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Excerpt from the Steelhead Report Concerning Napa County (212
Historical Distribution and Current Status of Steelhead/Rainbow Trout (Oncorhynchus mykiss) in Streams of the San Francisco Estuary, California Robert A. Leidy, Environmental Protection Agency, San Francisco, CA Gordon S. Becker, Center for Ecosystem Management and Restoration, Oakland, CA Brett N. Harvey, John Muir Institute of the Environment, University of California, Davis, CA This report should be cited as: Leidy, R.A., G.S. Becker, B.N. Harvey. 2005. Historical distribution and current status of steelhead/rainbow trout (Oncorhynchus mykiss) in streams of the San Francisco Estuary, California. Center for Ecosystem Management and Restoration, Oakland, CA. Center for Ecosystem Management and Restoration NAPA COUNTY Huichica Creek Watershed The Huichica Creek watershed is in the southwest corner of Napa County. The creek flows in a generally southern direction into Hudeman Slough, which enters the Napa River via the Napa Slough. Huichica Creek consists of approximately eight miles of channel. Huichica Creek In March 1966 and in the winters of 1970 and 1971, DFG identified O. mykiss in Huichica Creek (Hallett and Lockbaum 1972; Jones 1966, as cited in Hallett, 1972). In December 1976, DFG visually surveyed Huichica Creek from the mouth to Route 121 and concluded that the area surveyed offered little or no value as spawning or nursery grounds for anadromous fish. However, the area was said to provide passage to more suitable areas upstream (Reed 1976). In January 1980, DFG visually surveyed Huichica Creek from Route 121 upstream to the headwaters. Oncorhynchus mykiss ranging from 75–150 mm in length were numerous and were estimated at a density of 10 per 30 meters (Ellison 1980). -
ROGER Y. ANDERSON Department of Geology, the University of New Mexico, Albuquerque, New Mexico 87106 WALTER E
ROGER Y. ANDERSON Department of Geology, The University of New Mexico, Albuquerque, New Mexico 87106 WALTER E. DEAN, JR. Department of Geology, Syracuse University, Syracuse, New Yor\ 13210 DOUGLAS W. KIRKLAND Mobil Research and Development Corporation, Dallas, Texas 75221 HENRY I. SNIDER Department of Physical Sciences, Eastern Connecticut State College, Willimantic, Connecticut 06226 Permian Castile Varved Evaporite Sequence, West Texas and New Mexico ABSTRACT is a change from thinner undisturbed anhy- drite laminae to thicker anhydrite laminae that Laminations in the Upper Permian evaporite generally show a secondary or penecontem- sequence in the Delaware Basin appear in the poraneous nodular character, with about 1,000 preevaporite phase of the uppermost Bell to 3,000 units between major oscillations or Canyon Formation as alternations of siltstone nodular beds. These nodular zones are correla- and organic layers. The laminations then change tive throughout the area of study and underly character and composition upward to organi- halite when it is present. The halite layers cally laminated claystone, organically laminated alternate with anhydrite laminae, are generally calcite, the calcite-laminated anhydrite typical recrystallized, and have an average thickness of the Castile Formation, and finally to the of about 3 cm. The halite beds were once west anhydrite-laminated halite of the Castile and of their present occurrence in the basin but Salado. were dissolved, leaving beds of anhydrite Laminae are correlative for distances up to breccia. The onset and cessation of halite depo- 113 km (70.2 mi) and probably throughout sition in the basin was nearly synchronous. most of the basin. Each lamina is synchronous, The Anhydrite I and II Members thicken and each couplet of two laminated components gradually across the basin from west to east, is interpreted as representing an annual layer of whereas the Halite I, II, and III Members are sedimentation—a varve. -
DIAGENESIS of the BELL CANYON and CHERRY CANYON FORMATIONS (GUADALUPIAN), COYANOSA FIELD AREA, PECOS COUNTY, TEXAS by Katherine
Diagenesis of the Bell Canyon and Cherry Canyon Formations (Guadalupian), Coyanosa field area, Pecos County, Texas Item Type text; Thesis-Reproduction (electronic) Authors Kanschat, Katherine Ann Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 28/09/2021 19:22:41 Link to Item http://hdl.handle.net/10150/557840 DIAGENESIS OF THE BELL CANYON AND CHERRY CANYON FORMATIONS (GUADALUPIAN), COYANOSA FIELD AREA, PECOS COUNTY, TEXAS by Katherine Ann Kanschat A Thesis Submitted to the Faculty of the DEPARTMENT OF GEOSCIENCES In Partial Fulfillment of the Requirements For the Degree of MASTER OF SCIENCE In the Graduate College THE UNIVERSITY OF ARIZONA 19 8 1 STATEMENT BY AUTHOR This thesis has been submitted in partial fulfillment of requirements for an advanced degree at The University of Arizona and is deposited in the University Library to be made available to borrowers under rules of the Library. Brief quotations from this thesis are allowable with out special permission, provided that accurate acknowledge ment of source is made. Requests for permission for ex tended quotation from or reproduction of this manuscript in whole or in part may be granted by the head of the major de partment or the Dean of the Graduate College when in his judgment the proposed use of the material is in the inter ests of scholarship. -
Salt Caverns Studies
SALT CAVERN STUDIES - REGIONAL MAP OF SALT THICKNESS IN THE MIDLAND BASIN FINAL CONTRACT REPORT Prepared by Susan Hovorka for U.S. Department of Energy under contract number DE-AF22-96BC14978 Bureau of Economic Geology Noel Tyler, Director The University of Texas at Austin Austin, Texas 78713-8924 February 1997 CONTENTS Executive Summmy ....................... ..... ...................................................................... ...................... 1 Introduction ..................................................... .. .............................................................................. 1 Purpose .......................................................................................... ..................................... ............. 2 Methods ........................................................................................ .. ........... ...................................... 2 Structural Setting and Depositional Environments ......................................................................... 6 Salt Thickness ............................................................................................................................... 11 Depth to Top of Salt ...................................................................................................................... 14 Distribution of Salt in the Seven Rivers, Queen, and Grayburg Formations ................................ 16 Areas of Salt Thinning ................................................................................................................. -
The Southern California Wetlands Recovery Project’S Regional Strategy
Developing a Science-based, Management- driven Plan for Restoring Wetlands: The Southern California Wetlands Recovery Project’s Regional Strategy Carolyn Lieberman U.S. Fish and Wildlife Service Coastal Program Mediterranean Climate Average Monthly Temperature at Lindbergh Field, San Diego 80 70 60 50 40 30 Temperature (*F) Temperature 20 10 0 JAN FEB MAR APR MAY JUN JUL AUG SEP OCT NOV DEC Month Average Monthly Rainfall at Lindbergh Field, San Diego 2 1.8 1.6 1.4 1.2 1 0.8 Rainfall Rainfall (inches) 0.6 0.4 0.2 0 JAN FEB MAR APR MAY JUN JUL AUG SEP OCT NOV DEC Month Based on data from 1948-1990 (http://www.wrh.noaa.gov/sgx/climate/san-san.htm) Coastal Wetland Systems of Southern California • Approximately 100 distinct systems • Total of 8,237 ha • Range = 0.03 ha – 1,322 ha – Average size = 81 ha Small Creek Mouth Systems Bell Canyon Arroyo Burro Intermittently Closing River Mouth Estuaries Malibu Lagoon Open Basin, Fringing Intertidal Wetland Anaheim Bay and Seal Beach Large Depositional River Valley Tijuana River Valley Harbors, Bay, Lagoons Mission Bay Mission Bay San Diego Bay Sensitive Species in Coastal Estuaries Ridgway’s rail Western snowy plover Belding’s savannah sparrow Salt marsh bird’s beak Light-footed clapper rail California least tern Migratory Birds Southern California Wetland Recovery Project Federal Partners National Marine Fisheries Service Natural Resources Conservation Service U.S. Army Corps of Engineers U.S. Environmental Protection Agency U.S. Fish and Wildlife Service State Partners California Natural Resources -
Southern Coastal Santa Barbara Streams and Estuaries Bioassessment Program
SOUTHERN COASTAL SANTA BARBARA STREAMS AND ESTUARIES BIOASSESSMENT PROGRAM 2014 REPORT AND UPDATED INDEX OF BIOLOGICAL INTEGRITY Prepared for: City of Santa Barbara, Creeks Division County of Santa Barbara, Project Clean Water Prepared By: www.ecologyconsultantsinc.com Ecology Consultants, Inc. Executive Summary Introduction This report summarizes the results of the 2014 Southern Coastal Santa Barbara Streams and Estuaries Bioassessment Program, an effort funded by the City of Santa Barbara and County of Santa Barbara. This is the 15th year of the Program, which began in 2000. Ecology Consultants, Inc. (Ecology) prepared this report, and serves as the City and County’s consultant for the Program. The purpose of the Program is to assess and monitor the “biological integrity” of study streams and estuaries as they respond through time to natural and human influences. The Program involves annual collection and analyses of benthic macroinvertebrate (BMI) samples and other pertinent physiochemical and biological data at study streams using U.S. Environmental Protection Agency (USEPA) endorsed rapid bioassessment methodology. BMI samples are analyzed in the laboratory to determine BMI abundance, composition, and diversity. Scores and classifications of biological integrity are determined for study streams using the BMI based Index of Biological Integrity (IBI) constructed by Ecology. The IBI was initially built in 2004, updated in 2009, and has been updated again this year. The IBI yields a numeric score and classifies the biological integrity of a given stream as Very Poor, Poor, Fair, Good, or Excellent based on the contents of the BMI sample collected from the stream. Several “core metrics” are calculated and used to determine the IBI score. -
ACR Heron and Egret Project (HEP) 2018 Season
ACR Heron and Egret Project (HEP) 2018 Season Dear Friends, Here it is once again, our annual call to “get HEP!” To all new and returning volunteers, thank you so much for contributing your time and expertise to the 29th season of ACR’s Heron and Egret Project. Together we continue to expand our rich, decades‐long data set that is put into action each year to increase our understanding of the natural world and promote its conservation. Last year we were pleased to tell you about the new Heron and Egret Telemetry Project. Led by Scott Jennings and David Lumpkin, we had a successful first year—safely tagging three adult Great Egrets. You can follow along as we observe the highly‐detailed log of their movements right here: https://www.egret.org/heron‐egret‐telemetry‐project. Coupled with the detailed reproductive information that you collect at each nesting site, these GPS data will help us improve our understanding of the roles herons and egrets play in the wetland ecosystem and how their habitat needs affect population dynamics. Ultimately, we hope these findings will inform conservation efforts and inspire generations of people to value these beautiful birds and the wetlands that sustain us all. As most of you already know, this is John Kelly’s last year as Director of Conservation Science at Audubon Canyon Ranch. Though it is difficult to imagine life at the Cypress Grove Research Center without John’s intelligent leadership, fierce conservation ethic, and kind support, we are all very grateful for the time he has given this organization and look forward to hearing about his new adventures. -
Speleogenesis and Delineation of Megaporosity and Karst
Stephen F. Austin State University SFA ScholarWorks Electronic Theses and Dissertations 12-2016 Speleogenesis and Delineation of Megaporosity and Karst Geohazards Through Geologic Cave Mapping and LiDAR Analyses Associated with Infrastructure in Culberson County, Texas Jon T. Ehrhart Stephen F. Austin State University, [email protected] Follow this and additional works at: https://scholarworks.sfasu.edu/etds Part of the Geology Commons, Hydrology Commons, and the Speleology Commons Tell us how this article helped you. Repository Citation Ehrhart, Jon T., "Speleogenesis and Delineation of Megaporosity and Karst Geohazards Through Geologic Cave Mapping and LiDAR Analyses Associated with Infrastructure in Culberson County, Texas" (2016). Electronic Theses and Dissertations. 66. https://scholarworks.sfasu.edu/etds/66 This Thesis is brought to you for free and open access by SFA ScholarWorks. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of SFA ScholarWorks. For more information, please contact [email protected]. Speleogenesis and Delineation of Megaporosity and Karst Geohazards Through Geologic Cave Mapping and LiDAR Analyses Associated with Infrastructure in Culberson County, Texas Creative Commons License This work is licensed under a Creative Commons Attribution-Noncommercial-No Derivative Works 4.0 License. This thesis is available at SFA ScholarWorks: https://scholarworks.sfasu.edu/etds/66 Speleogenesis and Delineation of Megaporosity and Karst Geohazards Through Geologic Cave Mapping and LiDAR Analyses Associated with Infrastructure in Culberson County, Texas By Jon Ehrhart, B.S. Presented to the Faculty of the Graduate School of Stephen F. Austin State University In Partial Fulfillment Of the requirements For the Degree of Master of Science STEPHEN F. -
WANDERING TATTLER Newsletter
Wandering Dec. 2011- Jan. 2012 Tattler Volume 61 , Number 4 The Voice of SEA AND SAGE AUDUBON, an Orange County Chapter of the National Audubon Society President’s Message General Meeting by Bruce Aird January 20th - Friday evening - 7:30 pm So its December, and the thought on everyones mind is… “A Photographic Adventure at the holidays? No, what all birders are thinking about is Midway Atoll” Christmas Bird Counts (CBCs). You dont know about those? How is that even possible?! CBCs are a long- presented by Bob Steele standing holiday tradition - one of the best there is. Its as non-denominational as holiday cheer gets, and for just a Midway Atoll (mid-way between the U.S. mainland and $5 fee, its way cheaper than most of those other Japan) is important for many historical and biological traditions. This is when that bright Wilsons Warbler, so reasons. Today it is part of three federal designations - common as to be unworthy of notice three months ago, is Midway Atoll NWR, Papahânaumokuâkea Marine National suddenly a prize. The winter vagrants are settled in and Monument, and the Battle of Midway National Memorial. now we work to find them for the CBCs. Trust me, theres Well over a million seabirds use the three tiny islands in no better present under the tree than a previously the atoll to breed each season, including over half of the unreported Varied Thrush! world's population of Laysan Albatross. Join wildlife photographer Bob Steele as he explores the human and Heres how it works. Within established count circles of 15 natural history of this unique and fascinating place. -
Salado Formation Followed
GW -^SZ-i^ GENERAL CORRESPONDENCE YEAR(S): B. QUICK, Inc. 3340 Quail View Drive • Nashville, TN 37214 Phone: (615) 874-1077 • Fax: (615) 386-0110 Email: [email protected] November 12,2002 Mr Roger Anderson Environmental Bureau Chief New Mexico OCD 1220 S. ST. Francis Dr. 1 Santa Fe, NM 87507 Re: Class I Disposal Wells Dear Roger, I am still very interested in getting the disposal wells into salt caverns in Monument approved by OCD. It is my sincere belief that a Class I Disposal Well would be benefical to present and future industry in New Mexico. I suspect that one of my problems has been my distance from the property. I am hoping to find a local company or individuals who can be more on top of this project. In the past conditions have not justified the capital investment to permit, build and operate these wells and compete with surface disposal. Have there been any changes in OCD policy that might effect the permitting of these wells? If so, would you please send me any pretinent documents? Sincerely, Cc: Lori Wrotenbery i aoie or moments rage i uu Ctoraeferiz&MoiHi ©ff Bedded Satt fltoir Storage Caverns Case Stundy from the Midlamdl Basim Susan D. Hovorka Bureau of Economic Geology The University of Texas at Austin AUG1 0R9 9 Environmental Bureau Introduction to the Problem °" Conservation D/ws/on About solution-mined caverns l^Btg*** Geolojy_ofsalt Purpose, scope, and methods of our study Previous work: geologic setting of the bedded salt in the Permian Basin J^rV^W^' " Stratigraphic Units and Type Logs s Midland Basin stratigraphy -
Ru Bidium-Strontium and Related Studies of the Salado Formation, Southeastern New Mexico
CONTRACTOR REPORT SAND8 1-7072 PROPERTY OF GSA LIBRARY Unlimited.Release UC-70 Ru bidium-Strontium and Related Studies of the Salado Formation, Southeastern New Mexico Joseph K. Register University of New Mexico, Albuquerque Prepared by Sandia National Laboratones, Albuquerque. New Mexico 87185 and Livermore, Californ~a94550 for the United States Department of Energy under Contract DE-AC04-76DP00789 Printed October 198 1 Prepared for Sandia National Laboratories under Contract No. 13-9756 Issued by Sandia National Laboratories, operated for the United States Department of Energy by Sandia Corporation. NOTICE: This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees nor any of theu contractors subcontractors or their employees makes any wanan'ty express or implied or assukes any legal lAbility or responsibdty for the accuracy cdmp~etenessorusefuiness of any information apparatus product or process disclosed or represent; that its use would not inhinie privatel; owned iights. Reference here& to any specific commercial product. process. or,service by trade name trademark manufacturer or otherwise does not necessarily constitute or imply its enddrsement re'commendation' or favoring by the United States Government any agency thereof or hyof their contr;ctors or subcontractors. The views and opinion; expressed herein do not necessarily state ,or reflect those of the United States Government, any agency thereof or any of theu contractors or subcontractors. Printed in the United States of America Available from National Technical Information Servlce U. S. Department of Commerce 5285 Port Royal Road Springfield. -
Karst in Evaporites in Southeastern New Mexico*
Waste Isolation Pilot Plant Compliance Certification Application Reference 27 Bachman, G. 0., 1987. Karst in Evaporites in Southeast~m New Mexico, SAND86-7078, Albuquerque, NM, Sandia National Laboratories. Submitted in accordance with 40 CPR §194.13, Submission of Reference Materials. ~I SAND86-7078 Distribution Unlimited Release Category UC-70 Printed September 1987 Karst in Evaporites in Southeastern New Mexico* SAND--86-7078 DE88 001315 George 0. Bachman, Consultant 4008 Hannett Avenue NE Albuquerque, NM 87110 Abstract Permian evaporites in southeastern New Mexico include gypsum, anhydrite, and salt, which are subject to both blanket and local, selective dissolution. Dissolution has produced many hundreds of individual karst features including collapse sinks, karst valleys, blind valleys, karst plains, caves, and breccia pipes. Dissolution began within some formations during Permian time and has been intermittent but continual ever since. Karst features other than blanket deposits of breccia are not preserved from the early episodes of dissolution, but some karst features preserved today-such as breccia pipes-are remnants of karst activity that was active at least as early as mid-Pleistocene time. Rainfall was much more abundant during Late Pleistocene time, and many features visible today may have been formed then. The drainage history of the Pecos River is related to extensive karstification of the Pecos Valley during mid-Pleistocene time. Large-scale stream piracy and dissolution of - salt in the subsurface resulted in major shifts and excavations in the channel. In spite of intensive groundwater studies that have been carried out in the region, major problems in groundwater in near-surface evaporite karst remain to be solved.