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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. -
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 -
Geologic Gems of California's State Parks
STATE OF CALIFORNIA – EDMUND G. BROWN JR., GOVERNOR NATURAL RESOURCES AGENCY – JOHN LAIRD, SECRETARY CALIFORNIA GEOLOGICAL SURVEY DEPARTMENT OF PARKS AND RECREATION – LISA MANGAT, DIRECTOR JOHN D. PARRISH, Ph.D., STATE GEOLOGIST DEPARTMENT OF CONSERVATION – DAVID BUNN, DIRECTOR PLATE 1 The rugged cliffs of Del Norte Coast Redwoods State Park are composed of some of California’s Bio-regions the most tortured, twisted, and mobile rocks of the North American continent. The California’s Geomorphic Provinces rocks are mostly buried beneath soils and covered by vigorous redwood forests, which thrive in a climate famous for summer fog and powerful winter storms. The rocks only reveal themselves in steep stream banks, along road and trail cut banks, along the precipitous coastal cliffs and offshore in the form of towering rock monuments or sea stacks. (Photograph by CalTrans staff.) Few of California’s State parks display impressive monoliths adorned like a Patrick’s Point State Park displays a snapshot of geologic processes that have castle with towering spires and few permit rock climbing. Castle Crags State shaped the face of western North America, and that continue today. The rocks Park is an exception. The scenic beauty is best enjoyed from a distant exposed in the seacliffs and offshore represent dynamic interplay between the vantage point where one can see the range of surrounding landforms. The The Klamath Mountains consist of several rugged ranges and deep canyons. Klamath/North Coast Bioregion San Joaquin Valley Colorado Desert subducting oceanic tectonic plate (Gorda Plate) and the continental North American monolith and its surroundings are a microcosm of the Klamath Mountains The mountains reach elevations of 6,000 to 8,000 feet. -
An Examination of a Barrier Jet in the Sacramento Valley Using the Weather Event Simulator (WES)
An Examination of a Barrier Jet in the Sacramento Valley Using the Weather Event Simulator (WES) James Mathews, WFO Sacramento, CA & John Juskie, WFO Sacramento, CA Introduction Barrier winds or barrier jets are common occurrences in the Sacramento valley due to the orientation of the topography. The Sacramento valley is bounded by the Sierra Nevada Mountains to the east and the coastal range to the west. These mountains often cause terrain-induced winds in the Sacramento valley. As an example, onshore flow from the Pacific Ocean causes air to be forced through the gap in the coastal range mountains called the Golden Gate. Once the air passes through the Carquinez Strait east of the Golden Gate, it spreads out as it reaches the valley and results in a southerly wind direction for the Sacramento valley. Usually, these wind speeds are not strong enough to cause significant problems. However, on occasion, southerly winds can result in the formation of the southerly barrier jet along side the Sierra Nevada Mountains (Parish, 1982). Given unique circumstances, wind speeds can become significant to the public and wind advisories, high wind warnings, or Red Flag Warnings are issued to highlight this phenomenon. Staudenmaier (1994) discussed the formation of a northerly barrier jet and the implications to extreme fire behavior. Staudenmaier offered three conditions forecasters should examine for the potential development of a northerly barrier jet: (1) a sufficiently deep surface or near-surface based layer (at least 150 mbs deep) of northeasterly flow over the Sacramento valley for at least 6 hours, (2) strong stability as shown by the Oakland, CA (KOAK) sounding extending from around 800 mbs to at least as high as the terrain and, (3) enhancement of gusty surface winds if the stable layer caps a slightly less stable layer allowing for momentum transfer to the surface. -
Birding Hotspots of the Northern Sacramento Valley 15 Miles North to Red Bluff ° Upper Bidwell Park !!# !!# 6 Duncan Wildwood !Hcorning ")2 East Ave
Birding Hotspots of the Northern Sacramento Valley 15 miles north to Red Bluff ° Upper Bidwell Park !!# !!# 6 Duncan Wildwood !HCorning ")2 East Ave. Manzanita MainSt Corning 3 ")1 Samuel Ayer/ ") Sacramento River NWR - Bruce Dog Island Park South Ave City Main St Rio Vista Unit ¤£99 Breckenridge of 32 ¤£ Bruce Rd City of Antelope Chico §¨¦I-5 ¤£32 Red £99 Skyway ° Dominic S ¤ S a River Rd. a c ° Bluff c r Morrow r ° a a Genetic Resource & m 11 m Conservation Center Cramer ee n County Rd 200 e tto k o R a R iiv L v ee r e r t t u County Rd 200 I-5 B §¨¦ Sacramento River NWR- k East Ave 6 k k c ")4 Pine Creek Unit ")Bruce Rd e e la Hamilton City ee B Orland ")5 ¤£32 CCrr !H tet e 32 t ¤£ !H t !H uu Black Butte Rd Chico BB ¤£99W ")7 W Sacramento Ave Chico ¤£45 10 11 ")8 ") ") Skyway ")9 Chico River Rd ")12 Oroville-Chico Hwy Sacramento River NWR- ¤£191 Ord Bend Unit River Rd Durham Dayton Hwy ¤£70 ")15 14 Rd 32 Road 33 ") Ord Ferry Road ")17 Grainland Rd ¤£149 Road R ")16 Table # # Llano Seco Unit - Midway !! !! Road WW Mountain ")13 Steve Thompson 18 Road 39 North Central Valley ") Wildlife Mg't Area ¤£99 ")19 Seven Mile Lane Cottonwood Rd. Upper Butte Nelson Rd £162 Basin WA - ")20 ¤ Llano Seco Unit !H ¤£162 Nelson Rd Willows Upper T Road V h 162 !H Aguas Frias Rd ¤£ Butte e Road WW r m Oroville Road 57 Road P Rd 57 Basin WA - Oroville Rd Rd W l Howard i National Wildlife Refuge Road 59 t Larkin Rd Slough Unit ")21 o 22 ¤£162 Af terbay ") Road 60 State Wildlife Area Road 61 !HButte City Oroville Hamilton WA Sacramento State Park 24 River NWR- ") Road Z 23 Packer Unit ") Afton Rd City Park Upper Afton Afton Blvd(RdY) Road 68 !H Butte Roads Sacramento PrincetonPrinceton Basin WA - NWR Little Dry Gravel Creek Unit Butler Rd Adobe Rd !H Gridley Colusa Hwy Gridley Paved Rd. -
Data on California's Extreme Rainfall from 1862- 1995
Data on California's Extreme Rainfall from 1862- 1995 By Jim Goodridge PO Box 970 Mendocino CA 95460 707 937 4709 June 29,1996 Prepared for: 19% CALIFORNIA WEATHER SYMPOSIUM Theme: "A prehistoric Look at California Rainfall and Floods" Sierra College Science Center, 5000 Rocklin Road, Rocklin, CA 95677 Introduction Prehistoric storms sculpted Earth's landscape and left evidences of their effects every where we look. Prehistoric storms eroded 10,000 feet of the top of the Sutter Buttes and filled the Sacramento Valley on the west side three miles deep with alluvial sediments. Among the condominiums of Incline Village they left boulders that could only have been deposited between houses by debris flows. Debris flows generally have the density of newly mixed concrete and move at about the speed of a freight train. Debris flows are a major force in sculpting Earth's land surface. All rainfalls when they hit the ground pick up minerals and modify the landscape. Significant sever storms can be quite localized and of short duration. They often fall between the measurements from our rain gage network and even now might still qualify as prehistoric. Sometimes we can find the sudden peaks in the stream flow records to tell us of their existence; if we are lucky. This is an account of some of the measured storms within the memories of recent California inhabitants. Some of these storms have remarkably large return periods (Map 1). They are not limited to the windward slopes like winter time orographic storms, (Map 2) they occur randomly distributed geographically as well as by season. -
The Sutter Buttes: Attachments to the Land
The Sutter Buttes: Attachments to the Land Antonio E. Valdes Humboldt State University Abstract The Sutter Buttes are an isolated group of lava domes jutting out of California’s flat Central Valley. They are a publicly valued icon, and have been compared to natural wonders such as Crater Lake and Yosemite, but unlike those icons, access into the Buttes is currently limited to authorized individuals and private landowners (Martin 1991). In 2003 the California Department of Parks and Recreation (State Parks) purchased 1,785 acres in the northern portion of the Buttes (CapRadio 2007). However, because the property is surrounded entirely by private land, the park is currently not available for public use (Rogers 2013). As a result, State Parks has offered many of the surrounding landowners exorbitant prices for their properties, with the intention of augmenting these properties to the park. By doing so, the state hopes to eventually border a county road, thus making the park accessible to the public. However, as of yet, no landowners have sold their properties to the state. This research investigates landowners’ sense of place, and, more specifically, reveals that a positive sense of place is a strong factor in- fluencing a number of the landowners’ decisions to retain the titles to their properties. The Sutter Buttes’ prominence above the surrounding plains, their near- ly perfect circular arrangement, and their geologic distinctiveness from other mountain ranges makes them anything but normal. Indeed, the physical features of the so-called “smallest mountain range in the world” are unique, but it is the human decisions surrounding these physical features that have allowed the Buttes to retain their character as an undeveloped rangeland. -
Geochemistry of Ground Water in the 1 Sacramento Valley, California
IQJUN GEOCHEMISTRY OF GROUND WATER IN THE 1 SACRAMENTO VALLEY, CALIFORNIA U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1401-B Geochemistry of Ground Water in the Sacramento Valley, California By LAURENCE C. HULL CENTRAL VALLEY OF CALIFORNIA RASA PROJECT GEOLOGICAL SURVEY PROFESSIONAL PAPER 1401-B UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1984 UNITED STATES DEPARTMENT OF THE INTERIOR WILLIAM P. CLARK, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data Hull, Laurence C. Geochemistry of ground water in the Sacramento Valley, California (Geological Survey Professional Paper 1401-B) (Central Valley of California RASA Project) Bibliography: 36 p. 1. Water, Underground California Sacramento Valley. 2. Water chemistry. I. Title. II. Series. III. Series: Central Valley of California RASA Project. GB1025.C2H781984 551.4'9'097945 84-600016 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Abstract .................. Bl Temporal changes ............... B13 Introduction ................ 1 Methods of data analysis ........ 15 Geography ............... 1 Dissolved solids .............. 15 Purpose and scope .......... 3 Hydrochemical facies ......... 16 Data compilation ............ 3 1 Nitrate ................... 19 Well-numbering system ........ 3 Hydrochemical facies ......... 20 Acknowledgments ........... 3 Hypothesis testing ............ 21 Description of the study area ...... 3 Processes controlling ground-water chemistry 22 Geology and geomorphology ..... 3 Methods of data analysis ........ 22 Geologic synopsis ......... 4 Principal components analysis .... 22 Geomorphic units ......... 4 Trend surface analysis ........ 22 Hydrogeology ............. 6 Processes and their spatial variation . 22 Hydrochemical facies ........... 7 Mineral stability relations ........... 25 Criteria and procedure for division . 7 Mineralogy of sediments ......... 25 Descriptions of hydrochemical facies Well 12N/01E-34Q .......... 25 Tuscan volcanic rocks ..... -
Terrestrial Mammal Species of Special Concern in California, Bolster, BC, Ed., 1998
Terrestrial Mammal Species of Special Concern in California, Bolster, B.C., Ed., 1998 147 Watch List Accounts Salinas ornate shrew, Sorex ornatus salaries Paul W. Collins Museum records of S. o. salarius extend from the vicinity of the mouth of the Pajaro River (Watsonville Slough), Santa Cruz County (Rudd 1948), south along the immediate coast to Carmel (Von Bloeker 1939). This subspecies was originally described as inhabiting coastal salt-marshes and adjacent sandhill areas in the vicinity of Monterey and Carmel bays, Monterey County (Von Bloeker 1938, 1939). According to Williams (1986), it occupies riparian, wetland and upland terrestrial communities in the vicinity of the Salinas River Delta. The capture of 61 ornate shrews near the Salinas River mouth in July 1990 with 700 trap-nights of effort suggests that S. o. salarius may still be common in the area (J. Maldonado pers. comm.). More recent data than these on the distribution and status of this subspecies were not available during the preparation of this document. Although the Salinas ornate shrew has a restricted distribution in a region under pressure from urban and agricultural developments, it occupies a diversity of habitats, and much of the remaining coastal salt marshes within its geographic range are protected from development. Recent surveys indicate it is still common. Rudd (1948) and Junge and Hoffmann (1981) questioned the currently accepted taxonomy of ornate shrews from the vicinity of Monterey Bay. A more extensive range-wide genetic and morphologic evaluation of ornate shrews is currently under way (Maldonado pers. comm.). Results of that study should help to clarify whether ornate shrews from the vicinity of Monterey Bay warrant subspecific recognition. -
David Wyatt • Bats of the Sutter Buttes What Is the Only Mammal That Flies? Yes, You Got It
Volume 54, Number 6 March 2009 David Wyatt • Bats of the Sutter Buttes What is the only mammal that flies? Yes, you got it . they are our bats. Bats are also one of our most misunderstood creatures with many myths and misconceptions sur- rounding them. Whether you love them, hate them, or are simply indifferent to them, join us in discovering the fascinating, some- times bizarre, world of bats. On March 5, The Dusky Warbler, biologist David Wyatt will introduce us to found by Emilie many of the bat species we can find here in Strauss on October 9 California and beyond. Learn that most bats at Point Isabel, was, eat insects and are extremely important in by far, the best bird controlling insect pest numbers. Also dis- on Denise’s 2008 cover how bat biologists study these mam- Contra Costa Big mals and what that information is revealing Year list. about their behavior and life histories. Photo by Bob Lewis Dave Wyatt is currently co-chair of the Biology Department of Sacramento City College. He has taught in community colleges since 993 and has been full time at SCC since 998 teaching various courses in Field Ecology. His primary research interests have revolved around three areas: Ringtails, bats, Sutter Buttes, the world’s smallest mountain range, were known by the Maidu as Esto and insects (primarily beetles, since 987). Yamani–The Middle Mountains–and were regarded as a place for spiritual renewal . His research has been predominantly in Dave is a parent and is currently owned by up close and personal and found it a great California, but has extended to Baja Califor- four beagles that fill his life with howls of pleasure to see Dave with his students. -
Park Lands, Historic Sites, Wildlife and Forest Conservation. Bonds
University of California, Hastings College of the Law UC Hastings Scholarship Repository Initiatives California Ballot Propositions and Initiatives 6-7-1993 Park Lands, Historic Sites, Wildlife And Forest Conservation. Bonds. Follow this and additional works at: http://repository.uchastings.edu/ca_ballot_inits Recommended Citation Park Lands, Historic Sites, Wildlife And Forest Conservation. Bonds. California Initiative 593 (1993). http://repository.uchastings.edu/ca_ballot_inits/756 This Initiative is brought to you for free and open access by the California Ballot Propositions and Initiatives at UC Hastings Scholarship Repository. It has been accepted for inclusion in Initiatives by an authorized administrator of UC Hastings Scholarship Repository. For more information, please contact [email protected]. OFFICE OF THE SECRETARY OF STATE December 9, 1993 TO: All County Clerks/Registrars of Voters (93155) Pursuant to Section 3523 of the Elections Code, I hereby certify that on December 9, 1993 the certificates received from the County Clerks or Registrars of Voters by the Secretary of State established that the Initiative Statute, PARK LANDS, HISTORIC SITES, WILDLIFE AND FOREST CONSERVATION. BONDS has been signed by the requisite number of qualified electors needed to declare the petition sufficient. The PARK LANDS, HISTORIC SITES, WILDLIFE AND FOREST CONSERVATION. BONDS. INITIATIVE STATUTE is, therefore, qualified for the June 7, 1994 Primary Election. PARK LANDS, HISTORIC SITES, WILDLIFE AND FOREST CONSERVA TION. BONDS. INITIATIVE STATUTE. Authorizes general obligation bonds of almost $2 billion, to be repaid from the General Fund, for acquisition, development, rehabilitation, restoration and conservation of park lands, historic sites, wildlife areas and forest throughout California. Includes funds for parks and recreational facilities throughout the State. -
Sacramento Valley Region Report
CALIFORNIA’S FOURTH CLIMATE CHANGE ASSESSMENT Sacramento Valley Region Report Coordinating Agencies: CALIFORNIA’S FOURTH CLIMATE CHANGE ASSESSMENT Introduction to California’s Fourth Climate Change Assessment alifornia is a global leader in using, investing in, and advancing research to set proactive climate change policy, and its Climate Change Assessments provide the scientifc foundation for understanding climate- related vulnerability at the local scale and informing resilience actions. The Climate Change Assessments directly inform State policies, plans, programs, and guidance to promote effective and integrated action to Csafeguard California from climate change. California’s Fourth Climate Change Assessment (Fourth Assessment) advances actionable science that serves the growing needs of state and local-level decision-makers from a variety of sectors. Tis cutting-edge research initiative is comprised of a wide-ranging body of technical reports, including rigorous, comprehensive climate change scenarios at a scale suitable for illuminating regional vulnerabilities and localized adaptation strategies in California; datasets and tools that improve integration of observed and projected knowledge about climate change into decision- making; and recommendations and information to directly inform vulnerability assessments and adaptation strategies for California’s energy sector, water resources and management, oceans and coasts, forests, wildfres, agriculture, biodiversity and habitat, and public health. In addition, these technical reports have been distilled into summary reports and a brochure, allowing the public and decision-makers to easily access relevant fndings from the Fourth Assessment. • A concise summary of the Fourth Assessment’s most important fndings and conclusions. • An in-depth report on how California’s people, built KEY FINDINGS environment, and ecosystems will be impacted by climate change and how we can proactively adapt, based on the Fourth Assessment’s fndings.