Columbia River Estuary Land and Water Use Section
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CLATSOP COUNTY Scale in Mlles
CLATSOP COUNTY Scale In Mlles 81 8 I A 0,6 O 6 Secmide 0 10 6 7 WASV INGTON T I L LAMOOK COUNTY CO Clatsop County Knappa Prairie U. S. Army Fort Stevens, Ruth C. Bishop Dean H. Byrd (1992) Janice M. Healy (1952) Oregon Burial Site Guide Clatsop County Area: 873 square miles Population (1998): 35,424 County seat: Astoria, Population: 10,130 County established: 22 June 1844 Located on the south bank of the lower Columbia River where it enters the Pacific Ocean. Clatsop County was the site of the first white trading post in Oregon and therefore the earliest established cemetery. This was Fort Astoria founded in the spring of 1811 for the fur trade. It was occupied by the British in the fall of I 813 during the War of 1812 and was renamed Fort George. Returned to the Americans in 1818 and once again called Fort Astoria, the name was gradually transferred to a small civilian settlement as Astoria. The earliest burials after 1811 and those dating from the 1850's to about 1878 are now built over. Eventually most of Astoria's known burials were transferred to Ocean View which was established in 1872. The Clatsop Plains Pioneer Cemetery was begun in 1846 and is the earliest organized cemetery outside of Astoria. By the 1870's there were at least four other organized cemeteries. There were many family burial sites and still some Indian burials sites and a United States Military cemetery begun as early as 1868 at Fort Stevens. The most prominent ethnic nationalities from Europe were Finns and Swedes who are scattered through many cemeteries and family burial sites. -
Tidal Hydrodynamic Response to Sea Level Rise and Coastal Geomorphology in the Northern Gulf of Mexico
University of Central Florida STARS Electronic Theses and Dissertations, 2004-2019 2015 Tidal hydrodynamic response to sea level rise and coastal geomorphology in the Northern Gulf of Mexico Davina Passeri University of Central Florida Part of the Civil Engineering Commons Find similar works at: https://stars.library.ucf.edu/etd University of Central Florida Libraries http://library.ucf.edu This Doctoral Dissertation (Open Access) is brought to you for free and open access by STARS. It has been accepted for inclusion in Electronic Theses and Dissertations, 2004-2019 by an authorized administrator of STARS. For more information, please contact [email protected]. STARS Citation Passeri, Davina, "Tidal hydrodynamic response to sea level rise and coastal geomorphology in the Northern Gulf of Mexico" (2015). Electronic Theses and Dissertations, 2004-2019. 1429. https://stars.library.ucf.edu/etd/1429 TIDAL HYDRODYNAMIC RESPONSE TO SEA LEVEL RISE AND COASTAL GEOMORPHOLOGY IN THE NORTHERN GULF OF MEXICO by DAVINA LISA PASSERI B.S. University of Notre Dame, 2010 A thesis submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the Department of Civil, Environmental, and Construction Engineering in the College of Engineering and Computer Science at the University of Central Florida Orlando, Florida Spring Term 2015 Major Professor: Scott C. Hagen © 2015 Davina Lisa Passeri ii ABSTRACT Sea level rise (SLR) has the potential to affect coastal environments in a multitude of ways, including submergence, increased flooding, and increased shoreline erosion. Low-lying coastal environments such as the Northern Gulf of Mexico (NGOM) are particularly vulnerable to the effects of SLR, which may have serious consequences for coastal communities as well as ecologically and economically significant estuaries. -
Tide Simplified by Phil Clegg Sea Kayaking Anglesey
Tide Simplified By Phil Clegg Sea Kayaking Anglesey Tide is one of those areas that the more you learn about it, the more you realise you don’t know. As sea kayakers, and not necessarily scientists, we don’t have to know every detail but a simplified understanding can help us to understand and predict what we might expect to see when we are out on the water. In this article we look at the areas of tide you need to know about without having to look it up in a book. Causes of tides To understand tide is convenient to imagine the earth with an envelope of water all around it, spinning once every 24 hours on its north-south axis with the moon on a line parallel to the equator. Moon Gravity A B Earth Ocean C The tides are primarily caused by the gravitational attraction of the moon. Simplifying a bit, at point A the gravitational pull is the strongest causing a high tide, point B experiences a medium pull towards the moon, while point C has the weakest pull causing a second high tide. Because the earth spins once every 24 hours, at any location on its surface there are two high tides and two low tides a day. There are approximately six hours between high tide and low tide. One way of predicting the approximate time of high tide is to add 50 minutes to the high tide of the previous day. The sun has a similar but weaker gravitational effect on the tides. On average this is about 40 percent of that of the moon. -
Chapter 5 Water Levels and Flow
253 CHAPTER 5 WATER LEVELS AND FLOW 1. INTRODUCTION The purpose of this chapter is to provide the hydrographer and technical reader the fundamental information required to understand and apply water levels, derived water level products and datums, and water currents to carry out field operations in support of hydrographic surveying and mapping activities. The hydrographer is concerned not only with the elevation of the sea surface, which is affected significantly by tides, but also with the elevation of lake and river surfaces, where tidal phenomena may have little effect. The term ‘tide’ is traditionally accepted and widely used by hydrographers in connection with the instrumentation used to measure the elevation of the water surface, though the term ‘water level’ would be more technically correct. The term ‘current’ similarly is accepted in many areas in connection with tidal currents; however water currents are greatly affected by much more than the tide producing forces. The term ‘flow’ is often used instead of currents. Tidal forces play such a significant role in completing most hydrographic surveys that tide producing forces and fundamental tidal variations are only described in general with appropriate technical references in this chapter. It is important for the hydrographer to understand why tide, water level and water current characteristics vary both over time and spatially so that they are taken fully into account for survey planning and operations which will lead to successful production of accurate surveys and charts. Because procedures and approaches to measuring and applying water levels, tides and currents vary depending upon the country, this chapter covers general principles using documented examples as appropriate for illustration. -
Source Water Assessment Report
Source Water Assessment Report Youngs River-Lewis & Clarl( Water District, Oregon PWS #4100062 December 11, 2000 Prepared for Youngs River-Lewis & Clark Water District Prepared by � rt: I •1 =<•1 Stale of Oregon Departmentof Environmental Quality Water Quality Division Drinking Water Protection Program Department of Human Services Oregon Health Division Drinking Water Program Department of Environmental Quality regon 811 SW Sixth Avenue Portland, OR 97204-1390 John A. Kitzhaber, ivf.D.,Governor (503) 229-5696 TDD (503) 229-6993 December 11, 2000 Mr. Ric Saavedra - Superintendent Youngs River-Lewis & Clark Water District 810 US Highway IOI Astoria, OR 97013 RE: Source Water Assessment Report Youngs River-Lewis & Clark Water District PWS # 4100062 Dear Mr. Saavedra: Enclosed is Youngs River-Lewis & Clark Water District's Water Assessment Report. The assessment was prepared under the requirements and guidance of the Federal Safe Drinking Water Act and the US Environmental Protection Agency, as well as a detailed Source Water Assessment Plan developed by a statewide citizen's advisory committee here in Oregon over the past two years. The Department of Environmental Quality (DEQ) and the Oregon Health Division (OHD) are conducting the assessments for all public water systems in Oregon. The purpose is to provide information so that the public water system staff/operator, consumers, and community citizens can begin developing strategies to protect your source of drinking water. As you know, the 1996 Amendments to the SafeDrinking Water Act requires Consumer ConfidenceReports (CCR) by community water systems. CCRs include information about the quality of the drinking water, the source of the drinking water, and a summary of the source water assessment. -
Warrenton Mooring Basin
eetion Page ref ace ................... .. ...................................................................................................................VIII ..................... .............................................................................. 1-1 Plans and Policies .............................................................................................................. 1-3 Federal .......................................*..*... ........................................................................1-3 O'P .............................................................................................................. 1-3 Su~lsetEmpire Transit District ............................................................................... 1-4 Clatsop County ........................................................................................................ 1-4 City ...............................................................................................................................1-4 Public Involvement .............................................................................................................."14 1PuL.a~s ,.) .- * and Obje&ves ...................................... ..................... ..............1-5 Goal l .. hlobillty .............................. .....................................................................3-5 Coal 2: Livabilitv ................................................................................................ 1-6 Goal 3: Coordination ................................................................................................1-6 -
Chapter 9 Tides and Tidal Currents
CHAPTER 9 TIDES AND TIDAL CURRENTS ORIGINS OF TIDES 900. Introduction superimposed upon non-tidal currents such as normal river flows, floods, and freshets. Tides are the periodic motion of the waters of the sea due to changes in the attractive forces of the Moon and Sun 902. Causes of Tides upon the rotating Earth. Tides can either help or hinder a mariner. A high tide may provide enough depth to clear a The principal tidal forces are generated by the Moon bar, while a low tide may prevent entering or leaving a and Sun. The Moon is the main tide-generating body. Due harbor. Tidal current may help progress or hinder it, may set to its greater distance, the Sun’s effect is only 46 percent of the ship toward dangers or away from them. By the Moon’s. Observed tides will differ considerably from understanding tides and making intelligent use of the tides predicted by equilibrium theory since size, depth, predictions published in tide and tidal current tables and and configuration of the basin or waterway, friction, land descriptions in sailing directions, the navigator can plan an masses, inertia of water masses, Coriolis acceleration, and expeditious and safe passage through tidal waters. other factors are neglected in this theory. Nevertheless, equilibrium theory is sufficient to describe the magnitude 901. Tide and Current and distribution of the main tide-generating forces across The rise and fall of tide is accompanied by horizontal the surface of the Earth. movement of the water called tidal current. It is necessary Newton’s universal law of gravitation governs both the to distinguish clearly between tide and tidal current, for the orbits of celestial bodies and the tide-generating forces relation between them is complex and variable. -
ASTORIA PARKS & RECREATION Comprehensive Master Plan 2016
ASTORIA PARKS & RECREATION Comprehensive Master Plan 2016 - 2026 Adopted July 18, 2016 by Ordinance 16-04 Acknowledgments Parks & Recreation Staff City Council Angela Cosby.......... Director Arline LaMear.......... Mayor Jonah Dart-Mclean... Maintenance Supervisor Zetty Nemlowill....... Ward 1 Randy Bohrer........... Grounds Coordinator Drew Herzig............ Ward 2 Mark Montgomery... Facilities Coordinator Cindy Price............. Ward 3 Terra Patterson........ Recreation Coordinator Russ Warr................ Ward 4 Erin Reding............. Recreation Coordinator Parks Advisory Board City Staff Norma Hernandez... Chair Brett Estes............... City Manager Tammy Loughran..... Vice Chair Kevin Cronin........... Community Josey Ballenger Development Director Aaron Crockett Rosemary Johnson... Special Projects Planner Andrew Fick John Goodenberger Historic Buildings Eric Halverson Consultant Jim Holen Howard Rub Citizen Advisory Committee Jessica Schleif Michelle Bisek......... Astoria Parks, Recreation, and Community Foundation Community Members Melissa Gardner...... Clatsop Community Kenny Hageman...... Lower Columbia Youth College Drafting and Baseball Historic Preservation Jim Holen................. Parks Advisory Board Program Craig Hoppes.......... Astoria School District Workshop attendees, survey respondents, Zetty Nemlowill....... Astoria City Council focus group participants, and volunteers. Jan Nybakke............ Volunteer Kassia Nye............... MOMS Club RARE AmeriCorps Ed Overbay............. Former Parks Advisory Ian -
Fort Clatsop, Lewis and Clark's 1805-1806 Winter Establishment "Living History" Demonstrations Feature for Visitors to National Park Facility
T HE OFFICIAL PUBLICATION OF THE LEWIS & CLARK T RAIL H ERITAGE FOUNDATION, INC. VOL. 12, NO. 3 AUGUST 1986 Fort Clatsop, Lewis and Clark's 1805-1806 Winter Establishment "Living History" Demonstrations Feature for Visitors to National Park Facility Photograph by Andrew E. Cier, Astoria, Oregon Replica of Fort Clatsop, Near Astoria, Oregon - See Story on Page 3 - President Wang's THE LEWIS AND CLARK TRAIL Message HERITAGE FOUNDATION, INC. Thank you's are due at least four Incorporated 1969 under Missouri General Not-For-Profit Corporation Act IRS Exemption different groups of Foundation Certificate No. 501(C)(3) - I dentification No. 51-0187715 members for the efforts put forth by them these past twelve months. OFFICERS - EXECUTIVE COMMITTEE First, I am most thankful for the President 1st Vice President 2nd Vice President excellent support that has been L. Edw in Wang John E. Foote H. John Montague provided by Foundation officers, 6013 St . Johns Ave. 1205 Rimhaven Way 2864 Sudbury Ct. directors, past presidents, and all M inneapolis. MN 55424 Billings. MT 591 02 Marietta. GA'30062 other committee members. Second, I am much indebted to the 1986 Edrie Lee Vinson. Secretary John E. Walker. Treasurer P.O. Box 1651 200 Market St .. Suite 1177 Program Committee, headed by Red Lodge. MT 59068 Portland. OR 97201 Malcolm Buffum, for the tre mendous effort they have put forth Ruth E. Lange, Membership Secretary. 5054 S.W. 26th Place. Port land. OR 97201 to arrange one of the finest-ever annual meeting programs. Third, I DIRECTORS am so grateful for all that is ac Harold Billian Winifred C. -
Geophysical and Geochemical Analyses of Selected Miocene Coastal Basalt Features, Clatsop County, Oregon
Portland State University PDXScholar Dissertations and Theses Dissertations and Theses 1980 Geophysical and geochemical analyses of selected Miocene coastal basalt features, Clatsop County, Oregon Virginia Josette Pfaff Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Part of the Geochemistry Commons, Geophysics and Seismology Commons, and the Stratigraphy Commons Let us know how access to this document benefits ou.y Recommended Citation Pfaff, Virginia Josette, "Geophysical and geochemical analyses of selected Miocene coastal basalt features, Clatsop County, Oregon" (1980). Dissertations and Theses. Paper 3184. https://doi.org/10.15760/etd.3175 This Thesis is brought to you for free and open access. It has been accepted for inclusion in Dissertations and Theses by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. AN ABSTRACT OF THE THESIS OF Virginia Josette Pfaff for the Master of Science in Geology presented December 16, 1980. Title: Geophysical and Geochemical Analyses of Selected Miocene Coastal Basalt Features, Clatsop County, Oregon. APPROVED BY MEMBERS OF THE THESIS COMMITTEE: Chairman Gi lTfiert-T. Benson The proximity of Miocene Columbia River basalt flows to "locally erupted" coastal Miocene basalts in northwestern Oregon, and the compelling similarities between the two groups, suggest that the coastal basalts, rather than being locally erupted, may be the westward extension of plateau -
Wallooskee-Youngs Confluence Restoration Project
B O N N E V I L L E P O W E R A D M I N I S T R A T I O N Wallooskee-Youngs Confluence Restoration Project Draft Environmental Assessment December 2014 DOE/EA-1974 This page left intentionally blank � Contents Contents .............................................................................................................................................................. i � Tables v � Figures ............................................................................................................................................................... vi � Appendices ....................................................................................................................................................... vi � Chapter 1 ......................................................................................................................................................... 1-1 � Purpose of and Need for Action ............................................................................................................. 1-1 � 1.1 Need for Action .................................................................................................................................. 1-3 1.2 Purposes ............................................................................................................................................... 1-3 1.3 Background ......................................................................................................................................... 1-4 1.3.1 Statutory Context ............................................................................................................. -
Assessment of Coastal Water Resources and Watershed Conditions at Lewis and Clark National Historical Park, Oregon and Washington
National Park Service U.S. Department of the Interior Natural Resources Program Center Assessment of Coastal Water Resources and Watershed Conditions at Lewis and Clark National Historical Park, Oregon and Washington Natural Resource Report NPS/NRPC/WRD/NRTR—2007/055 ON THE COVER Upper left, Fort Clatsop, NPS Photograph Upper right, Cape Disappointment, Photograph by Kristen Keteles Center left, Ecola, NPS Photograph Lower left, Corps at Ecola, NPS Photograph Lower right, Young’s Bay, Photograph by Kristen Keteles Assessment of Coastal Water Resources and Watershed Conditions at Lewis and Clark National Historical Park, Oregon and Washington Natural Resource Report NPS/NRPC/WRD/NRTR—2007/055 Dr. Terrie Klinger School of Marine Affairs University of Washington Seattle, WA 98105-6715 Rachel M. Gregg School of Marine Affairs University of Washington Seattle, WA 98105-6715 Jessi Kershner School of Marine Affairs University of Washington Seattle, WA 98105-6715 Jill Coyle School of Marine Affairs University of Washington Seattle, WA 98105-6715 Dr. David Fluharty School of Marine Affairs University of Washington Seattle, WA 98105-6715 This report was prepared under Task Order J9W88040014 of the Pacific Northwest Cooperative Ecosystems Studies Unit (agreement CA9088A0008) September 2007 U.S. Department of the Interior National Park Service Natural Resources Program Center Fort Collins, CO i The Natural Resource Publication series addresses natural resource topics that are of interest and applicability to a broad readership in the National Park Service and to others in the management of natural resources, including the scientific community, the public, and the NPS conservation and environmental constituencies. Manuscripts are peer-reviewed to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and is designed and published in a professional manner.