1 ARROYO CHUB Gila Orcutti (Eigenmann and Eigenmann
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LOMR)? for a One-Year Premium Refund
the Arroyo Chico and Tucson Arroyo a FIRM. You may view this tutorial at: Property owners whose buildings have been watercourses. http://www.fema.gov/media- removed from an SFHA and are now located in library/assets/documents/7984 a Zone X or a Shaded Zone X may be eligible What is a Letter of Map Revision (LOMR)? for a one-year premium refund. Your lender When does a LOMR change a FIRM? must provide you with a letter agreeing to A LOMR is an official revision to the Flood remove the requirement for flood insurance. If Insurance Rate Maps (FIRMs) issued by the LOMRs become effective once the statutory your lender refuses to send you a letter stating Federal Emergency Management Agency Technical Appeal Period is over. The that they will not require flood insurance, you (FEMA). LOMRs reflect changes to the 100- effective date is listed on the LOMR cover will not be eligible for a refund. If you do not year floodplains or Special Flood Hazard letter. have a lender, you will not be eligible for a Areas (SFHA) shown on the FIRMs. In rare refund. To learn if you are eligible, please situations, LOMRs also modify the 500-year Can I drop my flood insurance if my follow these steps: floodplain boundaries. Changes may include residence or business is removed from ARROYO CHICO FLOODPLAIN modifications to Base Flood Elevations, the floodplain by a LOMR? 1. View the revised flood maps to REMAPPING floodplain widths, and floodways. The determine if your property has been re- QUESTIONS AND ANSWERS LOMRs are issued after a floodplain has The Flood Disaster Protection Act of 1973 mapped to a Zone X or Shaded Zone been remapped due to a major flood event, and the National Flood Insurance Reform Act X. -
PREHISTORIC FORAGING PATTERNS at CA-SAC-47 SACRAMENTO COUNTY, CALIFORNIA a Thesis Presented to the Faculty of the Department Of
PREHISTORIC FORAGING PATTERNS AT CA-SAC-47 SACRAMENTO COUNTY, CALIFORNIA A Thesis Presented to the Faculty of the Department of Anthropology California State University, Sacramento Submitted in partial satisfaction of the requirements for the degree of MASTER OF ARTS in Anthropology by Justin Blake Cairns SUMMER 2016 © 2016 Justin Blake Cairns ALL RIGHTS RESERVED ii PREHISTORIC FORAGING PATTERNS AT CA-SAC-47 SACRAMENTO COUNTY, CALIFORNIA A Thesis by Justin Blake Cairns Approved by: ________________________________, Committee Chair Mark E. Basgall, Ph.D. ________________________________, Second Reader Jacob L. Fisher, Ph.D. ____________________________ Date iii Student: Justin Blake Cairns I certify that this student has met the requirements for format contained in the University format manual, and that this thesis is suitable for shelving in the Library and credit is to be awarded for the thesis. __________________________________, Graduate Coordinator _______________ Jacob Fisher, Ph.D. Date Department of Anthropology iv Abstract of PREHISTORIC FORAGING PATTERNS AT CA-SAC-47 SACRAMENTO COUNTY, CALIFORNIA by Justin Blake Cairns Subsistence studies conducted on regional archaeological deposits indicate that in the Sacramento Delta, as in the rest of the Central Valley, there is a decrease in foraging efficiency during the Late Period. A recently excavated site, CA-SAC-47, provides direct evidence of subsistence strategies in the form of faunal and plant remains. This faunal assemblage is compared to direct evidence of subsistence from Delta sites SAC-42, SAC-43, SAC-65, SAC-145, and SAC-329. The results and implications of this direct evidence are used to address site variability and resource selectivity. ___________________________________, Committee Chair Mark E. -
Drainage Net
Drainage Net GEOLOGICAL SURVEY PROFESSIONAL f APER 282-A Ephemeral Streams Hydraulic Factors and Their Relation to the Drainage Net By LUNA B. LEOPOLD and JOHN P. MILLER PHYSIOGRAPHIC AND HYDRAULIC STUDIES OF RIVERS GEOLOGICAL SURVEY PROFESSIONAL PAPER 282-A UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1956 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY H. William Menard, Director Fin* printing 19M Second printing 1K9 Third printing 1MB For sale by the Branch of Distribution, U.S. Geological Survey, 1200 South Eads Street, Arlington, VA 22202 CONTENTS Page Page Symbols. __________________________________________ iv Equations relating hydraulic and physiographic Abstract. __________________________________________ 1 factors....________-_______.__-____--__---_-_ 19 Introduction and acknowledgments ___________________ 1 Some relations of hydraulic and physiographic factors to Geographic setting and basic measurements ____________ 2 the longitudinal profile.___________________________ 24 Measurement of hydraulic variables in ephemeral streams, 4 Channel roughness and particle size.______________ 24 General features of flow _________________________ 4 Effect of change of particle size and velocity on Problems of measurement._______________________ 6 stream gradient.____.__._____-_______-____--__ 26 Changes of width, depth, velocity, and load at indi Equilibrium in ephemeral streams _____________________ 28 vidual channel cross sections ___________________ 7 Mutual adjustment of hydraulic factors._____.._._ -
UCLA UCLA Electronic Theses and Dissertations
UCLA UCLA Electronic Theses and Dissertations Title Macroparasite Study of Cypriniform fishes in the Santa Clara Drainage Permalink https://escholarship.org/uc/item/3kp0q16j Author Murray, Max DeLonais Publication Date 2019 Peer reviewed|Thesis/dissertation eScholarship.org Powered by the California Digital Library University of California UNIVERSITY OF CALIFORNIA Los Angeles Macroparasite Study of Cypriniform fishes in the Santa Clara Drainage A thesis submitted in partial satisfaction of the requirements for the degree Master of Science in Biology by Max DeLonais Murray 2019 © Copyrite by Max DeLonais Murray 2019 ABSTRACT OF THE THESIS Macroparasite Study of Cypriniform fishes in the Santa Clara Drainage by Max DeLonais Murray Master of Science in Biology University of California, Los Angeles, 2019 Professor Donald G. Buth, Chair Several species of fishes have been introduced into the Santa Clara River system in southern California, including Catostomus santaanae (Santa Ana sucker), Catostomus fumeiventris (Owens sucker), Gila orcutti (arroyo chub), and Pimephales promelas (fathead minnow). These species are known to inhabit similar ecological niches but little is known about their associated parasite fauna. Two C. fumeiventris, 35 C. santaanae, 63 hybrid catostomids, 214 G. orcutti, and 18 P. promelas were collected and necropsied in the summers of 2017 and 2018. Nine macroparasite taxa were harvested including seven native, and two nonnative parasites Schyzocotyle acheilognathi (Asian fish tapeworm) and Lernaea cyprinacea (anchor worm). Prevalence and intensity of parasites were not related to the genetic history of these catostomids. This is the first host-association record for G. orcutti with Gyrodactylus sp., S. acheilognathi, ii diplostomid metacercariae, Rhabdochona sp, Contracaecum sp., and larval acuariid cysts and for P. -
Floods Floods Are the Most Common Natural Disasters in the Country
Floods Floods are the most common natural disasters in the country. However, not all floods are alike. Some can develop slowly over a long period of rain or during warm weather after a heavy snowfall. Others, such as flash floods, can happen quickly, even without any visible signs of rain. It is important to be prepared for flooding no matter where you live, but especially if you live in a low-lying area, near water or downstream from a dam. Even a very small stream or a dry creek bed can overflow and cause flooding. Prepare supplies Make a Plan Stay informed Prepare an emergency supply kit, Develop a family emergency plan. Know the terms which includes items like non- Your family may not be together in the perishable food, water, battery same place when disaster strikes, so Flash Flood Warning: there has been a sudden flood. Head for operated or crank radio, extra it is important to know how you will flashlights and batteries. Consider contact one another, how to get back higher ground immediately keeping a laptop computer in your together and what you will do in case height. vehicle. The kit should include: of emergency. Flood Warning: there has been Prescriptions Plan places where your family will a flood or will there be a flood Bottled water, a battery radio meet, both within and outside your soon. It is advised to evacuate and extra batteries, a first aid immediate neighborhood. immediately. kit and a flashlight. Copies of important Be sure to take into account the Flood Watch: It is possible that specific needs of family members. -
Sediment Discharge in the Upper Arroyo Grande and Santa Rita Creek Basins 23 5
PB 256 422 Sediment Discharge in the Upper Arroyo Grande and 41,111 anta Rita Creek Basins, tot,:San Luis Obispo County, 1144300,6k California U. S. GEOLOGICAL SURVPFY Water-Resources Investigations 151/4 76-64 101„,14.11kup lemw QE Prepared in cooperation with the 75 .U58w SAN LUIS OBISPO COUNTY no.76-64 1976 ENGINEERING DEPARTMENT lkigtikPHIC DATA I. ReportuNo.Gs 2. 3. Recipient's Accession No. S NRD/WRI-76/053 4. Title and Subtitle 5.keport Date WS14/3610WPOISCHARGE IN THE UPPER ARROYO GRANDE AND SANTA RITA June 1976,/ 6. ben,/ erctFardthf INS, SAN LUIS OBISPO COUNTY, CALIFORNIA (t;"f„ ,, ,/,,,,,,,, °./. Author(s) 8. Performing Organization Rept. .„ J. M. Knott,! N'- USGS/WRI 76-64 9. Performing Organization Name and Address 10. Project/Task/Work Unit No. U.SAeological Survey, Water Resources Division California District )- 11. Contract/Grant No. 345 Middlefield Road Menlo Park, California 94025 12. Sponsoring Organization Name and Address 13. Type of Report & Period U.S. Geological Survey, Water Resources Division Covered California District Final 345 Middlefield Road 14. Menlo Park, California 9409c 15. Supplementary Notes Prepared in cooperation wit igir. .ng Department 16.AbstractsSediment data collected in the upper Arroyo Grande and Santa Rita Creek basins during the 1968-73 water years were analyzed to determine total sediment discharge at four stations in the basins. Water discharge and total sediment discharge at these stations, representative of the 1943-72 period, were estimated from'long-term flow data for nearby gaging stations and water-sediment discharge relations determined for the 1968-73 water years. -
The Central Arroyo Stream Restoration Program
This presentation premiered at WaterSmart Innovations watersmartinnovations.com Breaking Down the Barriers to Generate Sustainable Water Solutions The Arroyo Seco – A Case Study Tim Brick and Eliza Jane Whitman Arroyo Seco Foundation The Arroyo Seco Major tributary of the Los Angeles River Linking downtown LA to the San Gabriel Mountains Home of JPL and the Rose Bowl Watershed Management Program for last ten years Corps Feasibility Study The Historic Arroyo Seco Two different views of the Colorado Street Bridge The Most Celebrated Canyon in Southern California “This arroyo would make one of the greatest parks in the world” - Theodore Roosevelt, 1911 Current Status of the Arroyo Seco Though long celebrated as one of the most beautiful streams in Southern California, the Arroyo Seco has not escaped wide-spread damage caused by human impact Damage Caused by Urbanization / Channelization * destruction of habitat and wildlife * reduced infiltration * impaired water quality Central Arroyo Planning How does a golf course fit into watershed management and restoration? Alternative Alignments for Stream Restoration Celebrating the Arroyo The Central Arroyo Stream Restoration Program Improving the health of a stream and ensuring the future and sustainability of Pasadena The Central Arroyo Brookside Golf Course Project Accomplishments Improved water quality Enhanced trail network Implemented runoff BMPs Restored aquatic habitat Reintroduced the native Arroyo Chub Provided a model of stream restoration for urban SoCal Improved Aquatic Habitat ☼ Created backwater pools and structures to provide resting, foraging, and spawning areas for fish. ☼ Stabilized stream banks ☼ Improvements were constructed with natural materials (native trees and arroyo Backwater pool and stone). woody debris ☼ Under direction of CDFG, reintroduced 300 arroyo chub to the central Arroyo Seco. -
Rationales for Animal Species Considered for Species of Conservation Concern, Sequoia National Forest
Rationales for Animal Species Considered for Species of Conservation Concern Sequoia National Forest Prepared by: Wildlife Biologists and Biologist Planner Regional Office, Sequoia National Forest and Washington Office Enterprise Program For: Sequoia National Forest June 2019 In accordance with Federal civil rights law and U.S. Department of Agriculture (USDA) civil rights regulations and policies, the USDA, its Agencies, offices, and employees, and institutions participating in or administering USDA programs are prohibited from discriminating based on race, color, national origin, religion, sex, gender identity (including gender expression), sexual orientation, disability, age, marital status, family/parental status, income derived from a public assistance program, political beliefs, or reprisal or retaliation for prior civil rights activity, in any program or activity conducted or funded by USDA (not all bases apply to all programs). Remedies and complaint filing deadlines vary by program or incident. Persons with disabilities who require alternative means of communication for program information (e.g., Braille, large print, audiotape, American Sign Language, etc.) should contact the responsible Agency or USDA’s TARGET Center at (202) 720-2600 (voice and TTY) or contact USDA through the Federal Relay Service at (800) 877-8339. Additionally, program information may be made available in languages other than English. To file a program discrimination complaint, complete the USDA Program Discrimination Complaint Form, AD-3027, found online at http://www.ascr.usda.gov/complaint_filing_cust.html and at any USDA office or write a letter addressed to USDA and provide in the letter all of the information requested in the form. To request a copy of the complaint form, call (866) 632-9992. -
Southern Exposures
Searching for the Pliocene: Southern Exposures Robert E. Reynolds, editor California State University Desert Studies Center The 2012 Desert Research Symposium April 2012 Table of contents Searching for the Pliocene: Field trip guide to the southern exposures Field trip day 1 ���������������������������������������������������������������������������������������������������������������������������������������������� 5 Robert E. Reynolds, editor Field trip day 2 �������������������������������������������������������������������������������������������������������������������������������������������� 19 George T. Jefferson, David Lynch, L. K. Murray, and R. E. Reynolds Basin thickness variations at the junction of the Eastern California Shear Zone and the San Bernardino Mountains, California: how thick could the Pliocene section be? ��������������������������������������������������������������� 31 Victoria Langenheim, Tammy L. Surko, Phillip A. Armstrong, Jonathan C. Matti The morphology and anatomy of a Miocene long-runout landslide, Old Dad Mountain, California: implications for rock avalanche mechanics �������������������������������������������������������������������������������������������������� 38 Kim M. Bishop The discovery of the California Blue Mine ��������������������������������������������������������������������������������������������������� 44 Rick Kennedy Geomorphic evolution of the Morongo Valley, California ���������������������������������������������������������������������������� 45 Frank Jordan, Jr. New records -
Flowing Waters, Fruitful Valley a Brief History of Water Development in the Arroyo Seco
Page 1 Flowing Waters, Fruitful Valley A Brief History of Water Development in the Arroyo Seco By Tim Brick Geographically and historically the Arroyo Seco has played an important role in the development of water resources in Southern California. The Natural History Geology divided the Arroyo Seco into three distinct sections with very different hydrologic characteristics: 1) the precipitous upper mountain watershed; 2) the Raymond Basin area including Pasadena and surrounding communities; and 3) the region below the Raymond Dyke in South Pasadena and northeast Los Angeles. • About half the length and area of the Arroyo Seco lies in the upper mountain watershed. This is the front range of the Sierra Madre or San Gabriel Mountains, well known for their harsh conditions. Fierce rainstorms and raging forest fires periodically attack the steep erosion-prone slopes in this relatively small upper watershed (32 square miles) to create the conditions for substantial floods that occasionally roar into the heavily populated communities below. As the Arroyo Seco emerges from the San Gabriel Mountains, its steep descent slows and the waters cut through an alluvial plain. Beneath this region, which includes La Cafiada-Flintridge, Altadena, Pasadena, Sierra Madre and part of Arcadia, lies the Raymond Basin - a massive bowl of alluvial sand and gravel filled with water. The south rim of the basin is the Raymond Dyke, a geological fault that runs from Highland Park to Raymond Hill at Pasadena’s southern boundaiy with South Pasadena and then through San Marino just north of Huntington Drive to Santa Anita Canyon on the east side of Arcadia. -
4.8 Hydrology and Water Quality
Redwood City New General Plan 4.8 Hydrology and Water Quality 4.8 HYDROLOGY AND WATER QUALITY This section discusses surface waters, groundwater resources, storm water collection and transmission, and flooding characteristics in the plan area. Key sources of information for this section include the San Francisco Bay Basin Water Quality Control Plan (Basin Plan) prepared by the San Francisco Bay Regional Water Quality Control Board (January 2007), the Urban Water Management Plan (UWMP) for the City of Redwood City (2005), and the Unified Stream Assessment in Seven Watersheds in San Mateo County, California by the San Mateo Countywide Water Pollution Prevention Program (August 2008), Kennedy/Jenks/Chilton Consulting Engineers Water, Sewer Storm Drainage Master Plan dated 1986, and Winzler & Kelly’s Bayfront Canal Improvement Project Design Development Alternative Analysis, dated December 2003. 4.8.1 ENVIRONMENTAL SETTING Hydrologic Conditions The regional climate of the plan area is typical of the San Francisco Bay Area and is characterized by dry, mild summers and moist, cool winters. Average annual precipitation in the plan area is about 20 inches. About 80 percent of local precipitation falls in the months of November through March. Over the last century for which precipitation records are available, annual precipitation has ranged from an historic low of 8.01 inches in 1976 to an historic high of 42.82 inches in 1983.1 Surface Waters Figure 4.4-1 (in Section 4.4, Biological Resources) depicts surface water bodies in the plan area, which include Redwood and Cordilleras Creeks and their tributaries. Also shown are bay channels, including Westpoint Slough, Corkscrew Slough, northerly reaches of Redwood Creek, Smith Slough and Steinberger Slough, the Atherton Channel (Marsh Creek), and the Bay Front Canal. -
Arroyo Chub Survey Report 2010
Western Riverside County Multiple Species Habitat Conservation Plan (MSHCP) Biological Monitoring Program Arroyo chub (Gila orcutti) Survey Report 2010 23 March 2011 Arroyo Chub Survey Report 2010 TABLE OF CONTENTS INTRODUCTION ...............................................................................................................................................1 GOALS AND OBJECTIVES...............................................................................................................2 METHODS ........................................................................................................................................................2 PROTOCOL DEVELOPMENT............................................................................................................2 PERSONNEL AND TRAINING ..........................................................................................................2 STUDY SITE SELECTION .................................................................................................................3 ESTABLISHING SAMPLING UNITS ..................................................................................................5 SURVEY METHODS .......................................................................................................................5 RESULTS..........................................................................................................................................................6 DISCUSSION .....................................................................................................................................................9