Sierra Nevada Framework FEIS Chapter 3
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Sites Reservoir Project Public Draft EIR/EIS
12. Aquatic Biological Resources 12.1 Introduction This chapter describes the aquatic habitat and fish resources found within the Extended, Secondary, and Primary study areas. Descriptions and maps of these three study areas are provided in Chapter 1 Introduction. Fish species of management concern include special-status species and species that have substantial tribal, commercial or recreation value. The biology and life history of these species are described in Appendix 12A Aquatic Species Life Histories. Permits and authorizations for aquatic biological resources are presented in Chapter 4 Environmental Compliance and Permit Summary. The regulatory setting for aquatic biological resources is presented in Appendix 4A Environmental Compliance. The descriptions and evaluation of potential impacts in this chapter are presented using a broad, generalized approach for the Secondary and Extended study areas, whereas the Primary Study Area is presented in greater detail. Potential local and regional impacts from constructing, operating, and maintaining the alternatives are described and compared to applicable significance thresholds. Mitigation measures are provided for identified significant or potentially significant impacts, where appropriate. The descriptions of species and biological and hydrodynamic processes in this chapter frequently use the terms “Delta” and “San Francisco Estuary.” The Delta refers to the Sacramento-San Joaquin Delta, as legally defined in the Delta Protection Act. The San Francisco Estuary refers to the portion of the Sacramento-San Joaquin rivers watershed downstream of Chipps Island that is influenced by tidal action, and where fresh water and salt water mix. The estuary includes Suisun, San Pablo, and San Francisco bays. 12.2 Environmental Setting/Affected Environment This section, which is organized by study area, describes fish and aquatic resources that would be affected by the implementation of the alternatives considered in this EIR/EIS. -
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 -
4. Climate and Hydrology Many Aspects of the Physical Setting of Butte County Play a Role in the Hydrologic Cycle Within the County
Butte County 4. Climate and Water Inventory and Analysis Hydrology 4. Climate and Hydrology Many aspects of the physical setting of Butte County play a role in the hydrologic cycle within the County. Topography within the County significantly impacts precipitation patterns. Temperature variations influence whether precipitation falls as rain or snow, which in turn impacts the timing of surface water runoff. Temperature and other factors also influence the evaporative demand of the atmosphere and corresponding irrigation requirements for crops. Both surface water and extracted groundwater are used to meet the water demands. System components impacting water resources in the County described in this section include climate, surface water hydrology, and groundwater hydrology. 4.1 Climate Butte County has a Mediterranean climate with cool, wet winters and hot, dry summers. Unlike many locations in California, rainfall and winter snowpack in the Sierra Nevada provide significant surface water flows and groundwater recharge as water drains through the County. Climate variation within the County occurs primarily due to changes in elevation. Precipitation is least on the valley floor and greatest in the Foothill Inventory Unit (IU) and Mountain IU areas as elevation increases. Conversely, temperatures are warmest on the valley floor and coolest in the mountains. Similarly, reference evapotranspiration (ETo), a measure of evaporative demand, is greatest on the valley floor and least in the mountains. This variability in climate is discussed in greater detail in the following sections. 4.1.1 Precipitation Average annual precipitation generally increases from west to east across Butte County, associated with increasing elevation. Moisture-laden weather patterns from the Pacific Ocean travel west to east across California and Butte County during the winter months. -
Gazetteer of Surface Waters of California
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTI8 SMITH, DIEECTOE WATER-SUPPLY PAPER 296 GAZETTEER OF SURFACE WATERS OF CALIFORNIA PART II. SAN JOAQUIN RIVER BASIN PREPARED UNDER THE DIRECTION OP JOHN C. HOYT BY B. D. WOOD In cooperation with the State Water Commission and the Conservation Commission of the State of California WASHINGTON GOVERNMENT PRINTING OFFICE 1912 NOTE. A complete list of the gaging stations maintained in the San Joaquin River basin from 1888 to July 1, 1912, is presented on pages 100-102. 2 GAZETTEER OF SURFACE WATERS IN SAN JOAQUIN RIYER BASIN, CALIFORNIA. By B. D. WOOD. INTRODUCTION. This gazetteer is the second of a series of reports on the* surf ace waters of California prepared by the United States Geological Survey under cooperative agreement with the State of California as repre sented by the State Conservation Commission, George C. Pardee, chairman; Francis Cuttle; and J. P. Baumgartner, and by the State Water Commission, Hiram W. Johnson, governor; Charles D. Marx, chairman; S. C. Graham; Harold T. Powers; and W. F. McClure. Louis R. Glavis is secretary of both commissions. The reports are to be published as Water-Supply Papers 295 to 300 and will bear the fol lowing titles: 295. Gazetteer of surface waters of California, Part I, Sacramento River basin. 296. Gazetteer of surface waters of California, Part II, San Joaquin River basin. 297. Gazetteer of surface waters of California, Part III, Great Basin and Pacific coast streams. 298. Water resources of California, Part I, Stream measurements in the Sacramento River basin. -
List of Fish and Game Commission Designated Wild Trout Waters
The following waters are designated by the Commission as "wild trout waters": 1. American River, North Fork, from Palisade Creek downstream to Iowa Hill Bridge (Placer County). 2. Carson River, East Fork, upstream from confluence with Wolf Creek excluding tributaries (Alpine County). 3. Clavey River, upstream from confluence with Tuolumne River excluding tributaries (Tuolumne County). 4. Fall River, from Pit No. 1 powerhouse intake upstream to origin at Thousand Springs including Spring Creek, but excluding all other tributaries (Shasta County). 5. Feather River, Middle Fork, from Oroville Reservoir upstream to Sloat vehicle bridge, excluding tributaries (Butte and Plumas counties). 6. Hat Creek, from Lake Britton upstream to Hat No. 2 powerhouse (Shasta County). 7. Hot Creek, from Hot Springs upstream to west property line of Hot Creek Ranch (Mono County). 8. Kings River, from Pine Flat Lake upstream to confluence with South and Middle forks excluding tributaries (Fresno County). 9. Kings River, South Fork, from confluence with Middle Fork upstream to western boundary of Kings Canyon National Park excluding tributaries (Fresno County). 10. Merced River, South Fork, from confluence with mainstem Merced River upstream to western boundary of Yosemite National Park excluding tributaries (Mariposa County). 11. Nelson Creek, upstream from confluence with Middle Fork Feather River excluding tributaries (Plumas County). 12. Owens River, from Five Bridges crossing upstream to Pleasant Valley Dam excluding tributaries (Inyo County). 13. Rubicon River, from confluence with Middle Fork American River upstream to Hell Hole Dam excluding tributaries (Placer County). 14. Yellow Creek, from Big Springs downstream to confluence with the North Fork of the Feather River (Plumas County). -
Sacramento-San Joaquin Delta Chapter
Evolution of River Flows in the Sacramento and San Joaquin Valleys Historical Level of Development Study Technical Memorandum, Final March 2016 Prepared by MWH for the Metropolitan Water District of Southern California …… Table of Contents Executive Summary .................................................................................................................................... 1 Study Approach ......................................................................................................................................... 1 Modeling Tools ......................................................................................................................................... 2 Model Validation ....................................................................................................................................... 3 Model Results ............................................................................................................................................ 3 Climate Change ......................................................................................................................................... 9 Conclusions ............................................................................................................................................... 9 Chapter 1 Purpose and Scope of Work .......................................................................................... 1-1 Study Approach ..................................................................................................................................... -
Section 3 Existing Environment
Yuba County Water Agency Narrows Hydroelectric Project FERC Project No. 1403 SECTION 3 EXISTING ENVIRONMENT In addition to this introductory information, this section is divided into two subsections. Section 3.1 provides a general description of the river basin in which the Project occurs. Section 3.2 provides existing, relevant and reasonably available information regarding the resources. 3.1 General Description of the River Basin 3.1.1 Existing Water Projects in the Yuba River Basin Sixteen existing water projects occur in the Yuba River Basin. Eight of the water projects are licensed or exempt from licensing by FERC. Together, these eight projects have a combined FERC-authorized capacity of 782.1 MW, of which the Narrows Hydroelectric Project has approximately 1.5 percent of the total capacity. The remaining eight non-FERC-licensed projects do not contain generating facilities. Each of these water projects is described briefly below. 3.1.1.1 Narrows Hydroelectric Project The existing Narrows Hydroelectric Project is described in detail in Section 2 of this PAD. 3.1.1.2 Upstream of the Narrows Hydroelectric Project 3.1.1.2.1 South Feather Power Project The 117.5-MW South Feather Power Project, FERC Project No. 2088, is a water supply/power project constructed in the late 1950s/early 1960s and is owned and operated by the South Feather Water and Power Agency (SFWPA). None of the project facilities or features is located in the Yuba River watershed except for the Slate Creek Diversion Dam, which is located on a tributary to the North Yuba River. -
Foothill Yellow-Legged Frog Comments
The Center for Biological Diversity submits the following information for the status review of the foothill yellow-legged frog (Rana boylii) (Docket #FWS-R8-ES-2015-0050), including substantial new information regarding the species' biology, population structure (including potential Distinct Population Segments of the species), historical and recent distribution and status, population trends, documented range contraction, habitat requirements, threats to the species and its habitat, disease, and the potential effects of climate change on the species and its habitat. The foothill yellow-legged frog has experienced extensive population declines throughout its range and a significant range contraction. Multiple threats continue unabated throughout much of the species’ remaining range, including impacts from dams, water development, water diversions, timber harvest, mining, marijuana cultivation, livestock grazing, roads and urbanization, recreation, climate change and UV-radiation, pollution, invasive species and disease. The species warrants listing as threatened under the Endangered Species Act. Contact: Jeff Miller, [email protected] Contents: NATURAL HISTORY, BIOLOGY AND STATUS . .. 2 Biology. .2 Habitat . .. .4 Range and Documented Range Contraction . 4 Taxonomy . 9 Population Structure . 9 Historical and Recent Distribution and Status . 15 Central Oregon . .15 Southern Oregon . 18 Coastal Oregon . .20 Northern Coastal California . 25 Upper Sacramento River . 40 Marin/Sonoma . 45 Northern/Central Sierra Nevada . .47 Southern Sierra Nevada . .67 Central Coast/Bay Area . 77 South Coast. 91 Southern California . .. 94 Baja California, Mexico . .98 Unknown Population Affiliation. .99 Population Trends . .. .103 THREATS. .108 Habitat Alteration and Destruction . .. 108 Dams, Water Development and Diversions . .. .109 Logging . .. .111 Marijuana Cultivation . .. .112 Livestock Grazing . .. .112 Mining . .. .. .113 Roads and Urbanization . -
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. -
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. -
Management Area 12 - HARVEY
Management Area 12 - HARVEY A. DESCRIPTION Location The Harvey Management Area bor- Management Most of the larger-sized trees in ders the northern edge of the Eagle Lake Dis- the area have been harvested Cattle graze the trict The southern boundary isjust northeast of Harvey Valley, Grays Valley, Upper Pine Creek, and a sliver of the Dixie Valley Range Allot- State Highway 44 The most prominent feature is Harvey Mountain, topped by a Forest Servlce ments Hunting is the primary recreation activ- fire lookout ity The Harvey Valley Demonstration Range contains 127 research plots which are monitored intermittently. The eastern boundary of the Physical Environment Slopes on the 7,354 foot Harvey Mountain are moderate to gentle, Blacks Mountain Expenmental Forest adjoins this area Harvey Valley (5,550 feet) and Grays Valley (5,600 feet) in the southwest are almost flat Precipitation averages 33 inches a year Soils Facilities The Lassen and Nobles Emigrant are moderately deep, and surface rock is common Trails cross the area A cinder pit lies on the on the timbered slopes Grays Valley and Harvey western edge Geothermal lease applications Valley have deep alluvial soils, and Harvey Val- have been filed for lands in the area The area is ley soils are clayey Ephemeral streams drain linked to Highway 44 by a well-developed Forest the mountain slopes into Pine Creek in Harvey road system, and the Union Pacific Railroad Valley parallels Highway 44 Biological Environment Eastside pine and B. STANDARDSAND mixed conifer forests, most of them havlng com- GUIDELINES mercial value, and brushfields cover the slopes Grass-sagebrush and wet meadow communities Recreation occupy the flats Fuel loads in the north half of the area are heavy, due pnmanly to timber 1 Manage the undeveloped camping area at harvest. -
Floods in Northern California, January 1997
science for a changing world &2CV FLOODS IN NORTHERN fl' CALIFORNIA, JANUARY 1997 Photo by John Trotter, Jan.4, 1997/Sacramento Bee Photo: The community of Olivehurst was inundated with water after a levee failed on the Feather River INTRODUCTION Flooding in California in recent years has been increased evaporation from the warmer surface water. attributed mostly to climate conditions referred to as the The result is an increase in the number and intensity of "El Nino" effect. However, floods in California also have storms. La Nina, characterized by colder than average been associated with other climate conditions (table 1). ocean temperatures, does not entirely prevent storms of The flood of January 1997 occurred during a weak "La sufficient precipitation to cause flooding in California. Nina" or near-normal (average) climate condition (U.S. Precipitation in the Sierra Nevada mountain range Department of Commerce, 1997). These climate produced an above-normal snowpack and saturated conditions are based on sea-surface water temperatures soils during November and December 1996. A series of and trade-wind velocities in the Pacific Ocean. storms from December 29, 1996, through January 4, Precipitation from storms during any climate condition 1997. brought heavy and relatively warm precipitation generally increases with orographic uplift as the storms across much of California. Precipitation totals of up to move easterly across the mountains of California. 24 inches were recorded for the week. Virtually all of During El Nino, trade winds diminish, and upwelling of this precipitation was rain because temperatures were colder water in the ocean is inhibited along the Pacific above freezing at elevations as high as about 9,000 feet.