California Coast Viticultural Area

Total Page:16

File Type:pdf, Size:1020Kb

California Coast Viticultural Area Federal Register / Vol. 65, No. 187 / Tuesday, September 26, 2000 / Proposed Rules 57763 notice of transferee liability to U at any time corporation for a separate return year ACTION: Notice of proposed rulemaking. on or before May 30 of Year 8 and assess the pursuant to § 1.1502±21(b), 1.1502± unpaid liability against U at any time on or 22(b), or 1.1502±79(c). In the case of the SUMMARY: The Bureau of Alcohol, before October 27 of Year 8. The result would portion of a consolidated net operating Tobacco and Firearms (ATF) has be the same even if S±1 ceased to exist before loss or consolidated net capital loss or received a petition proposing the March 1 of Year 5, the date P executed the establishment of a viticultural area waiver. consolidated unused business credit to which the preceding sentence does not located along the coast of California. (g) Cross-reference. For further rules apply and which is to be carried back The proposed California Coast applicable to groups that include to a corporation that was not a member viticultural area would consist of 22,000 insolvent financial institutions, see of a consolidated group in the carryback square miles, or 14 million acres of that § 301.6402±7 of this chapter. year, the corporation to which such loss land which the petitioner states is (h) Effective dateÐ(1) Application. or credit is attributable shall make any subject to maritime influences and This section applies with respect to application under section 6411. In the which is warm enough for commercial taxable years beginning on or after the case of a net capital loss or net operating premium winegrape growth. date final regulations are published in loss or unused business credit arising in DATES: Written comments must be the Federal Register. a separate return year which may be received by December 26, 2000. (2) Prior law. For taxable years carried back to a consolidated return ADDRESSES: Send written comments to: beginning before the date final year, after taking into account the Chief, Regulations Division, Bureau of regulations are published in the Federal application of § 1.1502±21(b)(3)(ii)(B) Alcohol, Tobacco and Firearms, P.O. Register, see § 1.1502±77A. with respect to any net operating loss Box 50221, Washington, DC 20091±0221 Par. 6. Section 1.1502±77T(a) is arising in another consolidated group, (Attn: Notice No. 903). Copies of the redesignated as § 1.1502±77A(e) and the common parent for the carryback petition, the proposed regulations, the § 1.1502±77T is removed. year (or agent designated under appropriate maps, and any written Par. 7. The amendments to § 1.1502± § 1.1502±77(d) for the carryback year) comments received will be available for 78(a), as contained in the notice of shall make any application under public inspection during normal proposed rulemaking (LR±97±79) section 6411. business hours at ATF Reading Room, published in the Federal Register on * * * * * Office of Public Affairs and Disclosure, July 31, 1984 (49 FR 30528), are (e) Cross-reference. For further rules Room 6480, 650 Massachusetts Avenue, withdrawn. applicable to groups that include NW, Washington, DC 20226 Par. 8. Section 1.1502±78 is amended insolvent financial institutions, see FOR FURTHER INFORMATION CONTACT: Tom as follows: § 301.6402±7 of this chapter. Busey, Regulations Division, Bureau of 1. Paragraph (a) is revised. (f) Effective dateÐ(1) In general. This Alcohol, Tobacco and Firearms, 650 2. Paragraph (b)(1) is amended by section applies to taxable years to which Massachusetts Avenue, NW, adding the language ``for the carryback a loss or credit may be carried back and Washington, DC 20226 (202) 927±8095. year (or agent designated under for which the due date (without SUPPLEMENTARY INFORMATION: § 1.1502±77(d) for the carryback year)'' extensions) of the original return is after Background at the end of the first sentence. the date final regulations are published 3. In paragraph (c), the last sentence in the Federal Register. On August 23, 1978, ATF published of Example (1) is amended by adding (2) Prior law. For taxable years to Treasury Decision ATF±53 (43 FR the language ``for the carryback year'' which a loss or credit may be carried 37672, 54624) revising regulations in 27 after ``parent.'' back and for which the due date CFR part 4. These regulations allow the 4. In paragraph (c), the last sentence (without extensions) is on or before the establishment of definitive viticultural of Example (2) is amended by removing date final regulations are published in areas. The regulations allow the name of the language ``S±1'' and adding ``P'' in the Federal Register, see § 1.1502±78 in an approved viticultural area to be used its place. effect prior to the date final regulations as an appellation of origin on wine 5. In paragraph (c), Example (3), the are published in the Federal Register, as labels and in wine advertisements. On seventh sentence is amended by contained in 26 CFR part 1 revised as of October 2, 1979, ATF published removing ``Z must'' and adding ``X April 1, 2000. Treasury Decision ATF±60 (44 FR must'' in its place. 56692) which added a new part 9 to 6. Paragraphs (e) and (f) are added. Robert E. Wenzel, Title 27, CFR, for the listing of approved The revision and additions read as Deputy Commissioner of Internal Revenue. American viticultural areas, the names follows: [FR Doc. 00±24039 Filed 9±25±00; 8:45 am] of which may be used as appellations of BILLING CODE 4830±01±P origin. § 1.1502±78 Tentative carryback Section 4.25a(e)(1), title 27, CFR, adjustments. defines an American viticultural area as (a) General rule. If a group has a DEPARTMENT OF THE TREASURY a delimited grape-growing region consolidated net operating loss, a distinguishable by geographic features, consolidated net capital loss, or a Bureau of Alcohol, Tobacco and the boundaries of which have been consolidated unused business credit for Firearms delineated in subpart C of part 9. any taxable year, then any application Section 4.25a(e)(2) outlines the under section 6411 for a tentative 27 CFR Part 9 procedure for proposing an American carryback adjustment of the taxes for a [Notice No. 903] viticultural area. Any interested person consolidated return year or years may petition ATF to establish a grape- preceding such year shall be made by RIN 1512±AA07 growing region as a viticultural area. the common parent corporation for the California Coast Viticultural Area The petition should include: carryback year (or agent designated (2000R±166P) (a) Evidence that the name of the under § 1.1502±77(d) for the carryback proposed viticultural area is locally year) to the extent such loss or unused AGENCY: Bureau of Alcohol, Tobacco and/or nationally known as referring to business credit is not apportioned to a and Firearms (ATF), Treasury. the area specified in the petition; VerDate 11<MAY>2000 17:43 Sep 25, 2000 Jkt 190000 PO 00000 Frm 00016 Fmt 4702 Sfmt 4702 E:\FR\FM\26SEP1.SGM pfrm03 PsN: 26SEP1 57764 Federal Register / Vol. 65, No. 187 / Tuesday, September 26, 2000 / Proposed Rules (b) Historical or current evidence that the consumer. ATF is looking for early production of wines in these the boundaries of the viticultural area specific comments on this situation and missions which extended along the are as specified in the petition; how the approval of this viticultural California Coast and fall within the (c) Evidence relating to the area should effect the future use of the boundaries of this AVA (see historical geographical characteristics (climate, term ``Coastal.'' discussions by wine experts in The soil, elevation, physical features, etc.) Wine Regions of America, by John J. which distinguish the viticultural Evidence That the Name of the Area Is Locally or Nationally Known Baxevanis (Vinifera Wine Journal 1992) features of the proposed area from at 257±8; Winemaking in California, by surrounding areas; According to the petitioners, the Teiser and Harroun (McGraw-Hill 1983) (d) A description of the specific name, ``California Coast'' is universally at 1±3; General Viticulture, by A.J. boundaries of the viticultural area, recognized. The petitioners point out Winkler at 2±4; The World Atlas of based on features which can be found that on a map of California, the state Wine, by Hugh Johnson at 226; and on United States Geological Survey has, on the western edge, one long Wine, by Amerine and Singleton (U.C. (U.S.G.S.) maps of the largest applicable rugged coastline next to a relatively Press 1977) at 281±3.) In addition, the scale; and narrow area of flatter land, which is petitioners seek to coordinate the (e) A copy (or copies) of the itself bordered, on the east, by a long, proposed ``California Coast'' viticultural appropriate U.S.G.S. map(s) with the nearly continuous string of mountains area with the existing boundaries of the boundaries prominently marked. known as the Coast Ranges. The other current North, Central, South, and side of the Coast Ranges is accompanied Petition Sonoma Coast viticultural areas in by a long, north-south, interior strip of The Bureau of Alcohol, Tobacco and California along with the previously continental mass distinguished by the unconnected coastal areas which link Firearms (ATF) has received a petition hot Central Valley and, east of that from the ``California Coast Alliance'' the existing ``Coast'' viticultural areas. basin, the high peaks of the Sierra According to the petitioners, the proposing the establishment of a Nevada Range. The petitioners cite viticultural area located along the coast northern, southern, and eastern numerous books referring to ``the boundaries set by these ``Coast'' of California.
Recommended publications
  • Chapter 5: Parks, Recreation, and Open Space
    5 Parks, Recreation, and Open Space This chapter is a guide to the parks, recreation and open space resources in Humboldt County. Humboldt is home to recreational, park, and open space resources of statewide, nationwide, and even global significance. With this in mind, the first two sections describe these resources, while the final section addresses existing policies and policy issues identified during Phase I along with policy options that respond to them. 5.1 PARK AND RECREATION FACILITIES Humboldt County has a wealth of outdoor recreational opportunities and areas of incomparable value and unsurpassed beauty. More than twenty percent of the county’s 2.3 million acres are protected open space, forests, and recreation areas. Within the county boundaries, there are 4 federal parks and beaches, 10 state parks (3 of which are encompassed by Redwood National Park), 16 county parks and beaches, recreational areas and reserves, and National Parkland and National Forest land. These areas contribute to the quality of life in Humboldt County and provide needed recreation opportunities for residents of neighboring counties and from all over the world as well. Parklands are important elements of the Humboldt economy through both their role in the timber industry and the tourist industry. As tourism eclipses timber as the stronghold of Humboldt’s economy, parks and recreational resources will prove of greater and greater value to Humboldt’s future. The natural qualities of Humboldt County attract a great many people from outside the county. The tourist industry and demand for park resources in Humboldt are linked to the accessibility of parkland.
    [Show full text]
  • 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).
    [Show full text]
  • 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.
    [Show full text]
  • Bigbig Sursur
    CalCal PolyPoly -- PomonaPomona GeologyGeology ClubClub SpringSpring 20032003 FFieldield TTriprip BigBig SurSur David R. Jessey Randal E. Burns Leianna L. Michalka Danielle M. Wall ACKNOWLEDGEMENT The authors of this field guide would like to express their appreciation and sincere thanks to the Peninsula Geologic Society, the California Geological Survey and Caltrans. Without their excellent publications this guide would not have been possible. We apologize for any errors made through exclusion or addition of trip field stops. For more detailed descriptions please see the following: Zatkin, Robert (ed.), 2000, Salinia/Nacimiento Amalgamated Terrane Big Sur Coast, Central California, Peninsula Geological Society Spring Field Trip 2000 Guidebook, 214 p. Wills, C.J., Manson, M.W., Brown, K.D., Davenport, C.W. and Domrose, C.J., 2001, LANDSLIDES IN THE HIGHWAY 1 CORRIDOR: GEOLOGY AND SLOPE STABILITY ALONG THE BIG SUR COAST, California Department of Conservation Division of Mines & Geology, 43 p. 0 122 0 00' 122 0 45' 121 30 Qal Peninsula Geological Society Qal G a b i Qt la Field Trip to Salina/Nacimento 1 n R S a A n L Big Sur Coast, Central California I g N qd A e S R Qt IV E Salinas R S a lin a s Qs V Qal 101 a Qs Monterey Qc lle Qt Qp y pgm Tm Qm Seaside pgm EXPLANATION Qt Chualar Qp Qt UNCONSOLIDATED Tm pgm SEDIMENTS Qp Carmel Qal sur Qs Qal Alluvium qd CARMEL RIVER Tm Qal Point sur Qs Dune Sand Tm Lobos pgm 0 S 0 36 30 ie ' r 36 30' pgm ra Qt Quaternary non-marine d CARMEL e S terrace deposits VALLEY a Qal lin a Qt Pleistocene non-marine Tm pgm s Qc 1 Tm Tula qd rcit Qp Plio-Pleistocene non-marine qd os F ault Qm Pleistocene marine Terrace sur sur deposits qd Tm COVER ROCKS pgm qd Tm Monterey Formation, mostly qm pgm qm pgm marine biogenic and sur pgm clastic sediments middle to qdp sur qd late Miocene in age.
    [Show full text]
  • Development and Implications of a Sediment Budget for the Upper Elk River Watershed, Humboldt County1
    Proceedings of the Coast Redwood Science Symposium—2016 Development and Implications of a Sediment Budget for the Upper Elk River Watershed, Humboldt County1 2 3 3 3 Lee H. MacDonald, Michael W. Miles, Shane Beach, Nicolas M. Harrison, 4 5 6 Matthew R. House, Patrick Belmont, and Ken L. Ferrier Abstract A number of watersheds on the North Coast of California have been designated as sediment impaired under the Clean Water Act, including the 112 km2 upper Elk River watershed that flows into Humboldt Bay just south of Eureka. The objectives of this paper are to: 1) briefly explain the geomorphic context and anthropogenic uses of the Elk River watershed; 2) develop a process-based sediment budget for the upper watershed, including an explicit assessment of the uncertainties in each component; and 3) use the results to help guide future management and restoration. Natural (background) sediment inputs are believed to be relatively high due to high uplift rates, weak Miocene-Pliocene bedrock materials, steep slopes, high rainfall, and resulting high landslide frequency. The primary land use in the upper watershed is industrial timberlands, and intensive logging in the 1980s and 1990s greatly increased sediment production rates and downstream aggradation. Road improvements and major changes in forest practices have caused anthropogenic sediment inputs to drop by roughly an order of magnitude since the 1990s. Suspended sediment yields plotted against annual maximum peak flows indicate a decline since 2013, suggesting that the legacy pulse of sediment is now moving into the lower portions of the watershed and that improved management practices are having a beneficial effect.
    [Show full text]
  • Living with Fire in California's Coast Ranges
    SYMPOSIUM PROGRAM LIVING WITH FIRE IN CALIFORNIA’S COAST RANGES Promoting Fire-Resilient Communities and Landscapes in an Era of Global Change PHOTO CREDITS FROM LEFT TO RIGHT 1. COFFEY PARK, TUBBS FIRE - JOHN BURGESS 2. NUNS FIRE - KENT PORTER 3. POCKET FIRE - KENT PORTER MONDAY MAY 7 Setting the stage: Fire ecology and fire history of the Central and North Coast Ranges 08:30-08:50 1. Welcome, introduction, Sonoma State University welcome Hugh Safford, US Forest Service Pacific and agenda SW Region, Lenya Quinn-Davidson, UC-Cooperative Extension, and Lisa Vollendorf, SSU Provost 08:50-09:10 2. Fire ecology basics: a primer for northern California Lenya Quinn-Davidson, UC- communities Cooperative Extension 09:10-09:45 3. Fire ecology of the central and north Coast Ranges of Scott Stephens, UC-Berkeley California 09:45-10:15 4. Modern era fire history in the Central Coast Region: What Marshall Turbeville, CAL FIRE, the past can tell us about the future Sonoma-Lake-Napa Unit 10:15-10:35 Discussion 10:35-10:55 Break (coffee and tea provided) Understanding the Wine Country Fires 10:55-11:40 5. Fall 2017 Sonoma Fires: An operational perspective on Greg Bertelli, CAL FIRE, Sonoma-Lake- emergency response, tactics, and the modern Urban-Interface Napa Unit fire problem 11:40-12:10 Discussion 12:10-13:40 Lunch (Provided) Understanding the Wine Country Fires (cont) 13:40-14:10 6. Meteorology and weather associated with extreme wildfire Craig Clements, San Jose State in Coastal California University 14:10-14:40 7. Nexus between climate, weather and ignition sources: Jon Keeley, US Geological Survey Regional patterns in California 14:40-15:00 Discussion 15:00-15:20 Break Fire and humans 15:20-15:50 8.
    [Show full text]
  • Chronology of Emplacement of Mesozoic Batholithic Complexes in California and Western Nevada by J
    Chronology of Emplacement of Mesozoic Batholithic Complexes In California and Western Nevada By J. F. EVERNDEN and R. W. KISTLER GEOLOGICAL SURVEY PROFESSIONAL PAPER 623 Prepared in cooperation with the University of California (Berkeley) Department of Geological Sciences UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1970 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Con;gress CSJtalog-card No. 7s-.60.38'60 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price $1.25 (paper cover) CONTENTS Page Abstract-------------------------------~---------------------------------------------------------------------- 1 Introduction--------------------------------------------------------------------------------~----------------- 1 Analyt:cal problems ____________________ -._______________________________________________________________________ 2 Analytical procedures______________________________________________________________________________________ 2 Precision and accuracy ___________________ -.- __ _ _ _ _ __ _ _ _ __ _ _ _ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 2 Potassium determinations_______________________________________________________________________________ · 2 Argon determinations--------~------------------~------------------------------------------------------ 5 Chemical and crystallographic effects on potassium-argon ages----------.-----------------------------------------
    [Show full text]
  • Late Neogene and Quaternary Landscape Evolution of the Northern California Coast Ranges: Evidence for Mendocino Triple Junction Tectonics
    Late Neogene and Quaternary landscape evolution of the northern California Coast Ranges: Evidence for Mendocino triple junction tectonics Jane Lock† Department of Geosciences, Pennsylvania State University, University Park, Pennsylvania 16802, USA Harvey Kelsey‡ Department of Geology, Humboldt State University, Arcata, California 95521, USA Kevin Furlong§ Department of Geosciences, Pennsylvania State University, University Park, Pennsylvania 16802, USA Adam Woolace# Department of Geology, Humboldt State University, Arcata, California 95521, USA ABSTRACT the double-humped pattern of uplift and our understanding of the lithospheric forces subsidence migrates, and the Coast Ranges that have built the orogen, and recognizing the A landscape records the surface response emerge. Smaller drainages develop and tectonic signal recorded by the landscape. We to tectonics at time scales intermedi- evolve by stream capture and fl ow reversal, describe how the surface responds to tectonics ate between short time-scale information and the two main divides migrate in concert in northern California, and we use the tectonic derived from seismic imaging and global with the triple junction. In contrast to the signal contained in the landscape to test and positioning systems and the long-term geo- systematic development of the small streams, develop our understanding of the geodynamics. logic record. We link late Neogene and the largest trunk streams can maintain grade A variety of mechanisms has been proposed Quaternary deposits and landforms in the through regions of high uplift, and coastal to explain the timing of uplift of the northern northern California Coast Ranges to the tec- river mouths remain stationary despite the California Coast Ranges. Dumitru (1989), using tonics of the Mendocino triple junction.
    [Show full text]
  • Geologic Map and Map Database of Western Sonoma, Northernmost Marin, and Southernmost Mendocino Counties, California
    Geologic Map and Map Database of Western Sonoma, Northernmost Marin, and Southernmost Mendocino Counties, California By M.C. Blake, Jr., R.W. Graymer, and R.E. Stamski Pamphlet to accompany MISCELLANEOUS FIELD STUDIES MAP MF-2402 Version 1.0 2002 U.S. Department of the Interior U.S. Geological Survey Contents Geologic explanation and acknowledgements 1 Introduction 1 Stratigraphy 1 Mesozoic and Tertiary terrane complexes 1 Description of Terranes 2 Tertiary Stratigraphy 10 Quaternary Surficial Deposits 11 Paleontology 11 Radiometric Ages 11 Structure 12 Structural History 12 Description of Map Units 15 Acknowledgements 23 Digital publication and database description 24 Introduction 24 For those who don’t use digital geologic map databases 24 MF-2402 Digital Contents 24 PostScript plotfile package 25 PDF plotfile package 25 Digital database package 25 TAR files 26 PostScript plotfiles 27 PDF plotfiles 27 Obtaining the Digital Database and Plotfile Packages 28 To obtain TAR files of database or plotfile packages from the USGS web pages 28 To obtain TAR files of database or plotfile packages by ftp 28 Obtaining plots from a commercial vendor 28 Obtaining plots from USGS Map On Demand Services 28 Revisions and version numbers 28 Digital database format 29 Converting ARC export files 29 Digital compilation 29 Base maps 29 Faults and landslides 29 Spatial resolution 29 Database specifics 30 Lines 30 Areas 32 Points 33 References Cited 35 ii Geologic Explanation and Acknowledgements Introduction The map in this report is modified from and supercedes USGS Open-File Report 71-44 (Blake and This report contains a new geologic map at 1:100,000 others, 1971).
    [Show full text]
  • Geology of the Cape Mendocino, Eureka, Garberville, and Southwestern Part of the Hayfork 30 X 60 Minute Quadrangles and Adjacent Offshore Area, Northern California
    Geology of the Cape Mendocino, Eureka, Garberville, and Southwestern part of the Hayfork 30 x 60 Minute Quadrangles and Adjacent Offshore Area, Northern California By R.J. McLaughlin1, S.D. Ellen1, M.C. Blake, Jr.2, A.S. Jayko1, W.P. Irwin1, K.R. Aalto3, G.A. Carver3, and S.H. Clarke, Jr.1 Pamphlet to accompany Miscellaneous Field Studies MF-2336 Version 1.0 Digital Database by J.B. Barnes1, J.D. Cecil1 and K.A. Cyr 1 1U.S. Geological Survey, 345 Middlefield Rd., Menlo Park, CA 94025 2U.S. Geological Survey, 1911 Wilson Ave., Belllingham, WA 98225 3Humboldt State University, Arcata, CA 95521 2000 U.S. Department of the Interior U.S. Geological Survey i CONTENTS INTRODUCTION 1 PURPOSE 1 FUNDING BACKGROUND 1 ACKNOWLEDGEMENTS 1 PREVIOUS WORK 2 METHODS 2 PHOTOINTERPRETIVE MAPPING 2 GEOLOGIC AND STRUCTURAL OVERVIEW 3 KLAMATH MOUNTAINS PROVINCE 3 COAST RANGES PROVINCE 4 Outliers of Great Valley Sequence and Coast Range Ophiolite 5 Franciscan Complex 5 Eastern belt 5 Pickett Peak terrane 5 Yolla Bolly terrane 6 Central belt 6 Coastal belt 7 Yager terrane 7 Coastal terrane 8 King Range terrane 9 False Cape terrane 10 Oligocene intrusive rocks 11 Late Cenozoic post-accretionary Overlap Assemblage 11 Wildcat Group 11 Bear River beds of Haller (1980) 12 Post-accretionary Neogene strata in the Cape Mendocino to Petrolia area 12 Unnamed upper Pleistocene and Holocene deposits 13 STRUCTURAL RELATIONS 13 Faults bounding belts of the Franciscan Complex 13 South Fork fault 13 Coast Range fault 13 Grogan-Red Mountain fault zone 14 Mule Ridge fault zone
    [Show full text]
  • Gold Bearing Mercury Deposits of the Coast Ranges of California
    TERTIARY GOLD BEARING MERCURY DEPOSITS OF THE COAST RANGES OF CALIFORNIA By LARRY M . VREDENBURGH. Geologist Bureau of Land Management Sacramento. California INTRODUCTION bon dioxide (CO,), silica (SiO,), and con­ cury deposits of the Pacific Coast was that taining abundant hydrocarbons, dissolved of Becker (1888). He determined the Recently an unsuspected reserve of the gold and mercury contained in the presence of gold at mercury mines at Wil­ gold, estimated to exceed 3.2 million sedimentary units. At the surface, hydr~ bur Hot Springs, Sulphur Bank Hot ounces, was discovered by Homestake carbons may have played an important Springs, and the Knoxville mine area. He Mining Company at the Knoxville mer­ role in the deposition of the gold, in a also reported the occurrence of gold at the cury mines in Napa County. This is one of manner similar to the Carlin-type depos­ Picacho Mine, located southwest of New several occurrences of gold associated its of Nevada, which closely resemble the ldria. Other worker8 (Crutchfield, 1953; with mercury or antimony in the Coast gold deposits of the Coast Ranges. Mer­ Newmont Exploration, 1965; Bailey and Ranges of California (figure 1) . These cury is presently being deposited by hot Meyers, 1949) have identified gold at the deposits began forming shortly after the springs at the Sulphur Bank mine near Calistoga and Oat Hill mines, and the implacement of volcanic rocks in the Mid­ The Geysers steam field in the Clear Lake Stayton District (table 1) . Tertiary Period and continued to form area of California . through Quaternary time. Connate water GEOLOGY squeezed from sedimentary units was PREVIOUS STUDIES heated and eventually found its way to the The major rock types found in the surface via fracture zones.
    [Show full text]
  • Loca: the Wines of Lodi, California Press Kit 2016
    LoCA: The Wines of Lodi, California Press Kit 2016 1 LODI WINE COUNTRY Ø Lodi—the Place: “Lodi Wine Country” is one of California’s major winegrowing regions, located 100 miles east of San Francisco near the San Joaquin/Sacramento River Delta, south of Sacramento and west of the Sierra Nevada mountain range. It is named after the most populous city within the region. Lodi is characterized by a rural atmosphere where wineries and farms run by 4th - and 5th generation families operate in tandem with a new group of vintners who have brought creative winemaking and cutting-edge technology to the region. In Lodi, grape-growing is inextricably woven into the culture: the city of Lodi’s police department prominently features a grape cluster in its logo, and high school teams are named after grape varieties. Ø A Track Record of Continuous Success: Lodi has been a major winegrape growing region for over 150 years. Unlike many U.S. wine regions, Lodi actually prospered during Prohibition and as such has been a continuous source of wine grapes since the 1850s. In fact, when early trappers wandered into what is now Lodi, they called one stream they discovered "Wine Creek" because of the proliferation of wild vines found there. As more and more Italian and German immigrants made their homes in Lodi, vinifera varieties such as Zinfandel, Tokay, and Alicante appeared by the 1880s. Ø Key Milestones In Lodi’s History: o Fruit supply routes to the East Coast had been well established and so home winemakers took advantage of the provisions of the Volstead Act during Prohibition by purchasing wine grapes from Lodi to make their legal allotment of wine.
    [Show full text]