies venusta (Douglas ex Hook.) K. Koch; Pinus bracteata D. Don; Pinus venusta Douglas ex Hook (Tropicos 2011). Table 1. Legal or Protection Status (CNDDB 2011, CNPS 2011, and Other Sources). Federal Listing Status; State Heritage Rank California Rare Other Lists Listing Status Plant Rank None; None G2/S2.3 1B.3 USFS Sensitive Plant description: Abies bracteata (Pinaceae) (Fig. 1) is a perennial monoecious plant with trunks longer than 55 m and less than 1.3 m wide. The branches are more-or-less drooping, and the bark is thin. The twigs are glabrous, and the buds are 1-2.5 cm long, sharp-pointed, and non- resinous. The leaves are less than 6 cm long, are dark green, faintly grooved on their upper surfaces, and have tips that are sharply spiny. Seed cones are less than 9 cm long with stalks that are under15 mm long. The cones have bracts that are spreading, exserted, and that are 1.5–4.5 cm long with a slender spine at the apex. Taxonomy: Abies bracteata is a fir species and a member of the pine family (Pinaceae). Out of the fir species growing in North America (Griffin and Critchfield 1976), Abies bracteata has the smallest range and is the least abundant. Identification: Many features of A. bracteata can be used to distinguish this species from other conifers, including the sharp-tipped needles, thin bark, club-shaped crown, non-resinous buds, and exserted spine tipped bracts (Gymnosperms Database 2010). -
Cholame Creek Watershed
Cholame Creek Watershed Hydrologic Water Acreage Flows to Groundwater Jurisdictions Unit Name Planning Basin(s) Area Estrella Cholame 151,701 Estrella Paso Robles County of San Luis Obispo, 17 WPA 15 acres total River– to Shandon (ptn) with Salinas 47,300 River and acres in Pacific San Luis Ocean Obispo (Monterey County bay National Marine Sanctuary) Description: The Cholame Watershed is located in the North easterly portion of San Luis Obispo County and crosses the county line entering Monterey County to the North. 47,300 acres of the total 151,701 acres are located in SLO County. The watershed is drained by Cholame Creek and its tributaries southeastward and westward into the Estrella River (a tributary to the Salinas River) with the Photo: Althouse and Meade confluence of the Estrella River and Cholame Creek occurring at the town of Shandon. The Cholame Creek watershed is a lightly-populated rural setting and drains into an alluvial valley and surrounding mountains within an ecosystem characterized of grassland, chaparral, oak woodland, and sagebrush and minor amounts of cropland, primarily consisting of grain or hay crops. The dominant land use is agriculture. The area around Shandon Valley is generally used most intensively for agriculture because of better soils and water availability. Irrigated production has increased during the last 10 years, particularly in vineyards and alfalfa. Dry farming and grazing operations encompass the rest of the agricultural uses. The highest Existing Watershed Plans: watershed elevation within the County limits is at approximately 2,476-feet with the lowest No existing plans to date elevation occurring at approximately 1,017-feet. -
Paso Robles Subbasin First Annual Report (2017—2019)
FINAL Paso Basin Cooperative Committee and the Groundwater Sustainability Agencies Paso Robles Subbasin First Annual Report (2017—2019) March 25, 2020 Prepared by: GSI Water Solutions, Inc. 5855 Capistrano Avenue, Suite C, Atascadero, CA 93422 This page intentionally left blank. Paso Robles Subbasin First Annual Report (2017–2019) This report was prepared by the staff of GSI Water Solutions, Inc. under the supervision of professionals whose signatures appear below. The findings or professional opinion were prepared in accordance with generally accepted professional engineering and geologic practice. Paul A. Sorensen, PG, CHg, CEG Nathan R. Page, PG Principal Hydrogeologist Consulting Hydrogeologist Project Manager This page intentionally left blank. FINAL | Paso Robles Subbasin First Annual Report (2017—2019) Contents Contents ..................................................................................................................................................................... v Abbreviations and Acronyms ................................................................................................................................... ix Annual Report Elements Guide and Checklist ........................................................................................................ xi Executive Summary (§ 356.2[a]) ............................................................................................................................. 1 Introduction ..........................................................................................................................................................