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TYPICAL VALLEY INDIAN HOMES Vol. 2 No. 11 YUBA CITY, CALIFORNIA
Vol. 2 No. 11 YUBA CITY, CALIFORNIA OCTOBER 17 1961 TYPICAL VALLEY INDIAN HOMES SUTTER COUNTY HISTORICAL SOCIETY FALL MEETING OCTOBER 17, 1961 TUESDAY EVENING — 8 P.M. PLACE: Board of Supervisors Chambers County Office Building, 2nd Street PRESIDENT: Mrs. Florence Arritt PROGRAM CHAIRMAN: Randolph Schnabel PROGRAM SPEAKER: Waddell F. Smith President, National Pony Express Centennial Association TOPIC: The History of the Pony Express and Its Centennial BOARD OF DIRECTORS MINUTES October 5, 1961 The Board of Directors of Sutter County Historical Society met in regular session October 5, 1961 at 7:30 P.M. in the office of the County Superintendent. The meeting was called to order by Vice President, Mrs. Ida Littlejohn in the absence of the president, Mrs. Florence Arritt. Mrs. Arritt is on her vacation traveling in the southwest and visiting many spots of historic interest such as Tombstone, Arizona. The minutes of the July Board meeting and regular meeting were read and approved. The treasurer reported cash in the bank $737.33. Film Fund $447.00 and general fund $290.33. Mr. Ramey reported a membership of 111. Fifteen new members were secured at the county fair booth. The following bills were approved for payment: Valley Print Shop — Membership Cards, Stationery $41.70. County of Sutter — Bulletin pictures $6.20. Earl Ramey — Postage $3.50. Program Chairman, Randolph Schnabel reported the program had already been arranged for the annual dinner meeting in January. Mrs. Gibson presented an invitation to the Sutter County Historical Society to en- tertain the Symposium of Historical Societies of Northern California and Southern Oregon in the fall of 1962. -
Enhancing Environmental Flows of Putah Creek for Chinook Salmon Reproductive Requirements
Enhancing environmental flows of Putah Creek for Chinook salmon reproductive requirements Written by: Chan, Brian; Jasper, Chris Reynolds; Stott, Haley Kathryn UC Davis, California ESM 122, Water Science and Management, Section: A02 Abstract: Putah creek, like many of California’s rivers and streams, is highly altered by anthropogenic actions and historically supported large populations of resident and anadromous native fish species. Now its ecosystem dynamics have changed drastically with the Monticello dam, the Solano diversion canal and the leveeing of its banks. Over time the creek has found a balance of habitats for native and non-native fish species that is mainly dictated by species-preferred temperature tolerances (Keirman et. al. 2012). Cooler temperatures and faster flows upstream from Davis prove to be ideal habitats for native species, in particular, the federally endangered Chinook salmon, which is the most widely distributed and most numerous run occurring in the Sacramento and San Joaquin rivers and their tributaries. As water moves downstream, it becomes shallower and warmer, resulting in ideal conditions for non-native species (Winters, 2005). This report analyzes the environmental flows released into putah creek and how much salmon preferred breeding habitat is available from this flow regime based on temperature. Introduction: Figure 1: Teale GIS Solutions Group (1999), US Census Bureau (2002), USGS (1993) [within Winters, 2005] The Putah Creek watershed is an important aspect in the natural, social, and economic livelihoods of the people of Yolo and Solano counties. The Putah Creek watershed begins at the highest point in Lake County, Cobb Mountain, and flows down to the Central Valley where it empties into the Yolo Bypass at near sea level. -
Geologic Features and Ground-Water Storage Capacity of the Sacramento Valley California
Geologic Features and Ground-Water Storage Capacity of the Sacramento Valley California By F. H. OLMSTED and G. H. DAVIS GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1497 Prepared in cooperation with the California Department of ff^ater Resources UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1961 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director Tlie TT.S. Geological Survey Library catalog card for this publication appears after page 241. For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. CONTENTS Page Abstract___________________________________________________ -_ 1 Introduction.-.--- .___-___________-___._--.______-----_ 5 Purpose and scope of the investigation.__________________ ______ 5 Location of area__-__-________-____________-_-___-_-__--____-_- 6 Development of ground water___________________-___-__ ___ __ 7 Acknowledgments....-------- ____________ _________________ 8 Well-numbering system..________________________________ _ 9 Geology--__--_--_--__----_--_-----____----_ --_ ___-__-- 10 Geomorphology_____________________________________________ 10 General features _______________________________________ 10 Mountainous region east of the Sacramento Valley...__________ 11 Sierra Nevada_______________________________________ 11 Cascade Range.._____________________-__--_-__-_---- 13 Plains and foothill region on the east side of the Sacramento Valley..__-_________-_.-____.___________ 14 Dissected alluvial uplands west of the Sierra -
Table of Contents Executive Summary
MARCH 2012 SACRAMENTO VALLEY WATER QUALITY COALITION Monitoring and Reporting Program Plan Annual Monitoring Report 2011 Prepared by: LARRY WALKER ASSOCIATES Table of Contents Executive Summary ...................................................................................................................... v Summary of Monitoring Program ............................................................................................... v Management Practices and Actions Taken ................................................................................ vi Conclusions and Recommendations ......................................................................................... vii Introduction ................................................................................................................................... 1 Description of the Watershed ...................................................................................................... 3 Monitoring Objectives .................................................................................................................. 4 Sampling Site Descriptions .......................................................................................................... 6 Sampling Site Locations and Land Uses .................................................................................... 7 Site Descriptions ......................................................................................................................... 9 Butte/Yuba/Sutter Subwatershed ........................................................................................... -
Emigration of Juvenile Chinook Salmon (Oncorhynchus Tshawytscha) in the Feather
State of California The Resources Agency Department of Water Resources Division of Environmental Services Emigration of Juvenile Chinook Salmon (Oncorhynchus tshawytscha) in the Feather River, 2002-2004. May 2005 Table of Contents Table of Contents.............................................................................................................ii List of Tables...................................................................................................................iii List of Figures..................................................................................................................iv Summary......................................................................................................................... 1 Introduction ..................................................................................................................... 2 Methods .......................................................................................................................... 3 Study Area ................................................................................................................... 3 Field Collection Methods .............................................................................................. 3 Trap Efficiency and Emigration Estimate...................................................................... 5 Results ............................................................................................................................ 9 RST Catch and Species Composition ......................................................................... -
Existing Program Summary Central Valley Salmon and Steelhead
EXISTING PROGRAM SUMMARY CENTRAL VALLEY SALMON AND STEELHEAD MONITORING PROGRAMS Photos: Tim Heyne, Doug Killam, Doug Demko, Colleen Harvey Arrison Contributors: Interagency Ecological Program Salmonid Escapement Project Work Team Interagency Ecological Program Juvenile Monitoring Project Work Team Edited by: Alice Low Department of Fish and Game May 2007 Contents I - Central Valley Adult Salmonid Escapement Monitoring Programs Central Valley-wide Chinook salmon and steelhead angler survey………………………………………. I-2 Upper Sacramento River Basin Mainstem Sacramento River All Chinook runs – aerial redd survey.………………………………………… I-5 Fall, winter, spring-run Chinook – ladder counts at RBDD…………………… I-11 Fall, late fall-run Chinook carcass survey…………………………....……….. I-14 Winter-run Chinook carcass survey……..………………………..…………… I-17 Upper Sacramento River Basin Tributaries Antelope Creek – Spring-run Chinook snorkel survey………………………..I-21 Beegum Creek – Spring-run Chinook snorkel survey………………………... I-24 Mill Creek – Spring-run Chinook redd survey………...………………..……. I-27 Spring-run Chinook hydroacoustic study………………………..I-30 Fall-run Chinook carcass survey……………..………………….I-33 Deer Creek – Spring-run Chinook snorkel survey……………..…..…………. I-36 Fall-run Chinook carcass survey……..………………………….I-39 Clear Creek –Fall-run Chinook carcass survey………………………………...I-42 Fall-run Chinook redd mapping…………….…………………...I-45 Spring-run Chinook snorkel survey………………………...…...I-47 Late-fall Chinook and steelhead redd survey………………..…. I-50 Cow Creek – Fall-run Chinook video monitoring……………………………. -
Sacramento River Flood Control System
A p pp pr ro x im a te ly 5 0 M il Sacramento River le es Shasta Dam and Lake ek s rre N Operating Agency: USBR C o rt rr reek th Dam Elevation: 1,077.5 ft llde Cre 70 I E eer GrossMoulton Pool Area: 29,500 Weir ac AB D Gross Pool Capacity: 4,552,000 ac-ft Flood Control System Medford !( OREGON IDAHOIDAHO l l a a n n a a C C !( Redding kk ee PLUMAS CO a e a s rr s u C u s l l Reno s o !( ome o 99 h C AB Th C NEVADA - - ^_ a a Sacramento m TEHAMA CO aa hh ee !( TT San Francisco !( Fresno Las Vegas !( kk ee e e !( rr Bakersfield 5 CC %&'( PACIFIC oo 5 ! Los Angeles cc !( S ii OCEAN a hh c CC r a S to m San Diego on gg !( ny ii en C BB re kk ee ee k t ee Black Butte o rr C Reservoir R i dd 70 v uu Paradise AB Oroville Dam - Lake Oroville Hamilton e M Operating Agency: CA Dept of Water Resources r Dam Elevation: 922 ft City Chico Gross Pool Area: 15,800 ac Gross Pool Capacity: 3,538,000 ac-ft M & T Overflow Area Black Butte Dam and Lake Operating Agency: USACE Dam Elevation: 515 ft Tisdale Weir Gross Pool Area: 4,378 ac 3 B's GrossMoulton Pool Capacity: 136,193Weir ac-ft Overflow Area BUTTE CO New Bullards Bar Dam and Lake Operating Agency: Yuba County Water Agency Dam Elevation: 1965 ft Gross Pool Area: 4,790 ac Goose Lake Gross Pool Capacity: 966,000 ac-ft Overflow Area Lake AB149 kk ee rree Oroville Tisdale Weir C GLENN CO ee tttt uu BB 5 ! Oroville New Bullards Bar Reservoir AB49 ll Moulton Weir aa nn Constructed: 1932 Butte aa CC Length: 500 feet Thermalito Design capacity of weir: 40,000 cfs Design capacity of river d/s of weir: 110,000 cfs Afterbay Moulton Weir e ke rro he 5 C ! Basin e kk Cre 5 ! tt 5 ! u Butte Basin and Butte Sink oncu H Flow from the 3 overflow areas upstream Colusa Weir of the project levees, from Moulton Weir, Constructed: 1933 and from Colusa Weir flows into the Length: 1,650 feet Butte Basin and Sink. -
SWFSC Archive
Historical Population Structure of Central Valley Steelhead and its Alteration by Dams STEVEN T. LINDLEY1, ROBERT S. SCHICK1, ADITYA AGRAWAL2, MATTHEW GOSLIN2, THOMAS E. PEARSON2, ETHAN MORA2, JAMES J. ANDERSON3, BERNARD MAY4, SHEILA GREENE5, CHARLES HANSON6, ALICE LOW7, DENNIS MCEWAN7, R. BRUCE MACFARLANE1, CHRISTINA SWANSON8 AND JOHN G. WILLIAMS9 ABSTRACT Effective conservation and recovery planning for Central Valley steelhead requires an understanding of historical population structure. We describe the historical structure of the Central Valley steelhead evolutionarily significant unit using a multi-phase modeling approach. In the first phase, we identify stream reaches possibly suitable for steelhead spawning and rearing using a habitat model based on environmental envelopes (stream discharge, gradient, and temperature) that takes a digital elevation model and climate data as inputs. We identified 151 patches of potentially suitable habitat with more than 10 km of stream habitat, with a total of 25,500 km of suitable habitat. We then measured the dis- tances among habitat patches, and clustered together patches within 35 km of each other into 81 dis- tinct habitat patches. Groups of fish using these 81 patches are hypothesized to be (or to have been) independent populations for recovery planning purposes. Consideration of climate and elevation differ- ences among the 81 habitat areas suggests that there are at least four major subdivisions within the Central Valley steelhead ESU that correspond to geographic regions defined by the Sacramento River basin, Suisun Bay area tributaries, San Joaquin tributaries draining the Sierra Nevada, and lower-ele- vation streams draining to the Buena Vista and Tulare basins, upstream of the San Joaquin River. -
Supervisorial Districts 2 & 4
Supervisorial Districts 2 & 4 er a Riv e Yub Middl 80 89 ¨¦§ Ãà yler Foote Crossi T ng Rd H o l le 5 y R a TRUCKEE v in e 89 r Trap Rd Walls R 80 à Bea d à d 20 ¨¦§ d Flat R à R t à 267 t G a 49 in l à o r F à P i à z à s g d z ll on gs R l a L Malakoff rin y W 1 Sp R p id Holiday Estates ra g r Black Wy T e ve d r R NEVADA CITY i R Sand d d a R ill R rp R e d a e a B b M Mine in t E Kaiser Ct u d M t Y l d ! s ya n G O R nd zo ra a W ru de e S I Oregon Creek l k ck n C R a la d 174 d B d H y e erbe d O i lm D c à ÆQ i g C R r W t à o d K e 3 M d e u k R W GRASS VALLEY Oregon Creek g | r i e o n i f d o s y R h s x Camp n s H o er ro r in F North e M C iv n Badger Hill h Rd e d d nc R k Oregon Creek J e a n un R R t R Bloomfield ru y g y a le e o D T (historical) a e a Covered Bridge l i w n B o s b y i d e b R ar F a u B M C S k an m d C e yo r d a n n u R Mi dl Y g e R l e o r d e e l M 4 o e C s R C S I m g San Juan y i d y u C c A l l R a lm z n u a T o z f R d d ra ri ri LAI a R S s e B 2 R d Ridge G e T S L ob cco R n a c R h d North N o Rd North o r Hill e Badge d d l Malakoff Diggins SHP R c w R t R i yron e C y San Juan B h Sugarloaf T k r i Columbia n r W S F ! a d n B R and U F D or is c North l e r R Peak R A l e i d b u h L m c m s d a e o S r R h Malakoff e Cherokee n Diggins S J o a C L d o j | Bloomfield a R S l n n a L B T ss a c t R te Cro ing Rd l a (historical) R o y k S Preston Rd o k k Pond Old Rd d r F k ! c a c h y yle S e Malakoff Diggins-North o O W T s C a Crystal s o ak d i B l T d o ty d r S r R o F e n h -
Draft Central Valley Salmon and Steelhead Recovery Plan
Draft Central Valley Salmon and Steelhead Recovery Plan for Sacramento River winter-run Chinook salmon Central Valley spring-run Chinook Salmon Central Valley Steelhead National Marine Fisheries Service Southwest Region November 2009 1 Themes of the CV Recovery Plan • This is a long-term plan that will take several decades to fully implement • The recovery plan is intended to be a “living document” that is periodically updated to include the best available information regarding the status or needs of the species • Implementation will be challenging and will require the help of many stakeholders • The plan is intended to have realistic and attainable recovery criteria (i.e, de-listing criteria) 2 What are Recovery Plans? • Purpose of the Endangered Species Act: To conserve (recover) listed species and their ecosystems • Required under section 4(f) of the ESA for all Federally listed species • Provide the road map to species recovery • Must contain objective, measurable criteria for delisting a species • Guidance documents, not regulations 3 Winter-run Chinook salmon (Endangered) 4 Status of Species – Winter-run Chinook 5 Central Valley Spring-run Chinook salmon (Threatened) 6 Status of Species – Spring-run Chinook Declining abundance across range: Extinction risk is increasing Central Valley Spring-run Chinook Salmon Adult Summer Holding Escapement Rivers/Creeks 25,000 Sacramento Battle 20,000 Clear Beegum 15,000 Antelope Mill 10,000 Deer Big Chico 5,000 Butte 0 1998 2000 2002 2004 2006 2008 7 Central Valley steelhead (Threatened) 8 Key -
Diverse Metamorphic Trajectories, Imbricated Ocean Plate Stratigraphy, and Fault Rocks, Yuba River Area, Feather River Ultramafic Belt, California
ABSTRACT DIVERSE METAMORPHIC TRAJECTORIES, IMBRICATED OCEAN PLATE STRATIGRAPHY, AND FAULT ROCKS, YUBA RIVER AREA, FEATHER RIVER ULTRAMAFIC BELT, CALIFORNIA The Feather River Belt (FRB), the most extensive of the ultramafic belts in the Sierra Nevada, is a north–south trending 150-km-long by 1-8 km wide ultramafic belt and includes related rocks that form the basement of the northern Sierra Nevada of California. These rocks have been long interpreted as a Paleozoic to early Mesozoic "suture" zone (position of former subduction zone) and provide a good opportunity to more closely investigate the details of the rock record associated with subduction processes. Conventional tectonic models cannot explain the spatial-temporal distribution of the metamorphic grade of the FRB. Geologic mapping, petrographic, and electron microprobe analyses reveal a complex spatial and relative time relationships between different lithologies and units of different metamorphic grade. In the greater Middle and North Yuba River area, ultramafic rocks structurally overlie amphibolite, composed of primarily metamafic rocks, that structurally overlies the blueschist facies Red Ant schist (RAS). These tectonic contacts have been isoclinally folded at scales of hundreds of meters to a km. In the North Yuba River area, amphibolite records low- pressure, high-temperature metamorphism with redbrown (high Ti, low Al) amphibole and ilmenite. In the Forest City and Alleghany areas on the North Fork-Middle Fork divide, amphibolite grade rocks comprise imbricates of ocean plate stratigraphy, represented by repeated sheets of metabasites, metacherts, and metaclastics. These rocks include zones of cataclasites with pseudotachylites (frictional melts generated by fault movement). The Alleghany amphibolites ii appear to comprise two slabs with contrasting metamorphic history. -
Bathymetric and Geophysical Surveys of Englebright Lake, Yuba-Nevada Counties, California
US Geological Survey Open-File Report 03-383 Bathymetric and geophysical surveys of Englebright Lake, Yuba-Nevada Counties, California by Jonathan R. Childs, Noah P. Snyder, and Margaret A. Hampton This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Geological Survey or the Department of the Interior. INTRODUCTION Harry L. Englebright Lake (Englebright Lake, Figure 1) is a 9-mile-long (14-kilometer) reservoir located in the Sierra Nevada foothills of northern California on the Yuba River gorge known as The Narrows. The reservoir is impounded by Englebright Dam (photo, page 3), a concrete arch structure spanning 348 meters (1,142 feet) across and 79 meters (260 feet) high. The dam was constructed in 1941 for the primary purpose of trapping sediment derived from anticipated hydraulic mining operations in the Yuba River watershed. Hydraulic mining in the Sierra Nevada was halted in 1884 but resumed on a limited basis until the 1930's under the regulation of the California Debris Commission. Although no hydraulic mining in the upper Yuba River watershed resumed after the construction of the dam, the historical mine sites continued to contribute sediment to the river. Today, Englebright Lake is used primarily for recreation and hydropower. In 2001 and 2002, the U.S. Geological Survey (USGS) conducted bathymetric, geophysical, geophysical, and geological studies of the reservoir under the auspices of the Upper Yuba River Studies Program (UYRSP), a multi-disciplinary investigation into the feasibility of introducing anadromous fish species to the Yuba River system upstream of Englebright Dam.