Chapter 2: History of the City of Tillamook
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Bay, Oregon, with Notes on Shehfish Temperature, and Physical
COASTAL RIVERS I NFORMAT I ON Observations onon FishFish LiistributDistribution ion inin TillamookTillamook Bay, Oregon,Oregon, wi-f-h with NotesNotes on ShellfishSheHfish Temperature, and Physical Characteristics by T. Edwin Cummings Richard L. Berry Fish Commission of Oregon Management and Research Division This work was conducted in cooperation with -f-hethe NationaJ National Marine Fisheries Service under the AnadromousFish Act PL 89-304 April 19741974 4 CONTENTS Page No. I NTRODUCT I(ON ON DESCRIPTION OF ThETHE AREA. METHODS.......................................................... 4 Seining Sites. 4 Equipment . 5 Data Recorded 5 RESULTS ..................................................................................................................... 5 Coho. Chinook. Herr! ng. .................................................... 12 Smell-..ei I 2 Sole..So I e.. 13 StanyFyFlounder Flounder............................................................ 13 SurfPerch .................................................................................................... 13 Col-tids....................... .,....... ..................... 14 MiscellaneousMiscellaneousFish Fish SpeciesSpecies.................................. 14 Shellfish................................................... 14 Temperature ................................................. 17 DISCUSSION. 17 ACKNOWLEDGMENTS. 19 LITERATURE CITED. 19 APPEND IX 20 FIGURES fj9urefure No.No. Page No. I Map of Tillamook Bay,Bay, OregonOregon 3 2 Presence ofof FishesFishes inin thethe Ti -
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. -
Lower Alsea River Watershed Analysis
Table of Contents Executive Summary .................................................. iii List of Tables ....................................................... xx List of Figures ..................................................... xxii List of Maps ...................................................... xxiii Chapter 1 - Characterization ............................................ 1 Chapter 2 - Issues and Key Questions ..................................... 6 Chapter 3 - Reference and Current Conditions ............................. 10 Forest Fragmentation ............................................ 10 Aquatic Habitat ................................................. 32 Human Uses ................................................... 72 Chapter 4 - Interpretation/Findings and Recommendations ................... 86 References ......................................................... 96 Appendices ........................................................ 103 Map Packet ........................................... (following p. 123) Page ii EXECUTIVE SUMMARY Characterization: The Analysis Area The Lower Alsea River watershed, located in the Alsea River Basin, encompasses about 98,470 land acres of the western Oregon Coast Range mountains along the lower Alsea River in Benton and Lincoln counties (Map 1: “Alsea Basin and Lower Alsea Analysis Area”). The watershed, with State Highway 34 running through it, stretches from Waldport on the coast to the inland town of Alsea. About 14 per cent of the watershed (13,786 acres) is managed by the Bureau -
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. -
Characterizing Tribal Cultural Landscapes, Volume II: Tribal Case
OCS Study BOEM 2017-001 Characterizing Tribal Cultural Landscapes Volume II: Tribal Case Studies US Department of the Interior Bureau of Ocean Energy Management Pacific OCS Region This page intentionally left blank. OCS Study BOEM 2017-001 Characterizing Tribal Cultural Landscapes Volume II: Tribal Case Studies David Ball Rosie Clayburn Roberta Cordero Briece Edwards Valerie Grussing Janine Ledford Robert McConnell Rebekah Monette Robert Steelquist Eirik Thorsgard Jon Townsend Prepared under BOEM-NOAA Interagency Agreement M12PG00035 by National Oceanic and Atmospheric Administration Office of National Marine Sanctuaries 1305 East-West Highway, SSMC4 Silver Spring, MD 20910 Makah Tribe Confederated Tribes of Grand Ronde Community of Oregon Yurok Tribe National Marine Sanctuary Foundation US Department of Commerce National Oceanic and Atmospheric Administration Office of National Marine Sanctuaries US Department of the Interior Bureau of Ocean Energy Management Pacific OCS Region December 31, 2017 This page intentionally left blank. DISCLAIMER This study was funded, in part, by the US Department of the Interior, Bureau of Ocean Energy Management (BOEM), Pacific Outer Continental Shelf (OCS) Region, Camarillo, CA, through Interagency Agreement Number M12PG00035 with the US Department of Commerce, National Oceanic and Atmospheric Administration (NOAA). This report has been technically reviewed by BOEM and it has been approved for publication. The views and conclusions contained in this document are those of the authors and should not be interpreted as representing the opinions or policies of the US Government, nor does mention of trade names or commercial products constitute endorsement or recommendation for use. REPORT AVAILABILITY This report can be downloaded from the Bureau of Ocean Energy Management’s Recently Completed Environmental Studies – Pacific webpage at https://www.boem.gov/Pacific-Completed-Studies/. -
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 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. -
Click Here to Download the 4Th Grade Curriculum
Copyright © 2014 The Confederated Tribes of Grand Ronde Community of Oregon. All rights reserved. All materials in this curriculum are copyrighted as designated. Any republication, retransmission, reproduction, or sale of all or part of this curriculum is prohibited. Introduction Welcome to the Grand Ronde Tribal History curriculum unit. We are thankful that you are taking the time to learn and teach this curriculum to your class. This unit has truly been a journey. It began as a pilot project in the fall of 2013 that was brought about by the need in Oregon schools for historically accurate and culturally relevant curriculum about Oregon Native Americans and as a response to countless requests from Oregon teachers for classroom- ready materials on Native Americans. The process of creating the curriculum was a Tribal wide effort. It involved the Tribe’s Education Department, Tribal Library, Land and Culture Department, Public Affairs, and other Tribal staff. The project would not have been possible without the support and direction of the Tribal Council. As the creation was taking place the Willamina School District agreed to serve as a partner in the project and allow their fourth grade teachers to pilot it during the 2013-2014 academic year. It was also piloted by one teacher from the Pleasant Hill School District. Once teachers began implementing the curriculum, feedback was received regarding the effectiveness of lesson delivery and revisions were made accordingly. The teachers allowed Tribal staff to visit during the lessons to observe how students responded to the curriculum design and worked after school to brainstorm new strategies for the lessons and provide insight from the classroom teacher perspective. -
The Spirit of the Tillamook People by Brian D
The Spirit of the Tillamook People By Brian D. Ratty © 2016 The terrain of the Northwest Coastline is rugged and untamed, in many ways as forbidding as the natives that flourished on its shore. This narrow strip of land was home to dozens of different Indian nations. Just south of Tillamook Bay were many other nations, including the Siletz and the Siuslaw, while to the north were the Clatsop and Chinook tribes. Unlike most inland Indians, these nations didn’tnomadically follow game or move with the seasons. Instead, they stayed close to the bays and the sea, establishing permanent homes and villages. Within each Indian nation there were tribes, and within these tribes there were bands, and within these bands there were different clans. Each nation lived to the dictates of the resources Mother Nature provided, and their ability to hunt and gather food. When Captain Robert Gray discovered Tillamook Bay in 1788, the Tillamook nation numbered roughly 2,200 natives. These people lived in nine different villages, from the Nestucca River in the south to the Nehalem Bay in the north. The largest Tillamook village was Kilharhurst, which occupied the land that is the present-day site of Garibaldi, Oregon. The river next to this village was called Kilharnar, known today as the Miami River. This village had about fifty lodges and five hundred inhabitants. Over time, the Tillamooks assumed most of the customs, habits and dress of their powerful neighbors to the north, the Chinooks. Although both nations spoke the Salish language, their dialects were so different that, when they talked, they had to sign, as well. -
Soil Survey of Tillamook County, Oregon
Index to Map Sheets Tillamook County, Oregon 1 2 3 4 5 6 Arch Cape Soapstone Lake Hamlet Elsie Sunset Spring Clear Creek N COLUMBIA COUNTY CLATSOP COUNTY WASHINGTON COUNTY Aldervale River TILLAMOOK COUNTY ! ¤£26 (!47 7 Nehalem £101 N. Fork 7 ¤ 8 9 10 11 12 Nehalem Nehalem53 !Enright ! ! (! Manzanita ! Mohler Batterson! River !Foss Foley Peak Cook Creek Rogers Peak Cochran Timber ¤£26 Nehalem !Manning Glenwood ! Manhattan Beach ! (!6 ! Rockaway Beach (!6 13 14 15 16 17 18 Jordan Creek Garibaldi ! Kilchis River Cedar Butte Wood Point Roaring Creek (!8 !Jordan Creek Garibaldi Watts ! Tillamook Bay 19 20 21 22 23 (!6 Wilson River ! Oceanside ! ! Tillamook Fairview (!47 Netarts Tillamook ! ¤£101 Trask River The Peninsula Trask Gobblers WASHINGTON COUNTY YAMHILL COUNTY Netarts Tillamook Knob Netarts River Bay Pleasant Valley ! 24 25 26 27 28 Yamhill ! (!240 Trask P A C I F I C O C E A N Sand Lake Beaver Blaine Dovre Peak Mountain (!47 ! Blaine ! Tierra Del Mar 29 ! Hebo 30 31 32 33 (!99W ¤£101 ! McMinnville Pacific City ! River Hebo Nestucca Springer (!18 Nestucca Niagara Creek Mountain Stony Mountain Bay (!18 (!233 Meda ! Amity Neskowin ! 34 ! 35 36 37 (!22 Neskowin YAMHILLCOUNTY Neskowin POLK Midway COUNTY OE W Dolph (!18 ! Grand Ronde 99W TILLAMOOK COUNTY (! LINCOLN COUNTY ¤£101 Sources: Shaded relief acquired from United States Geological Survey (USGS). County Boundaries, cities, and roads are provided by 0 2 4 6 8 TeleAtlas Dynamap. Miles Prepared by the Pacific Northwest Soil Survey Regional Office (MO1) 0 2 4 6 8 Portland, OR, 2012. All information is provided "as is" and United States Department of Agriculture, Forest Service without warranty, express or implied. -
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. -
Public Law 588-Aug. 13, 1954 [68 St At
724 PUBLIC LAW 588-AUG. 13, 1954 [68 ST AT. Public Law 588 CHAPTER 733 August 13, 1954 AN ACT [S. 2746] To provide for the termination of Federal supervision over the property of certain tribes and bands of Indians located in western Oregon and the indi vidual members thereof, and for other purposes. Be it enmted hy the Senate and House of Representatives of the Oregon Indians. Termination o f United States of America in Congress assembled^ That the purpose Federal super - of this Act is to provide for the termination of Federal supervision vision. over the trust and restricted property of certain tribes and bands of Indians located in western Oregon and the individual members thereof, for the disposition of federally owned property acquired or withdrawn for the administration of the affairs of such Indians, and for a termination of Federal services furnished such Indians because of their status as Indians. Definitions. SEC. 2. For the purposes of this Act: (a) "Tribe" means any of the tribes, bands, groups, or communities of Indians located west of the Cascade Mountains in Oregon, including the following: Confederated Tribes of the Grand Ronde Community, Confederated Tribes of Siletz Indians, Alsea, Applegate Creek, Cala- pooya, Chaftan, Chempho, Chetco, Chetlessington, Chinook, Clacka mas, Clatskanie, Clatsop, Clowwewalla, Coos, Cow Creek, Euchees, Galic Creek, Grave, Joshua, Karok, Kathlamet, Kusotony, Kwatami or Sixes, Lakmiut, Long Tom Creek, Lower Coquille, Lower Umpqua, Maddy, Mackanotin, Mary's River, Multnomah, Munsel Creek, Nal- tunnetunne, Nehalem, Nestucca, Northern Molalla, Port Orford, Pud ding River, Rogue River, Salmon River, Santiam, Scoton, Shasta, Shasta Costa, Siletz, Siuslaw, Skiloot, Southern Molalla, Takelma, Tillamook, Tolowa, Tualatin, Tututui, Upper Coquille, Upper Ump qua, Willamette Tumwater, Yamhill, Yaquina, and Yoncalla; (b) "Secretary" means the Secretary of the Interior, (c) "Lands" means real property, interest therein, or improve ments thereon, and includes water rights.