Mines and Mineral Resources of Monterey County, California

Total Page:16

File Type:pdf, Size:1020Kb

Mines and Mineral Resources of Monterey County, California MINES AND MINERAL RESOURCES OF MONTEREY COUNTY, CALIFORNIA COUNTY REPORT 5 CALIFORNIA DIVISION OF MINES AND GEOLOGY LIBRAE? UNIVERSITY OF CALIFORNIA DAVIS UNIVERSITY OF CALIFORNIA DAVIS JUL 6 1967 GOV'T. DOCS. - LIBRARY Digitized by the Internet Archive in 2012 with funding from University of California, Davis Libraries http://www.archive.org/details/minesandmineral05hart MINES AND MINERAL RESOURCES OF MONTEREY COUNTY, CALIFORNIA BY EARL W. HART California Division of Mines and Geology COUNTY REPORT 5 California Division of Mines and Geology 1966 LIBRARY UNIVERSITY OF CALIFORNIA DAVIS OF STATE OF CALIFORNIA EDMUND G. BROWN, Governor THE RESOURCES AGENCY HUGO FISHER, Administrator DEPARTMENT OF CONSERVATION IAN CAMPBELL, Director DIVISION OF MINES AND GEOLOGY IAN CAMPBELL, State Geologist COUNTY REPORT 5 Price $5.00 \W Q^M 3^/for^\td 1 CONTENTS Page ABSTRACT 5 Limestone and dolomite Gabilan Range Santa Lucia Range jl INTRODUCTION 7 San Andreas fault zone 67 Purpose and scope 7 Magnesite and magnesium compounds __ 69 Method of investigation _ 7 Manganese 70 Geography ._ _ 7 Mercury 7 History of mining and mineral utilization 11 Mineral water 74 Molybdenum 74 GEOLOGY ...... 12 Olivine 74 Rock units and associated mineral deposits 13 Peat 74 Structural features 21 Petroleum and natural gas 75 Phosphates ____ _ 80 Salt __ _____ 81 MINES AND MINERAL DEPOSITS.. ...... 22 Sand and Gravel 84 Arsenic 26 Quaternary beach and dune deposits 84 Asbestos 26 Quaternary stream deposits 98 Barite 28 Older formations ____ ___ __._ ____ .... 1 05 Bituminous sandstone 29 Silver 107 Chromite _ 31 Stone - 1 08 Clay 32 Crushed and broken stone 109 Coal __ 33 Dimension stone 110 Copper _ 36 Tungsten 113 Diatomite 36 Uranium and thorium 114 Feldspar 41 Gem stones _. 43 BIBLIOGRAPHY 115 Gold __ 44 Lead.... 52 TABULATION OF MINERAL DEPOSITS 119 [3] 1 ILLUSTRATIONS Page Page Plate 1. Geologic map of Monterey County showing mines Photo 11. View northeast across Peach Tree Valley toward Mus- and mineral deposits In Pocket tang Ridge 20 Plate 2. Map of underground workings— Stone Canyon coal Photo 12. Looking east from Presidio of Monterey across south- mine _ In Pocket ern Monterey Bay 20 Table 1. Summary of economic geology of Monterey County. 14 Photo 13. View northeast from Chews Ridge toward Sierra de Table 2. Mineral production of Monterey County, 1889-1964 __. 23 Salinas 22 Table 3. Oil and uranium contents of several bituminous sand- Photo 14. White dumps from barite workings on Rocky Ridge stone deposits in Monterey County 30 near Fremont Peak 27 Table 4. Chemical analyses of carbonate rock samples from Pico Photo 15. Closeup of white crystalline barite veins cutting gray Blanco deposit 65 dolomitic limestone west of Fremont Peak 28 Table 5. Production and disposition of oil, gas and water at San Photo 16. View of hills formed in diatomaceous rocks of the Ardo oil field 79 Monterey Formation north of Homes Valley 38 Photo 17. Old adit at Riewerts diatomite Table 6. Chemical and screen analyses of Moss Beach "flint" deposit 38 sand produced by Owens-Illinois 99 Photo 18. Thin chert interbeds in diatomite of the Monterey For- mation south of Valley Table 7. Summary of geology and development of important Hames 39 Quaternary stream deposits, Monterey County 101 Photo 19. Detail of banded sequence of limestone and dolomite at Fremont Peak Table 8. Geologic formations in Monterey County containing po- 54 tentially useful sources of stone products 108 Photo 20. Aerial view of Natividad dolomite quarry and plant of Kaiser Aluminum and Chemical Corporation 56 Photo 21. Rotary kilns at Natividad calcining plant of Kaiser Figure 1. Index map showing the principal geographic features Aluminum and Chemical Corporation 56 of Monterey County 8 Photo 22. Carbonate rock outcrops at Limekiln Creek 62 Figure 2. Bar diagram showing mineral production of Monterey Photo 23. Aerial view of Moss Landing magnesia plant of Kaiser County, 1 940-1 964 22 Aluminum and Chemical Corporation _ 67 Figure 3. Map— Burro Mountain asbestos prospect 27 Photo 24. Night view of Moss Landing magnesia plant 69 Figure 4. Geologic map of Fremont Peak area showing loca- Photo 25. Rotary kiln used to produce periclase at Moss Landing tions of barite workings 28 plant of Kaiser Aluminum and Chemical Corporation 69 Figure 5. Geologic map— Homes Valley diatomite 37 Photo 26. Hydraulic press used to form basic refractory brick at Figure 6. Geologic map— Diatomite west of King City 42 Kaiser Aluminum and Chemical Corporation's Moss Landing plant .. 71 Figure 7. Map— Patented claims of Buclimo gold mine 47 Photo 27. View of Recent beach and dune sands between mouth Figure 8. Schematic vertical sections of Buclimo gold mine 48 of Little Sur River and Point Sur 83 Figure 9. Map— Plaskett gold mine showing location of claims Photo 28. Dredging of modern beach sand on southern shore of and main workings _ 50 Monterey Bay 85 Figure 10. Limestone and dolomite districts in the northern Gabi- sand plant City lan Range 53 Photo 29. Granite Construction Company at Sand 86 Monterey sand plant Figure 11. Flowsheet of the Natividad dolomite quarry and Photo 30. Sand dunes and Sand Company's plant 58 at Marina, Monterey Bay 87 Pacific and Aggregates' Figure 12. Geologic map and sections of the Pico Blanco lime- Photo 31. Dredging pond at Cement stone deposit 64 Lapis sand deposit - 89 32. Pacific Aggregates' sand plant at Lapis Figure 13. Flowsheet of Moss Landing magnesia plant, Kaiser Photo Cement and _ 89 Aluminum and Chemical Corp _ 68 Photo 33. Pit at Fan Shell Beach dune deposit of Del Monte Properties 91 Figure 14. Map showing the distribution of peat deposits in Co Monterey County 75 Photo 34. Del Monte Properties Company sand plant near Pacific Grove - - 94 Figure 15. Map showing the evaporating and crystallizing ponds of Monterey Bay Salt Works 82 Photo 35. Test pit in Sawmill Gulch sand deposit of Del Monte . 96 Figure 16. Map of sand plants and dune deposits of Monterey Properties Company Peninsula 92 Photo 36. Close-up of test pit face at Sawmill Gulch sand de- Figure 17. Flowsheet of Del Monte Properties Company sand posit - 96 processing plant... 93 Photo 37. Sand dunes near Moss Beach utilized by Owens-Illinois for glass manufacture __ - 97 Photo 38. Owens-Illinois sand plant near Pacific Grove 98 Photo 1. Panorama across Salinas Valley toward northern Sierra Photo 39. Nacimiento River gravel deposit 103 de Salinas _ 9 Photo 40. South Counties Sand and Gravel Co. gravel pit at Photo 2. View southeast toward Swamp Creek area from Fre- mouth of Chalone Creek 103 mont Peak 9 Photo 41. Carmel River stream gravel deposit of Valley Rock Photo 3. View of rugged coastline and Santa Lucia Range at and Adobe Company... .~ 104 Big Creek __ 10 Photo 42. Zabala sand and gravel pit in Arroyo Seco drywash Photo 4. Bell tower of Carmel Mission 1 near Greenfield 104 Photo 5. Gristmill at Mission San Antonio de Padua 1 I Photo 43. Titus sand and gravel pit developed in Paso Robles Photo 6. Silicified dolomitic limestone at Fremont Peak 13 Formation at San Benancio Gulch 105 Photo 7. View of northern Santa Lucia Range 15 Photo 44. Haldorn decomposed granite pit near Carmel Valley. 109 Photo 8. Point Sur 16 Photo 45. Carmel Stone quarry (Passadori), Carmel Valley 110 Photo 9. Exposure of Eocene strata resting on basement com- Photo 46. Close-up of Carmel Stone quarry (Passadori) opera- plex near Church Creek 17 tions (two photos) - 112 Photo 10. View of Carmel River-Chupines Creek region 18 Photo 47. Use of Carmel Stone in home construction 113 [ 4 ] ABSTRACT Monterey County encompasses a 3,324-square-mile area that lies totally within the 1 Coast Ranges , jits rugged terrain is accented by the Santa Lucia Range which rises abruptly from the Pacific Ocean to an elevation of 5,844 feet. The broad, alluviated frl Salinas Valley separates that range from the Gabilan and Diablo Ranges to the north- east. Although the region is quite mountainous, agriculture is the foremost industry, accounting for well-over $100,000,000 production yearly. Other important industries include mining, and manufacturing based on agriculture and miningTjThe county also is noted for its natural beauty, early California history, and culture. Most of the 198,824 inhabitants are concentrated in the Salinas-Monterey Bay-Carmel Valley area where the climate is quite mild. The geology is typical of the southern Coast Ranges, being structurally and strati- graphically complex. Pre-Cretaceous metamorphic rocks of the Sur Series probably are the oldest rocks in Monterey County and these have been intruded by Cretaceous granitic rocks. This metamorphic-granitic complex is confined to the fault block between the northwest-trending San Andreas and Nacimiento-Sur fault zones. The Franciscan Formation and associated rocks of probable Late Jurassic and/or Cretaceous age comprise the oldest rocks of the flanking fault blocks. Overlying the "basement" rocks of the three fault blocks are a wide variety of sedimentary formations and some vol- canic rocks laid down during the Cretaceous, Tertiary, and Quaternary Periods. The rocks of the region have been subjected to strong structural deformation, resulting in the formation of important northwest-trending, right-lateral and high-angle reverse faults. Folding also has been intense in some areas but is manifested on a smaller scale. The most important mineral-bearing formations include the Sur Series (dolomite, lime- stone, barite); Franciscan Formation (gold) and related serpentine intrusives (chromite, mercury, asbestos); Cretaceous granitic rocks (stone, feldspar); Miocene sedimentary formations (oil, gas, coal, dimension stone, diatomite); and Quaternary alluvium, beach and dune deposits (sand, gravel, clay).
Recommended publications
  • Julia Pfeiffer Burns State Park
    Julia Pfeiffer Burns State Park Environmental Camping and Day-Use Area Big Sur, CA • (831) 667-2315 www.parks.ca.gov Located on Highway 1 at mile marker 36 you’ll find Julia Pfeiffer Burns State Park. This state park is named after Julia Pfeiffer Burns, a well respected pioneer woman in the Big Sur country. The park stretches from the Big Sur coastline into nearby 3,000-foot ridges. It features redwood, tan oak, madrone, chaparral, and an 80-foot waterfall that drops from granite cliffs into the ocean from the Overlook Trail. A panoramic view of the ocean and miles of rugged coastline maybe seen from the higher elevations along the trails east of Highway 1. FEES for day use parking are due upon entry into Trespassing into the closed areas may result in the park. Fee envelopes for self registration are citation and ejection from the park. located at the self pay station near the restrooms. ROPES, lines, swings or hammocks may not be Fee amounts for day use are posted. fastened to any plant, fence or park structure. Attach CAMPING is extremely popular year round and is lines to your own property only. generally available only by advance reservation. BICYCLES are not allowed on any hiking trails Campers parking vehicles in the main parking within the park. lot should display proof of reservation in the windshield. Campers may also check in at the kiosk FIREARMS/WEAPONS OR HUNTING is not in Pfeiffer Big Sur State Park (12 miles north) to get allowed. Possession of loaded firearms and air rifles vehicle tags also valid for day use entrance into is prohibited.
    [Show full text]
  • Field Guide to Neotectonics of the San Andreas Fault System, Santa Cruz Mountains, in Light of the 1989 Loma Prieta Earthquake
    Department of the Interior U.S. Geological Survey Field Guide to Neotectonics of the San Andreas Fault System, Santa Cruz Mountains, in Light of the 1989 Loma Prieta Earthquake | Q|s | Landslides (Quaternary) I yv I Vaqueros Sandstone (Oligocene) r-= I San Lorenzo Fm., Rices Mudstone I TSr I member (Eocene-Oligocene) IT- I Butano Sandstone, ' Pnil mudstone member (Eocene) Coseismic surface fractures, ..... dashed where discontinuous, dotted where projected or obscured ___ _ _ Contact, dashed where approximately located >"«»"'"" « « Fault, dotted where concealed V. 43? Strike and dip Strike and dip of of bedding overturned bedding i Vector Scale / (Horizontal Component of Displacement) OPEN-FILE REPORT 90-274 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, product, or firm names is for descriptive purposes only and does not imply endorsement by the U. S. Government. Men to Park, California April 27, 1990 Department of the Interior U.S. Geological Survey Field Guide to Neotectonics of the San Andreas Fault System, Santa Cruz Mountains, in Light of the 1989 Loma Prieta Earthquake David P. Schwartz and Daniel J. Ponti, editors U. S. Geological Survey Menlo Park, CA 94025 with contributions by: Robert S. Anderson U.C. Santa Cruz, Santa Cruz, CA William R. Cotton William Cotton and Associates, Los Gatos, CA Kevin J. Coppersmith Geomatrix Consultants, San Francisco, CA Steven D. Ellen U. S. Geological Survey, Menlo Park, CA Edwin L. Harp U. S. Geological Survey, Menlo Park, CA Ralph A.
    [Show full text]
  • Carmel Valley Resident Larry Scholink Turned to the Monterey County Board of Supervisors This Week for Help
    A celebration of the Carmel lifestyle… a special section inside InYouDr reamsthis week! BULK RATE U.S. POSTAGE PAID CARMEL, CA Permit No. 149 Volume 94 No. 13 On the Internet: www.carmelpinecone.com March 28-April 3, 2008 Y OUR S OURCE F OR L OCAL N EWS, ARTS AND O PINION S INCE 1915 THE SPEED BUMP IS NO MORE Laird calls for delay in By MARY BROWNFIELD water cutback order HE DOLORES Street speed T By KELLY NIX bump that had neighbors drawing battle lines was removed Tuesday, N A letter to the State Water Resources Control Board, 27th District a week after a contentious com- I Assemblyman John Laird urged the agency to delay acting on a cease and munity meeting in Carmel City desist order that would require the Peninsula to limit its water use to Hall where residents bickered, extremely low levels. found no compromises, threatened In the three-page letter dated March 25, Laird also criticized the to sue and walked out in anger. California Public Utilities Commission for taking three years to finalize At issue was the black and yel- an environmental impact report on Cal Am’s proposed Coastal Water low plastic speed hump nailed to Project, which includes a desalination plant that would provide a drought- the asphalt last October, mostly in free water supply. response to the organized cam- “This order would punish the local Monterey Peninsula community paign and repeated pleas of resi- for the slow speed at which the PUC has moved to conceive and design a dent Jeff White, who said people new project,” according to the letter.
    [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]
  • The Carmel Pine Cone
    VolumeThe 105 No. 42 Carmelwww.carmelpinecone.com Pine ConeOctober 18-24, 2019 T RUS T ED BY LOCALS AND LOVED BY VISI T ORS SINCE 1 9 1 5 Deal pending for Esselen tribe to buy ranch Cal Am takeover By CHRIS COUNTS But the takeover is not a done deal yet, despite local media reports to the contrary, Peter Colby of the Western study to be IF ALL goes according to plan, it won’t be a Silicon Rivers Conservancy told The Pine Cone this week. His Valley executive or a land conservation group that soon group is brokering the deal between the current owner of takes ownership of a remote 1,200-acre ranch in Big Sur the ranch, the Adler family of Sweden, and the Esselen released Nov. 6 but a Native American tribe with deep local roots. Tribe of Monterey County. “A contract for the sale is in place, By KELLY NIX but a number of steps need to be com- pleted first before the land is trans- THE LONG-AWAITED findings of a study to deter- ferred,” Colby said. mine the feasibility of taking over California American While Colby didn’t say how much Water’s local system and turning it into a government-run the land is selling for, it was listed operation will be released Nov. 6, the Monterey Peninsula at $8 million when The Pine Cone Water Management District announced this week. reported about it in 2017. But ear- The analysis was launched after voters in November lier this month, the California Nat- 2018 OK’d a ballot measure calling for the water district ural Resources Agency announced to use eminent domain, if necessary, to acquire Cal Am’s that something called “the Esselen Monterey Peninsula water system if the move was found Tribal Lands Conservation Project” to be cost effective.
    [Show full text]
  • Big Sur for Other Uses, See Big Sur (Disambiguation)
    www.caseylucius.com [email protected] https://en.wikipedia.org/wiki/Main_Page Big Sur For other uses, see Big Sur (disambiguation). Big Sur is a lightly populated region of the Central Coast of California where the Santa Lucia Mountains rise abruptly from the Pacific Ocean. Although it has no specific boundaries, many definitions of the area include the 90 miles (140 km) of coastline from the Carmel River in Monterey County south to the San Carpoforo Creek in San Luis Obispo County,[1][2] and extend about 20 miles (30 km) inland to the eastern foothills of the Santa Lucias. Other sources limit the eastern border to the coastal flanks of these mountains, only 3 to 12 miles (5 to 19 km) inland. Another practical definition of the region is the segment of California State Route 1 from Carmel south to San Simeon. The northern end of Big Sur is about 120 miles (190 km) south of San Francisco, and the southern end is approximately 245 miles (394 km) northwest of Los Angeles. The name "Big Sur" is derived from the original Spanish-language "el sur grande", meaning "the big south", or from "el país grande del sur", "the big country of the south". This name refers to its location south of the city of Monterey.[3] The terrain offers stunning views, making Big Sur a popular tourist destination. Big Sur's Cone Peak is the highest coastal mountain in the contiguous 48 states, ascending nearly a mile (5,155 feet/1571 m) above sea level, only 3 miles (5 km) from the ocean.[4] The name Big Sur can also specifically refer to any of the small settlements in the region, including Posts, Lucia and Gorda; mail sent to most areas within the region must be addressed "Big Sur".[5] It also holds thousands of marathons each year.
    [Show full text]
  • Possible Correlations of Basement Rocks Across the San Andreas, San Gregorio- Hosgri, and Rinconada- Reliz-King City Faults
    Possible Correlations of Basement Rocks Across the San Andreas, San Gregorio- Hosgri, and Rinconada- Reliz-King City Faults, U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1317 Possible Correlations of Basement Rocks Across the San Andreas, San Gregorio- Hosgri, and Rinconada- Reliz-King City Faults, California By DONALD C. ROSS U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1317 A summary of basement-rock relations and problems that relate to possible reconstruction of the Salinian block before movement on the San Andreas fault UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1984 DEPARTMENT OF THE INTERIOR WILLIAM P. CLARK, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data Boss, Donald Clarence, 1924- Possible correlations of basement rocks across the San Andreas, San Gregrio-Hosgri, and Rinconada-Reliz-King City faults, California (U.S. Geological Survey Bulletin 1317) Bibliography: p. 25-27 Supt. of Docs, no.: 119.16:1317 1. Geology, structural. 2. Geology California. 3. Faults (geology) California. I. Title. II. Series: United States. Geological Survey. Professional Paper 1317. QE601.R681984 551.8'09794 84-600063 For sale by the Distribution Branch, Text Products Section, U.S. Geological Survey, 604 South Pickett St., Alexandria, VA 22304 CONTENTS Page Abstract _____________________________________________________________ 1 Introduction __________________________________________________________ 1 San Gregorio-Hosgri fault zone ___________________________________________ 3 San Andreas
    [Show full text]
  • Julia Pfeiffer Burns State Park -2020 Special Event Permit Information
    Julia Pfeiffer Burns State Park - 2020 Special Event Permit Information The Mission of California State Parks is to provide for the health, inspiration, and education of the people of California by helping to preserve the state’s extraordinary biological diversity, protecting its most valued natural and cultural resources, and creating opportunities for high-quality outdoor recreation. Thank you for your interest in the Special Event Program at Julia Pfeiffer Burns State Park. Julia Pfeiffer Burns State Park is located along the coast on Highway 1. Although there is no beach or waterfall access at this park, there are spectacular views of the ocean and McWay Falls. This park offers two (2) unique event venues which are available for advanced reservation. All the locations in the park are outdoors and rustic. They are suitable for those wishing to have an event in a natural setting without modern trappings. We permit small, simple weddings with minimal decorations during day-use hours that may last up to two (2) hours. Large events, evening/night events, or events that will last more than two (2) hours are not permitted at this park. Because of the rustic nature of these sites, we highly recommend visiting the park and location(s) you are interested in reserving for your event prior to applying for a Special Event Permit. You can apply for a Special Event Permit up to one (1) year in advance. This packet contains information on how to obtain a Special Event Permit and the permit requirements. Please review this packet thoroughly. Table of Contents • Page 2: What is a Special Event? and What is the Special Event Coordinator? • Page 3: Special Event Permit Process • Page 4: Fees and Deposits • Page 5: Site Fees • Page 6: Certificate of Liability Insurance information • Pages 7 - 13: FAQ and Special Event Permit Parameters at Julia Pfeiffer Burns State Park.
    [Show full text]
  • California Coastal Commission Staff Report and Recommendation
    STATE OF CALIFORNIA – THE RESOURCES AGENCY ARNOLD SCHWARZENEGGE R, Governor CALIFORNIA COASTAL COMMISSION CENTRAL COAST DISTRICT OFFICE 725 FRONT STREET, SUITE 300 SANTA CRUZ, CA 95060 (831) 427-4863 Th10a Filed: 11/02/2004 49th day: Waived Staff: Katie Morange-SC Staff report: 10/26/2006 Hearing date: 11/16/2006 Hearing item number: Th10a APPEAL STAFF REPORT SUBSTANTIAL ISSUE DETERMINATION AND DE NOVO HEARING Application number.......A-3-MCO-04-064 Applicant.........................California Department of Parks & Recreation, Monterey District, Attn: Tom Moss Appellants .......................Friends of the Big Sur Coast & Joseph P. Schoendorf, Attn: John Briscoe, Stoel Rives LLP Local government ..........Monterey County (PLN030620) Local decision .................Board of Supervisors Resolution 04-326: approved with conditions on September 28, 2004, and received by Central Coast District office of Coastal Commission on October 19, 2004. Project location ..............Julia Pfeiffer-Burns State Park (Highway One), Big Sur Coast Planning Area, Monterey County (APNs 420-021-007, 420-021-022, 420-021-033, 420-021- 034, 420-021-020, 420-011-027, 420-221-013, 420-221-020). Project description.........Waterfall House Landscape Maintenance Project consisting of removing 4,516 exotic plants (trees and shrubs) and replacing them with native plants near environmentally sensitive habitat areas (ESHA) and on slopes exceeding 30%. File documents................Monterey County Certified Local Coastal Program (LCP); Final Local Action Notice (FLAN) for local permit PLN030620. Staff recommendation ...Substantial Issue; Approval with Conditions Summary On September 28, 2004, the Monterey County Board of Supervisors approved a Coastal Development Permit (CDP) for the Waterfall House Landscape Maintenance Project consisting of the removal of 4,516 non-native plants (including blue gum eucalyptus, Victoria box, and Bailey acacia) near environmentally sensitive habitat and on slopes exceeding 30% at Julia Pfeiffer-Burns State Park (JPBSP) in the Big Sur Coast Planning Area.
    [Show full text]
  • Coastal Management Accomplishments in the Big Sur Coast Area
    CCC Hearing Item: Th 13.3 February 9, 2012 _______________________________________________________________ California Coastal Commission’s 40th Anniversary Report Coastal Management in Big Sur History and Accomplishments Gorda NORTHERN BIG SUR Gorda NORTHERN BIG SUR CENTRAL BIG SUR Gorda NORTHERN BIG SUR CENTRAL BIG SUR SOUTHERN BIG SUR Gorda “A Highway Runs Through It” Highway One, southbound, north of Soberanes Point. ©Kelly Cuffe 2012 “A Highway Runs Through It” Highway One, at Cape San Martin, Big Sur Coast. CCRP#1649 9/2/2002 “A Highway Runs Through It” Heading south on Highway One. “A Highway Runs Through It” Southbound Highway One, near Partington Point. ©Kelly Cuffe 2012 “A Highway Runs Through It” Highway One, south of Mill Creek. ©Kelly Cuffe 2012 “A Highway Runs Through It” Historic Big Creek Bridge, at entrance to U.C. Big Creek Reserve. ©Kelly Cuffe 2012 “A Highway Runs Through It” Highway One, looking south to the coastal terrace at Pacific Valley. ©Kelly Cuffe 2012 “A Highway Runs Through It” Highway One, at Monterey County line, looking south into San Luis Obispo County, with Ragged Point and Piedras Blancas in far distance (on the right). ©Kelly Cuffe 2012 NORTHERN BIG SUR “Grand Entrance View” (from the north) of the Big Sur Coast, looking southwards to Soberanes Point, with Point Sur in the distance (on the horizon to the right). ©Kelly Cuffe 2012 Garrapata State Park/Beach, looking north to Soberanes Point. ©Kelly Cuffe 2012 Mouth of Garrapata Creek (from Highway One). ©Kelly Cuffe 2012 Sign for Rocky Point Restaurant, with Notley’s Landing and Rocky Creek Bridge in distance.
    [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]
  • Monterey County
    Steelhead/rainbow trout resources of Monterey County Salinas River The Salinas River consists of more than 75 stream miles and drains a watershed of about 4,780 square miles. The river flows northwest from headwaters on the north side of Garcia Mountain to its mouth near the town of Marina. A stone and concrete dam is located about 8.5 miles downstream from the Salinas Dam. It is approximately 14 feet high and is considered a total passage barrier (Hill pers. comm.). The dam forming Santa Margarita Lake is located at stream mile 154 and was constructed in 1941. The Salinas Dam is operated under an agreement requiring that a “live stream” be maintained in the Salinas River from the dam continuously to the confluence of the Salinas and Nacimiento rivers. When a “live stream” cannot be maintained, operators are to release the amount of the reservoir inflow. At times, there is insufficient inflow to ensure a “live stream” to the Nacimiento River (Biskner and Gallagher 1995). In addition, two of the three largest tributaries of the Salinas River have large water storage projects. Releases are made from both the San Antonio and Nacimiento reservoirs that contribute to flows in the Salinas River. Operations are described in an appendix to a 2001 EIR: “ During periods when…natural flow in the Salinas River reaches the north end of the valley, releases are cut back to minimum levels to maximize storage. Minimum releases of 25 cfs are required by agreement with CDFG and flows generally range from 25-25[sic] cfs during the minimum release phase of operations.
    [Show full text]