A Vegetative Guide to Selected Native Grasses
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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 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. -
Most Impaired" Coral Reef Areas in the State of Hawai'i
Final Report: EPA Grant CD97918401-0 P. L. Jokiel, K S. Rodgers and Eric K. Brown Page 1 Assessment, Mapping and Monitoring of Selected "Most Impaired" Coral Reef Areas in the State of Hawai'i. Paul L. Jokiel Ku'ulei Rodgers and Eric K. Brown Hawaii Coral Reef Assessment and Monitoring Program (CRAMP) Hawai‘i Institute of Marine Biology P.O.Box 1346 Kāne'ohe, HI 96744 Phone: 808 236 7440 e-mail: [email protected] Final Report: EPA Grant CD97918401-0 April 1, 2004. Final Report: EPA Grant CD97918401-0 P. L. Jokiel, K S. Rodgers and Eric K. Brown Page 2 Table of Contents 0.0 Overview of project in relation to main Hawaiian Islands ................................................3 0.1 Introduction...................................................................................................................3 0.2 Overview of coral reefs – Main Hawaiian Islands........................................................4 1.0 Ka¯ne‘ohe Bay .................................................................................................................12 1.1 South Ka¯ne‘ohe Bay Segment ...................................................................................62 1.2 Central Ka¯ne‘ohe Bay Segment..................................................................................86 1.3 North Ka¯ne‘ohe Bay Segment ....................................................................................94 2.0 South Moloka‘i ................................................................................................................96 2.1 Kamalō -
Appendix D Building Descriptions and Climate Zones
Appendix D Building Descriptions and Climate Zones APPENDIX D: Building Descriptions The purpose of the Building Descriptions is to assist the user in selecting an appropriate type of building when using the Air Conditioning estimating tools. The selected building type should be the one that most closely matches the actual project. These summaries provide the user with the inputs for the typical buildings. Minor variations from these inputs will occur based on differences in building vintage and climate zone. The Building Descriptions are referenced from the 2004-2005 Database for Energy Efficiency Resources (DEER) Update Study. It should be noted that the user is required to provide certain inputs for the user’s specific building (e.g. actual conditioned area, city, operating hours, economy cycle, new AC system and new AC system efficiency). The remaining inputs are approximations of the building and are deemed acceptable to the user. If none of the typical building models are determined to be a fair approximation then the user has the option to use the Custom Building approach. The Custom Building option instructs the user how to initiate the Engage Software. The Engage Software is a stand-alone, DOE2 based modeling program. July 16, 2013 D-1 Version 5.0 Prototype Source Activity Area Type Area % Area Simulation Model Notes 1. Assembly DEER Auditorium 33,235 97.8 Thermal Zoning: One zone per activity area. Office 765 2.2 Total 34,000 Model Configuration: Matches 1994 DEER prototype HVAC Systems: The prototype uses Rooftop DX systems, which are changed to Rooftop HP systems for the heat pump efficiency measures. -
4.11 Hydrology General Plan DEIR
4.11 HYDROLOGY AND WATER QUALITY This section discusses and analyzes the surface hydrology, groundwater, and water quality characteristics of the County and the proposed project. This analysis addresses impacts to hydrology and water quality and identifies mitigation measures to lessen those impacts. See Section 4.12 (Public Services and Utilities) for a more detailed discussion regarding water supplies and demand. Specifically, this section provides the following information regarding hydrology and water quality that are evaluated in this DEIR: • Identification of current hydrologic baseline of the County associated with surface water and groundwater conditions that includes identification of key watersheds and associated water features, precipitation, flood conditions, groundwater basins and associated conditions of the basins and water quality (see Section 4.11.1 below and Appendix H). • A description of the current federal, state, regional and County policies, regulations and standards that are associated with the hydrologic conditions of the County (see Section 4.11.2 below). • Identification of significant hydrologic impacts associated with the proposed General Plan Update (see Section 4.11.3 below). The impact analysis makes use of hydrologic modeling to identify the type and degree of potential impacts based on a range of potential vineyard development conditions in the future (see Appendix H) as well as consideration of current Napa County Conservation Regulations (County Code Chapter 18.108) and Best Management Practices (BMPs) that are typically applied to mitigate impacts (see Appendix I). 4.11.1 EXISTING SETTING SURFACE WATER Napa County is located within the Coast Range physiographic province northeast of San Francisco. The County is bordered to the east by California’s Central Valley and to the west by the Coast Ranges. -
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. -
51 SEVEN LAKES BASIN Here's The
Castle Lake and Mount Shasta from near Heart Lake (Photo by John R. Soares) mostly level as you continue, bringing you to Peak, Magee Peak, and numerous other Cascade the spine of Mount Bradley Ridge at 3 miles. A volcanoes lead to Mount Shasta, with Mount Eddy 0.2-mile scamper northeast (left) brings you to a to the west of the largest California volcano. knob with the best views. If you want more hiking, continue farther Look south at the immediate prospect of serrated toward Mount Bradley or hike the 0.5 mile path granite crests of Castle Crags. Eastward Lassen that skirts the east side of Castle Lake. SEVEN LAKES BASIN 51 Length: 6 miles round-trip Hiking time: 5 hours or 2 days High point: 6,825 feet Total elevation gain: 1,400 feet Difficulty: moderate Season: early June through late October Water: available only at Seven Lakes Basin (purify first); bring your own Maps: USGS 7.5’ Mumbo Basin, USGS 7.5’ Seven Lakes Basin Information: Mount Shasta Ranger Station, Shasta–Trinity National Forest 122 Seven Lakes Basin • 123 6850' One-way spires of the Trinity Alps to the west, with for- 6800' 6750' ested mountains filling in the northerly and 6700' southerly views. 6650' Travel south, undulating gently along the 6600' 6550' spine of the ridge, occasionally shaded by a Jef- 6500' frey pine, western white pine, red fir, or white fir. 6450' 6400' Note the various flowers, including blue lupines 6350' and yellow sulfur flowers. 6300' 6250' The first decent campsite appears on the left at 6200' 0.3 mile, followed by the inaugural view of Mount 0 mile 1.5 3.0 Shasta, with Mount Eddy and Gumboot Lake com- ThisHike 51. -
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. -
Geology, Soils, and Seismicity
City of American Canyon ‐ Napa Airport Corporate Center Project Draft EIR Geology, Soils, and Seismicity 3.5 ‐ Geology, Soils, and Seismicity 3.5.1 ‐ Introduction This section describes the existing geology, soils, and seismicity setting and potential effects from project implementation on the site and its surrounding area. Descriptions and analysis in this section are based on the Geotechnical Investigations prepared by Raney Geotechnical, Inc. and included in this EIR as Appendix E. 3.5.2 ‐ Environmental Setting Regional Geology Napa County is located within the California Coast Range geomorphic province. This province is a geologically complex and seismically active region characterized by sub‐parallel northwest‐trending faults, mountain ranges, and valleys. The oldest bedrock units are the Jurassic‐Crustaceous Franciscan Complex and Great Valley sequence sediments originally deposited in a marine environment. Subsequently, younger rocks such as the Tertiary‐period Sonoma Volcanics group, the Plio‐Pleistocene‐age Clear Lake Volcanics, and sedimentary rocks such as the Guinda, Domengine, Petaluma, Wilson Grove, Cache, Huichica, and Glen Ellen formations were deposited throughout the province. Extensive folding and thrust faulting during the late Crustaceous through early Tertiary geologic time created complex geologic conditions that underlie the highly varied topography of today. In valleys, the bedrock is covered by thick alluvial soils. The project site is located within the southern portion of the Napa Valley, which consists of a large northwest‐trending alluvial plain flanked by the Mayacama Mountains the west and the Howell Mountains to the east. The West Napa Fault is located within the southern portion of the Napa Valley and the Concord‐Green Valley Fault is located near the Howell Mountains along the east side of the valley. -
Napa Valley Preferred Wine Country DAY TRIPS X
NVdaytrips-0413_Layout 1 4/25/13 9:55 AM Page 1 Spring/Summer 2013 Napa Valley Preferred Wine Country DAY TRIPS x x x x FuN x FACT x NINE TRIpS WINE TASTING from Calistoga to Carneros A publication of FORTY-SEVEN9 TASTING ROOM REVIEWS Dining Directory1 47 plusand Varietals Chart NVdaytrips-0413_Layout 1 4/25/13 9:55 AM Page 2 TO CLEAR LAKE Lake E TT LAN ENNE B RD Berryessa Old Faithful ANYON TS C SUMMERS Geyser 29 BUT LANE BBS TO GEYSERVILLE ESTATE TU ALEXANDER VALLEY CALISTOGA Pre 128 LN PAGES 12>15 O NC CALISTOGA LI BALLOONS POPE VALLEY TO L A SUMMIT WINERY E SANTA ROSA W SUM A M STERLING LAKE IT LA DUN K E E G DR A VINEYARDS T T O C E T I D H W MEA POPE VALLEY ARK H L BRAVANTE OWEL L FRANK MTN E CASTELLO AN FAMILY L VIADER LE DI AMOROSA BA BURGESS CRYS TAL On & Around SPR IN G M S IU R A IT N A S HOWELL MTN RK PA R EE LODI D D9 Win PAGES 16>21 BALLENTINE HO ARK EER P W D EL ST. CLEMENT L MT N SI LEY ROS VAL CONN 29 SP RING MTN T MTN AT LL PR HOWE ST BERINGER E POP A ON MADR MERRYVALE SAGE CANYON VINEYARDS K HILL WINE CO. R OA NEWTON CHARTE VINEYARDS LOUIS M. PAGES 34>37 MARTINI RUTHERFORD ORD RF HI RUSTRIDGE E LL HILL ST. HELENA . H LN T L U D R V.