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D.W. ALLEY & Associates Aquatic Biology
D.W. ALLEY & Associates Aquatic Biology -------------------------------------------------------------------------- 2006 Juvenile Steelhead Densities in the San Lorenzo, Soquel, Aptos and Corralitos Watersheds, Santa Cruz County, California Coastrange Sculpin Photographed by Jessica Wheeler D.W. ALLEY & Associates, Aquatic Biology Don Alley, Chad Steiner and Jerry Smith, Fishery Biologists With Field Assistance from Kristen Kittleson, Dawn Reis and Jessica Wheeler Prepared For the Santa Cruz County Environmental Health Department Government Center, 701 Ocean Street, Room 312, Santa Cruz, CA 95060 Funding From the San Lorenzo Valley Water District, Soquel Creek Water District, Lompico County Water District, Cities of Santa Cruz and Watsonville and the County of Santa Cruz May 2007 Project # 200-04 340 Old River Lane • P.O. Box 200 • Brookdale, California 95007 • (831) 338-7971 TABLE OF CONTENTS REPORT SUMMARY...................................................................................10 INTRODUCTION..........................................................................................31 I-1. Steelhead and Coho Salmon Ecology...................................................... 31 I-3. Project Purpose and General Study Approach ........................................ 34 METHODS ....................................................................................................35 M-1. Choice of Reaches and Vicinity of Sites to be Sampled- Methods........... 35 M-2. Classification of Habitat Types and Measurement of Habitat Characteristics............................................................................................. -
City of Merced Town Hall Goals & Priorities Survey 504 Total
City of Merced Town Hall Goals & Priorities Survey 504 Total Responses 24:27 Average time to complete 1. Full Name - 471 Responses 2. Email address - 454 Responses 3. Phone Number – 428 Responses 4. Home Address – 426 Responses 5. Your City District District 1 41 District 2 23 District 3 50 District 4 99 District 5 50 District 6 111 Outside City Limits 32 Not Sure 62 6. The Merced City Council develops Goals & Priorities annually to guide budget development. Please indicate for each of the City of Merced's current Goals & Priorities it's importance to you from "Not At All Important" to "Very Important" Not At All Important Somewhat Important Important Fairly Important Very Important No Opinion Staffing Youth Programs City Beautification Local Streets Future Planning Economic Development Downtown Regional Transportation Sustainability Housing/Homelessness Community Wellness Agency Partnerships 7. City Staffing is tied directly to providing services to the community. Please indicate importance of fulfilling each service area staffing needs from "Not At All Important" to "Very Important". Not At All Important Somewhat Important Important Fairly Important Very Important No Opinion Police Department Code Enforcement Fire Department Parks and Greenspace Maintenance Street Improvements & Lighting Refuse Collection Water & Sewer Services Building Permits & Construction Parks & Recreation Services Economic Development (business & industrial) Airport Services Planning Services (code updates, entitlements) Affordable Housing Public Art Applegate Zoo 8. Parks & Recreation provides services to youth and adults within Merced. Please rank the current services provided by order of importance to you. Rank Options First choice Last choice 1. Family-friendly Events 2. Recreation Activities for children 5-12 3. -
New Empirical Relationships Among Magnitude, Rupture Length, Rupture Width, Rupture Area, and Surface Displacement
Bulletin of the Seismological Society of America, Vol. 84, No. 4, pp. 974-1002, August 1994 New Empirical Relationships among Magnitude, Rupture Length, Rupture Width, Rupture Area, and Surface Displacement by Donald L. Wells and Kevin J. Coppersmith Abstract Source parameters for historical earthquakes worldwide are com piled to develop a series of empirical relationships among moment magnitude (M), surface rupture length, subsurface rupture length, downdip rupture width, rupture area, and maximum and average displacement per event. The resulting data base is a significant update of previous compilations and includes the ad ditional source parameters of seismic moment, moment magnitude, subsurface rupture length, downdip rupture width, and average surface displacement. Each source parameter is classified as reliable or unreliable, based on our evaluation of the accuracy of individual values. Only the reliable source parameters are used in the final analyses. In comparing source parameters, we note the fol lowing trends: (1) Generally, the length of rupture at the surface is equal to 75% of the subsurface rupture length; however, the ratio of surface rupture length to subsurface rupture length increases with magnitude; (2) the average surface dis placement per event is about one-half the maximum surface displacement per event; and (3) the average subsurface displacement on the fault plane is less than the maximum surface displacement but more than the average surface dis placement. Thus, for most earthquakes in this data base, slip on the fault plane at seismogenic depths is manifested by similar displacements at the surface. Log-linear regressions between earthquake magnitude and surface rupture length, subsurface rupture length, and rupture area are especially well correlated, show ing standard deviations of 0.25 to 0.35 magnitude units. -
Infogroup Business Listing File
Infogroup Business Listing File Company location: Omaha, Nebraska Web address: www.infousa.com Description: Infogroup collects information on approximately 11 million private and public US companies. Individual businesses are located by address geocoding—not all will have an exact location. The Esri geocoder integrates an address-based approach with more than eighty-one million residential and commercial U.S. address records from the NAVTEQ Point Addressing database. This database maps street addresses to a physical location so each address is a fixed point and not an interpolation from an address range. The geocoder uses address locators in a cascading fallback approach to ensure a match for as many records as possible. The primary locator utilizes the NAVTEQ Point Addressing database. The secondary locator utilizes the NAVTEQ Street Address Range database. Records that did not match fall back to the geocode provided by Infogroup. Businesses can be retrieved by their Standard Industrial Classification Code (SIC) as well as by North American Industry Classification System (NAICS) Code and Location. The Infogroup Business File can be used for locating both competitors and marketing opportunities. This data is current as of July 2011. Fields: Note: Using the Identify a Business tool , click on a business in your map area to see these fields for an individual business. Fields marked in blue below are not visible in the business layer attribute table or exportable from Business Analyst. Company Name (Actual field name=CONAME) – The legal, incorporated business name. Example: ESRI, AT&T, IBM. Address – Physical address of location. The address field cannot be used for direct mailing purposes. -
Earthquake Myths
EARTHQUAKE MYTHS FICTION: California will fall into the ocean. FACT: The ocean is not a great hole into which California can fall, but it is itself land at a somewhat lower elevation with water above it. It’s absolutely impossible that California will be swept out to sea. Instead, southwestern California is moving horizontally northward towards Alaska as it slides past central and eastern California. The dividing point is the San Andreas fault system, which extends from the Salton Sea in the south to Cape Mendocino in the north. This 800 mile long fault is the boundary between the Pacific Plate and North American Plate. The Pacific Plate is moving to the northwest with respect to the North American Plate at approximately two inches per year (the rate your fingernails grow). At this rate, Los Angeles and San Francisco will one day (about 15 million years from now) be next-door neighbors, and in an additional 70 million years, Los Angeles residents will find themselves with an Alaska zip code! FACT VS. FICTION FICTION: It’s been raining a lot, or very hot--it must be earthquake weather! FACT: Many people believe that earthquakes are more common in certain kinds of weather. In fact, no correlation with weather has been found. Earthquakes begin many kilometers (miles) below the region affected by surface weather. People tend to notice earthquakes that fit the pattern and forget the ones that FICTION: During an earthquake you should head for the don't. doorway. FICTION: My house will be swallowed up during an FACT: That’s outdated advice. -
Water Commission Agenda Regular Meeting 7:00 P.M
Water Commission Agenda Regular Meeting 7:00 p.m. – Monday, November 4, 2013 Council Chambers 809 Center Street, Santa Cruz Agenda Call to Order Roll Call Presentation Organized groups may make presentations to the Water Commission. Presenta- tions that require more than three minutes should be scheduled in advance with Water Depart- ment staff. Statements of Disqualification Section 607 of the City Charter states that “…All members pre- sent at any meeting must vote unless disqualified, in which case the disqualification shall be publicly declared and a record thereof made.” The City of Santa Cruz has adopted a Conflict of Interest Code, and Section 8 of that Code states that no person shall make or participate in a governmental decision which he or she knows or has reason to know will have a reasonably foreseeable material financial effect distinguishable from its effect on the public generally. Oral Communications No action shall be taken on this item. Announcements No action shall be taken on this item. Approval of Minutes (Pages 4-8) Recommendation: Motion to approve the October 7, 2013 Water Commission Minutes. Consent Agenda (Pages 9-11) Items on the consent agenda are considered to be routine in nature and will be acted upon in one motion. Specific items may be removed by members of the advisory body or public for separate consideration and discussion. 1. Three-month Calendar (accept info) (Page 9) 2. City Council Items Affecting Water (accept info) (Pages 10-11) Items Removed from the Consent Agenda General Business (Page 12) Any document related to an agenda item for the General Business of this meeting distributed to the Water Commission less than 72 hours before this meeting is available for inspection at the Water Administration Office, 212 Locust Street, Suite A, Santa Cruz, California. -
Geodetic Constraints on San Francisco Bay Area Fault Slip Rates and Potential Seismogenic Asperities on the Partially Creeping Hayward Fault Eileen L
Masthead Logo Smith ScholarWorks Geosciences: Faculty Publications Geosciences 3-2012 Geodetic Constraints on San Francisco Bay Area Fault Slip Rates and Potential Seismogenic Asperities on the Partially Creeping Hayward Fault Eileen L. Evans Harvard University John P. Loveless Harvard University, [email protected] Brendan J. Meade Harvard University Follow this and additional works at: https://scholarworks.smith.edu/geo_facpubs Part of the Geology Commons Recommended Citation Evans, Eileen L.; Loveless, John P.; and Meade, Brendan J., "Geodetic Constraints on San Francisco Bay Area Fault Slip Rates and Potential Seismogenic Asperities on the Partially Creeping Hayward Fault" (2012). Geosciences: Faculty Publications, Smith College, Northampton, MA. https://scholarworks.smith.edu/geo_facpubs/21 This Article has been accepted for inclusion in Geosciences: Faculty Publications by an authorized administrator of Smith ScholarWorks. For more information, please contact [email protected] JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 117, B03410, doi:10.1029/2011JB008398, 2012 Geodetic constraints on San Francisco Bay Area fault slip rates and potential seismogenic asperities on the partially creeping Hayward fault Eileen L. Evans,1 John P. Loveless,1,2 and Brendan J. Meade1 Received 28 March 2011; revised 17 November 2011; accepted 31 January 2012; published 31 March 2012. [1] The Hayward fault in the San Francisco Bay Area (SFBA) is sometimes considered unusual among continental faults for exhibiting significant aseismic creep during the interseismic phase of the seismic cycle while also generating sufficient elastic strain to produce major earthquakes. Imaging the spatial variation in interseismic fault creep on the Hayward fault is complicated because of the interseismic strain accumulation associated with nearby faults in the SFBA, where the relative motion between the Pacific plate and the Sierra block is partitioned across closely spaced subparallel faults. -
Earthquake Weather: Where Grief and Memory Collide
EARTHQUAKE WEATHER: WHERE GRIEF AND MEMORY COLLIDE ELLA H. This work explores the relationship between grief and memory in my own life. In my research, I looked into earthquakes and compared the geological change that they cause to personal change in my life as a result of loss. To me, earthquakes feel like an appropriate metaphor for loss because, while they are destructive, they shape our world. Their unpredictability also mirrors the unpredictability of loss. As a San Franciscan, I’ve been taught to be prepared for disaster, even though we don’t know exactly when it will strike. During my sophomore year of high-school, my best friend died after a year and a half long battle with cancer. Within the last month of her life, I knew that she was close to death, although I didn’t know when it would happen. In my art, I aimed to create a piece to represent some of my memories of her, while also expressing the instability of not knowing when loss would occur. My art focuses on a specific memory that took place in my best friend’s old backyard. I recently returned there and sat on her rope-swing from our childhood. Although the yard was empty, I could clearly picture younger versions of ourselves, as well as other various memories associated with the place. I recreated the swing to physically recreate my present perspective; I intend for the swing to create a sense of instability for the viewer. I painted clouds in oil on a large-scale canvas and collaged charcoal drawings that represent memories from the backyard onto it. -
Castle Rock State Park 15000 Skyline Boulevard Los Gatos, CA 95030 (408) 867-2952
Our Mission The mission of California State Parks is to provide for the health, inspiration and xquisite sandstone Castle Rock education of the people of California by helping E to preserve the state’s extraordinary biological State Park diversity, protecting its most valued natural and formations and cultural resources, and creating opportunities for high-quality outdoor recreation. sculpted caves are among the treasured features within this California State Parks supports equal access. park’s vast wilderness. Prior to arrival, visitors with disabilities who need assistance should contact the park at (408) 867-2952. If you need this publication in an alternate format, contact [email protected]. CALIFORNIA STATE PARKS P.O. Box 942896 Sacramento, CA 94296-0001 For information call: (800) 777-0369 (916) 653-6995, outside the U.S. 711, TTY relay service www.parks.ca.gov SaveTheRedwoods.org/csp Castle Rock State Park 15000 Skyline Boulevard Los Gatos, CA 95030 (408) 867-2952 © 2011 California State Parks (Rev. 2017) C astle Rock State Park is a place of The Smead and Partridge farms were abundant solitude, wilderness, high cliffs, the largest operations on the ridge, with and sweeping vistas. Unique patterns on orchards of apples, pears, walnuts, and weathered sandstone, lush forests, and grapes. Near the park’s interpretive shelter, stream-fed canyons make up the park’s heritage trees planted in the early 1900s diverse features. still bear fruit. From one of the highest ridges in the Creation of the Park Santa Cruz Mountains, visitors enjoy Judge Joseph Welch of Santa Clara Valley panoramic views of Monterey Bay. -
4.5 Cultural Resources
Monterey Bay Sanctuary Scenic Trail Network Master Plan EIR Section 4.5 Cultural Resources 4.5 CULTURAL RESOURCES 4.5.1 Setting a. Environmental Setting. The Master Plan corridor stretches the entire length of Santa Cruz County from the San Mateo County line north of Davenport to Railroad Avenue in Monterey County. The corridor primarily aligns with the Santa Cruz Branch Rail Line right-of- way, a 32-mile, continuous travel corridor. The RTC now owns 31-miles of the Santa Cruz Branch Rail Lineis now owned by the RTC. The rail right-of-way would serve both rail service and bike/pedestrian trail functions. b. Historical Background. Prehistory. Santa Cruz County is in the Monterey Bay Area, a cultural-historical geographic region which spans the central California coastline from Big Sur northward to just south of the San Francisco Bay. This region generally corresponds to southern Costanoan language groups. The prehistory of the Monterey Bay Area is categorized according to temporal “periods,” which refer to the general social, economic, and environmental adaptations of Native California populations during a given time in prehistory. David A. Fredrickson’s Paleo-Archaic-Emergent cultural sequence (1974) is commonly used to interpret the prehistoric occupation of Central California and is broken into three broad periods: the Paleoindian Period (10,000-6000 B.C.); the three-staged Archaic Period, consisting of the Lower Archaic (6000-3000 B.C.), Middle Archaic (3000-500 B.C.), and Upper Archaic (500 B.C.-A.D. 1000); and the Emergent Period (A.D. 1000- 1800). T. Jones’ (1993) updated period sequence, which integrates data from the central California coast, consists of the Paleoindian (9000-6500 B.C.), Millingstone (6500-3500 B.C.), Early (3500-1000 B.C.), Early/Middle Transition (1000-600 B.C.), Middle (600 B.C.-A.D. -
History of Black Powder the Following Is Adapted from "A Chronology of Black Powder" by Richard D Frantz
History of Black Powder The following is adapted from "A chronology of Black Powder" by Richard D Frantz (Reference: http://footguards.tripod.com/06ARTICLES/ART28_blackpowder.htm) About Black Powder Black Powder is a mixture of three components: Potassium Nitrate ( KNO3 or saltpeter/saltpetre, or nitre/niter). Sulphur/sulphur . Charcoal. Ignition brings about a rapid reaction in which a group of gases is generated, and energy, in the form of heat, is liberated. The heating causes the gases to expand rapidly, producing an explosive force, especially if confined. The faster the reaction, the more powerful is the effectiveness. If this process is fully enclosed, we have a bomb. When the internal pressure exceeds the container's ability to contain it, we have an explosion. If the container has a vent, such as the open end of a gun barrel, the expanding gases may be used to propel a missile up its length. The length of barrel allows the process to sustain a major portion of the initial pressure, while the inertia of the missile is continually overcome. The missile continues to accelerate until it leaves the barrel, at which time, the effects of air resistance, and to a smaller effect, gravity, cause it to decelerate at predictable rates. Black Powder is classified as an explosive. This is because its actions after ignition meet some arbitrary criteria that takes it beyond the sense of "burning" - a slower reaction such as the burning of wood. Black Powder will indeed explode with considerable force if ignited when uncontained. In mining, it was often poured down cracks or into drilled holes to blast apart rock. -
City of Watsonville Historic Context Statement (2007)
Historic Context Statement for the City of Watsonville FINAL REPORT Watsonville, California April 2007 Prepared by One Sutter Street Suite 910 San Francisco CA 94104 415.362.7711 ph 415.391.9647 fx Acknowledgements The Historic Context Statement for the City of Watsonville would not have been possible without the coordinated efforts of the City of Watsonville Associate Planner Suzi Aratin, and local historians and volunteers Ann Jenkins and Jane Borg whose vast knowledge and appreciation of Watsonville is paramount. Their work was tireless and dependable, and their company more than pleasant. In addition to hours of research, fact checking and editing their joint effort has become a model for other communities developing a historic context statement. We would like to thank the City of Watsonville Council members and Planning Commission members for supporting the Historic Context Statement project. It is a testimony to their appreciation and protection of local history. Thanks to all of you. Table of Contents Chapter Page 1.0 Background and Objectives 1 1.1 Introduction 1.2 Location and Boundaries of Study 1.3 Context Statement Objective 2.0 Methodology 5 2.1 Context Statement Methodology 2.2 Summary of Resources 3.0 Introduction to Historic Contexts 7 3.1 Summary of Historic Contexts 3.2 Summary of Regional History Before Incorporation 3.3 Summary of regional history from 1868 – 1960 4.0 Historic Context 1 - Municipal Development 17 4.1 Overview 4.2 History 4.2.1 Schools 4.2.2 Civic Institutions 4.2.3 Infrastructure: Water 4.2.4 Infrastructure: