Bay, Oregon, with Notes on Shehfish Temperature, and Physical

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  • The 2014 Golden Gate National Parks Bioblitz - Data Management and the Event Species List Achieving a Quality Dataset from a Large Scale Event

    The 2014 Golden Gate National Parks Bioblitz - Data Management and the Event Species List Achieving a Quality Dataset from a Large Scale Event

    National Park Service U.S. Department of the Interior Natural Resource Stewardship and Science The 2014 Golden Gate National Parks BioBlitz - Data Management and the Event Species List Achieving a Quality Dataset from a Large Scale Event Natural Resource Report NPS/GOGA/NRR—2016/1147 ON THIS PAGE Photograph of BioBlitz participants conducting data entry into iNaturalist. Photograph courtesy of the National Park Service. ON THE COVER Photograph of BioBlitz participants collecting aquatic species data in the Presidio of San Francisco. Photograph courtesy of National Park Service. The 2014 Golden Gate National Parks BioBlitz - Data Management and the Event Species List Achieving a Quality Dataset from a Large Scale Event Natural Resource Report NPS/GOGA/NRR—2016/1147 Elizabeth Edson1, Michelle O’Herron1, Alison Forrestel2, Daniel George3 1Golden Gate Parks Conservancy Building 201 Fort Mason San Francisco, CA 94129 2National Park Service. Golden Gate National Recreation Area Fort Cronkhite, Bldg. 1061 Sausalito, CA 94965 3National Park Service. San Francisco Bay Area Network Inventory & Monitoring Program Manager Fort Cronkhite, Bldg. 1063 Sausalito, CA 94965 March 2016 U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics. These reports are of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Report Series is used to disseminate comprehensive information and analysis about natural resources and related topics concerning lands managed by the National Park Service.
  • Review of Selected California Fisheries for 2013

    Review of Selected California Fisheries for 2013

    FISHERIES REVIEW CalCOFI Rep., Vol. 55, 2014 REVIEW OF SELECTED CALIFORNIA FISHERIES FOR 2013: COASTAL PELAGIC FINFISH, MARKET SQUID, GROUNDFISH, HIGHLY MIGRATORY SPECIES, DUNGENESS CRAB, BASSES, SURFPERCH, ABALONE, KELP AND EDIBLE ALGAE, AND MARINE AQUACULTURE CALIFORNIA DEPARTMENT OF FISH AND WILDLIFE Marine Region 4665 Lampson Ave. Suite C Los Alamitos, CA 90720 [email protected] SUMMARY ings of northern anchovy were 6,005 t with an ex-vessel In 2013, commercial fisheries landed an estimated revenue of greater than $1.0 million. When compared 165,072 metric tons (t) of fish and invertebrates from to landings in 2012, this represents a 141% and 191% California ocean waters (fig. 1). This represents an increase in volume and value, respectively. Nearly all increase of almost 2% from the 162,290 t landed in 2012, (93.6%; 5,621.5 t) of California’s 2013 northern anchovy but still an 11% decrease from the 184,825 t landed catch was landed in the Monterey port area. Landings of in 2011, and a 35% decline from the peak landings of jack mackerel remained relatively low with 892 t landed; 252,568 t observed in 2000. The preliminary ex-vessel however, this represents a 515% increase over 2012 land- economic value of commercial landings in 2013 was ings of 145 t. $254.7 million, increasing once again from the $236 mil- Dungeness crab ranked as California’s second largest lion generated in 2012 (8%), and the $198 million in volume fishery with 14,066 t landed, an increase from 2011 (29%). 11,696 t landed in 2012, and it continued to dominate as Coastal pelagic species (CPS) made up four of the the highest valued fishery in the state with an ex-vessel top five volume fisheries in 2013.
  • DOGAMI TIM-Till-05, Plate 1: Local-Source (Cascadia Subduction Zone) Tsunami Inundation Map for Garibaldi

    DOGAMI TIM-Till-05, Plate 1: Local-Source (Cascadia Subduction Zone) Tsunami Inundation Map for Garibaldi

    STATE OF OREGON Tsunami Inundation Map Till-05 DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES Tsunami Inundation Maps for Garibaldi - Bay City, www.OregonGeology.org Local Source (Cascadia Subduction Zone) Tsunami Inundation Map Tillamook County, Oregon Larry Givens, Governing Board Chair Vicki S. McConnell, Director and State Geologist Plate 1 Don W.T. Lewis, Assistant Director Rachel R. Lyles Smith, Project Operations Manager Garibaldi - Bay City, Oregon Ian P. Madin, Chief Scientist 2012 123°56'0"W 123°54'0"W 123°52'0"W Introduction displacement of the Pacific Ocean, resulting in an increase of the tsunami inundation onshore in Oregon. DOGAMI has also The Oregon Department of Geology and Mineral Industries incorporated physical evidence that suggests that portions of the 200 (DOGAMI) has been identifying and mapping the tsunami inundation coast may drop 4 to 10 feet during the earthquake; this effect is hazard along the Oregon coast since 1994. In Oregon, DOGAMI known as subsidence. Detailed information on fault geometries, 100 manages the National Tsunami Hazard Mitigation Program, which subsidence, computer models, and the methodology used to create has been administered by the National Oceanic and Atmospheric the tsunami scenarios presented on this map can be found in Administration (NOAA) since 1995. DOGAMI’s work is designed to DOGAMI Special Papers 41 (Priest and others, 2009) and 43 (Witter help cities, counties, and other sites in coastal areas reduce the and others, 2011). potential for disastrous tsunami-related consequences by understanding and mitigating this geologic hazard. Using federal Map Explanation funding awarded by NOAA, DOGAMI has developed a new generation of tsunami inundation maps to help residents and visitors along the This tsunami inundation map displays the output of computer entire Oregon coast prepare for the next Cascadia Subduction Zone models representing five selected tsunami scenarios, all of which (CSZ) earthquake and tsunami.
  • Redacted for Privacy Ivan Pratt

    Redacted for Privacy Ivan Pratt

    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by ScholarsArchive@OSU AN ABSTRACT OF THE THESIS OF Alfred Warren Hanson for the Doctor of Philosophy (Name) (Degree) in Zoology presented on/8 1q72 (Major) /71date Title:LIFE CYCLE AND HOST SPECIFICITY OF DICLIDOPHORA sp. (MONOGENEA-DICLIDOPHORIDAE),A PARASITE OF EMBIOTOCID FISHES Abstract approved: Redacted for Privacy Ivan Pratt The life cycle of a monogenean, Diclidophora sp. , was studied with special attention to the time required for developmental stages to occur.Eggs are produced by adult worms at the rate of one every 13. 5 minutes and require 32 days tohatchwhen incubated at 12. 5°C and 30.90/00salinity.Rate of development and hatching success are strongly dependent on incubation temperature and salinity. Growth and development of the larval stages are similar to other known species of the family 1T)c1idophoridae.The presence in the oncomiracidium of a precocious set of attachment clampsand the premature loss of larval hooks distinguish it from related species. Oncorniracidia survive approximately 36 hours if no host fish is reached. Larvae attach to the inner lateral borders of primary lamellae of the host fish gill.A second set of clamps is added before the 36th day, the third set soon after the 44th day, and the last pair by the 58th day.Sexual maturity is reached by the 153rd day after hatching. Experimental infections were maintained on redtail surfperch for 203 days. Naturally infected redtail surfperch, silver surfperch and walleye surfperch were collected.Rates of infection with Di clidoph- ora were 38.
  • On Foot Scampering Over Tree Roots

    On Foot Scampering Over Tree Roots

    5. Netarts/Happy Camp Beaches Safety & Etiquette Netarts has two good beach access points, 7-9 Cape Lookout • Pack it in, pack it out. Cape to Cape with restrooms at both. Just north of the These hikes are longer and more • Keep dogs on leash. village of Netarts, take Happy Camp Road ! strenuous than the other hikes in this • Watch children closely. west down the hill. At the end of the road you guide. Be prepared for muddy sections and • Do not climb cliffs or walk out will find a gravel parking lot near the mouth on Foot scampering over tree roots. Wear good onto rock faces. of Netarts Bay. From the parking lot, you can shoes, carry water, and plan for unpredictable Netarts Area Trails and Beach Walks • Be prepared for sudden walk to the south along the bay or to the changes in weather. Cape Lookout can be weather changes. from Cape Meares to Cape Lookout north with great views of Three Arch Rocks. very windy or become shrouded in fog quickly. This area has strong tidal currents and is • Watch for sneaker waves. unsafe for swimming. Jim Young In Netarts, turn west off the main highway 7. North Trail at Netarts Bay Drive. You will immediately Jim Young see Netarts Bay and the County Boat Ramp North Trail crosses the cape and follows the parking lot. From the lot, walk west about coastline north 2.3 miles (4.6 miles round-trip) 100 yards to the bay beach. A day-use through the shaded forest and down to the parking fee is required.
  • Sediment Accumulation in Tillamook Bay, Oregon: Natural Processes Versus Human Impacts

    Sediment Accumulation in Tillamook Bay, Oregon: Natural Processes Versus Human Impacts

    Sediment Accumulation in Tillamook Bay, Oregon: Natural Processes versus Human Impacts Paul D. Komar, James McManus, and Michael Styllas College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis, Oregon 97331, U.S.A. (e-mail: [email protected]) ABSTRACT Tillamook Bay on the northern Oregon coast has experienced significant sediment accumulation and shoaling. Anal- yses show that part of the increased sedimentation was a result of substantial human impacts in the watersheds of the five rivers that drain into the bay. River discharges were enhanced by approximately 13% during the period 1931– 1954, when commercial logging and a series of devastating forest fires occurred, compared with discharges in the years after reforestation. Potential annual sediment yields calculated from daily discharges were enhanced by 29% during 1931–1954, but actual yields would have been substantially greater as a result of increased erosion rates because of deforestation. Sand transported by the rivers consists primarily of rock fragments, in contrast to the quartz and feldspar sand carried into the bay from the ocean beach. Surface sediments collected throughout the bay consist, on average, of about 40% sand from the rivers and 60% from the ocean beach. Cores show increasing percentages of beach sand beneath the surface, with evidence for major episodic inputs rather than the higher percentages of river- derived rock fragments that human impacts would have produced. Subduction earthquakes have struck the Oregon coast repeatedly during the past several thousand years; the most recent was in January 1700. The down-core increase in beach-derived sand in Tillamook Bay is from sand transport by the tsunami that accompanied the 1700 earthquake and the deepening of the bay from land subsidence at the time of the earthquake, which permitted more frequent and extensive spit overwash events during storms.
  • History of the Siletz This Page Intentionally Left Blank for Printing Purposes

    History of the Siletz This Page Intentionally Left Blank for Printing Purposes

    History of the Siletz This page intentionally left blank for printing purposes. History of the Siletz Historical Perspective The purpose of this section is to discuss the historic difficulties suffered by ancestors of the Confederated Tribes of Siletz Indians (hereinafter Siletz Indians or Indians). It is also to promote understanding of the ongoing effects and circumstances under which the Siletz people struggle today. Since time immemorial, a diverse number of Indian tribes and bands peacefully inhabited what is now the western part of the State of Oregon. The Siletz Tribe includes approximately 30 of these tribes and bands.1 Our aboriginal land base consisted of 20 million acres located from the Columbia to the Klamath River and from the Cascade Range to the Pacific Ocean. The arrival of white settlers in the Oregon Government Hill – Siletz Indian Fair ca. 1917 Territory resulted in violations of the basic principles of constitutional law and federal policy. The 1787 Northwest Ordinance set the policy for treatment of Indian tribes on the frontier. It provided as follows: The utmost good faith shall always be observed toward the Indians; their land and property shall never be taken from them without their consent; and in the property, rights, and liberty, they never shall be invaded, or disturbed, unless in just, and lawful wars authorized by Congress; but laws founded in justice and humanity shall from time to time be made for preventing wrongs being done to them, and for preserving peace, and friendship with them. 5 Data was collected from the Oregon 012.5 255075100 Geospatial Data Clearinghouse.
  • Tillamook Bay Watershed

    Tillamook Bay Watershed

    Tillamook Bay Watershed (Portions extracted from “Tillamook Bay Environmental Characterization: A Scientific and Technical Summary”, Tillamook Bay National Estuary Project, July 1998) WATER QUALITY CONCERNS: The federal Clean Water Act (CWA) requires each state to undertake specific activities to protect the quality of their rivers, estuaries and lakes. DEQ is required to develop and implement water quality standards that protect sensitive beneficial uses of waters throughout Oregon. Section 303(d) of the CWA requires each state to develop a list of waters that do not meet the water quality standards. These are called Water Quality Limited waters. The Tillamook Bay Watershed is Water Quality Limited for Temperature and Bacteria. The number of segments and parameters that exceed water quality standards in the Tillamook Watershed are summarized below. In addition, sedimentation is a parameter of concern throughout the basin and several sloughs in the lower watershed have low dissolved oxygen levels. For more information on streams that are listed in the Tillamook watershed, go to: http://waterquality.deq.state.or.us/WQLData/SubBasinList98.asp. Water Quality Limited Waters in Tillamook (from 1998 303(d) List) Total Number of Water Bodies Listed 20 Parameter Number of Segments Listed Bacteria 15 Temperature 12 Total Maximum Daily Loads: The CWA further requires DEQ to develop Total Maximum Daily Loads (TMDLs) for all water quality limited waters. Generally speaking, TMDLs define the maximum amount of controllable impacts a water body can accept and still assure that designated beneficial uses are being adequately protected. DEQ has developed TMDLs for temperature and bacteria in the Tillamook Bay Watershed.
  • RESULTS of BACTERIA SAMPLING in the WILSON RIVER Joseph M

    RESULTS of BACTERIA SAMPLING in the WILSON RIVER Joseph M

    RESULTS OF BACTERIA SAMPLING IN THE WILSON RIVER Joseph M. Bischoff and Timothy J. Sullivan April 1999 Report Number 97-16-02 E&S Environmental Chemistry, Inc. P.O. Box 609 Corvallis, OR 97339 ABSTRACT Water quality monitoring was conducted at eight sites on the Wilson River during the period late September, 1997 through early March, 1998, from river mile 8.6 to river mile 0.2 near where the river enters Tillamook Bay. Samples were collected approximately weekly by the Tillamook County Creamery Association (TCCA) during the course of the study, plus at more frequent intervals during two storm events in October, 1997 and March, 1998. Samples were analyzed by TCCA for fecal coliform bacteria (FCB) and E. coli. E&S Environmental Chemistry, Inc. provided the data analysis and presentation for this report. FCB concentrations and loads in the Wilson River were higher by a factor of two during the October, 1997 storm than during any of the other five storms monitored by TCCA or E&S. Similar results were found for the Tillamook and Trask Rivers by Sullivan et al. (1998b). Lowest loads in the Wilson River were found during the monitored spring storms in 1997 (by E&S) and 1998 (this study). By far the highest FCB loads were contributed by the land areas that drain into Site 7 (in the mixing zone just below the TCCA outfall) during the October 1997 and March 1998 storms. This site was the only site in the Wilson River basin that has contributing areas occupied by urban land use. Relatively high FCB loads were also found at a variety of other sites.
  • (J3+5Q I-’ /Fq.057 I I SENSITIVITY of COASTAL ENVIRONMENTS and WILDLIFE to SPILLED OIL ALAS KA - SHELIKOF STRAIT REGION

    (J3+5Q I-’ /Fq.057 I I SENSITIVITY of COASTAL ENVIRONMENTS and WILDLIFE to SPILLED OIL ALAS KA - SHELIKOF STRAIT REGION

    i (J3+5q i-’ /fq.057 I I SENSITIVITY OF COASTAL ENVIRONMENTS AND WILDLIFE TO SPILLED OIL ALAS KA - SHELIKOF STRAIT REGION - Daniel D. Domeracki, Larry C. Thebeau, Charles D. Getter, James L. Sadd, and Christopher H. Ruby Research Planning Institute, Inc. Miles O. Hayes, President 925 Gervais Street Columbia, South Carolina 29201 - with contributions from - Dave Maiero Science Applications, Inc. and Dennis Lees - Dames and Moore PREPARED FOR: National Oceanic and Atmospheric Administration Outer Continental Shelf Environmental Assessment Program Juneau, Alaska RPI/R/81/2/10-4 Contract No. NA80RACO0154 February 1981 .i i . i ~hou~d read: 11; Caption !s Page 26, Figure four distinct biO1~~~cal rocky shore show~ng algae 2oner and P Exposed (1) barnacle (Balanus glandula) zone, zones: (3) -and ~~~e. blue mussel zone, ~ar-OSUsJ (4) barnacle ~B_ - . 27 -.--d. 29 ..-.A =~na beaches . 31 fixposed tidal flats (low biomass) . 33 Mixed sand and gravel beaches . 35 Gravel beaches . 37 Exposed tidal flats (moderate biomass) . 39 Sheltered rocky shores . ...*.. 41 Sheltered tidal flats . 43 Marshes ● =*...*. 45 Critical Species and Habitats . 47 Marine Mammals . ...*. 48 Coastal Marine Birds. 50 Finish . ...*.. 54 Shellfish . ...**.. ● *...... ...*.. ..* 56 Critical Intertidal Habitats . 58 Salt Marshes . 58 Sheltered Tidal Flats. 59 Sheltered Rocky Shores . 59 Critical Subtidal Habitats . 60 Nearshore Subtidal Habitats . ...*.. 60 Seagrass Beds . ...* ● . 62 Kelp Beds ● . ...**. ● .*...*. ...* . 63 ● . TABLE OF CONTENTS (continued) PAGE Discussion of Habitats with Variable to Slight Sensitivity. ...*..... 65 Introduction . 65 Exposed Rocky Shores. 65 Beaches . ● . 66 Exposed Tidal Flats.. 67 Areas of Socioeconomic Importance . 68 Mining Claims . 68 Private Property ● . 69 Public Property . ...*.. 69 Archaeological Sites.
  • CASCADE HEAD: Fish Species Present Within Evaluation Area

    CASCADE HEAD: Fish Species Present Within Evaluation Area

    CASCADE HEAD: Fish species present within evaluation area EXTENT OF USE: C = Common, M = Minor, R = Rare or incidential use HABITAT: S = Sand, G = Gravel, R = Rock, P = Pelagic, I = Rocky intertidal HARVEST: C = Commercial, R = Recreational NAME USE HABITAT HARVEST Black Rockfish C R C, R Blue Rockfish CR Canary Rockfish CR China Rockfish CR Copper Rockfish CR Juvenile Rockfish spp. C R Quillback Rockfish CR Vermilion Rockfish R Yelloweye Rockfish (juveniles) CR Cabezon CR Red Irish Lord R Sculpin spp. C R, I Chinook Salmon P C, R Coho Salmon P C, R Steelhead P Green Sturgeon P White Sturgeon P Kelp Greenling CR Lingcod CR Rock Greenling R Monkeyface Prickleback R, I Prickleback spp. Sanddab S Pacific Halibut Starry Flounder Poacher spp. Redtail Surfperch S Shiner Surfperch S Striped Surfperch R Walleye Surfperch S Surfperch spp. Gunnel spp. Smelts spp. P Topsmelt Tubesnout Wolf Eel R Cascade Head: Fish Page 1 of 4 NAME USE HABITAT HARVEST Spiny Dogfish P Salmon Shark P White Shark P Leopard Shark Blue Shark P Pacific Angel Shark Big Skate Cascade Head: Fish Page 2 of 4 CASCADE HEAD: Invertebrate & algal species present within evaluation area EXTENT OF USE: C = Common, M = Minor, R = Rare or incidential use HABITAT: S = Sand, G = Gravel, R = Rock, P = Pelagic, I = Rocky intertidal HARVEST: C = Commercial, R = Recreational NAME USE HABITAT HARVEST Coonstripe Shrimp Brown Rock Crab Dungeness Crab C S, GC Mole Crab S Red Rock Crab S Striped Shore Crab Gooseneck Barnacle I Barnacle spp. California Mussel IR Cockle Clam S Scallop spp.
  • Marine Mammals of the Columbia River Estuary

    Marine Mammals of the Columbia River Estuary

    Marine mammals of the Columbia River estuary Item Type monograph Authors Jeffries, Steven Publisher Washington Department of Game Download date 01/10/2021 09:29:55 Link to Item http://hdl.handle.net/1834/40552 NOAA LISD SEA LE MARINE MAMMALS OF THE COLUMBIA RIVER ESTUARY I QH 541.5 ==============:::!J • E8 M35 cop.2 [I D 0 [] Final Report on the Marine Mammals Work Unit of the Columbia River Estuary Data Development Program tl MARINE MAMMALS n OF THE u COLUMBIA RIVER ESTUARY ] [] D Contractor: Washington Department of Game 600 N. Capitol Way Olympia, Washington 98504 Principal Investigator: [l Steven Jeffries Washington Department of Game Marine Mammal Investigations ] 53 Portway Street Astoria, Oregon 97103 (503) 325-8241 [l n i . Lj January 1984 ] D ] 7 ~I ,----- • __ J ,----- ,----- D D 0 D WASHINGTON DEPARTMENT OF GAME □ MARINE MAMMAL INVESTIGATIONS D PROJECT LEADER ~ Steven J. Jeffries □ WILDLIFE BIOLOGIST RESEARCH ANALYST Stephen D. Treacy Anne C. Geiger TYPIST Lynda Stansberry WORD PROCESSING Elizabeth Rummell [] lJ u [] iii J J J J J J ] J ] ] J J J J .J .J □ D D PREFACE The Columbia River Estuary Data Development Program This document is one of a set of publications and other materials [1 produced by the Columbia River Estuary, Data Development Program (CREDDP). CREDDP has two purposes: to increase understanding of the ecology of the Columbia River Estuary and to provide information useful J in making land and water use decisions. The program was initiated by local governments and citizens who saw a need for a better information base for use in managing natural resources and in planning for development.