Obsidian Biulletin 2006 June 06 11 Final.Pub
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State Highway Department
Description of WOrk of the State Highway Department in the Counties of the State 1923 -1924 BAKER COUNTY There was less activity in highway constructjon in Baker County dur- ing the biennium just past than in previousyears. However, the main trunk line highway known as the Old Oregon Trailwas completed during this period, and some work was doneon the Baker-Cornucopia and the Baker-Unity Highways. The work on the Baker-Cornucopia Highway involved theconstruction of the grade down the Powder River Canyon, which eliminated the high Sparta summit and materially improved existing communicationbetween the Eagle and Pine Valleys and Baker.However, there still remains a very bad section between Middle Bridge and Love Bridge, and the section between Black Bridge and Richland, through the Dry Gulch country, is impassable to automobile traffic during the spring of theyear. On the Baker-Unity Highway the gradeon both sides of Dooley Moun- tain was completed. Those who were forced to travel the old mountain grade, which was narrow, crooked, and in places reacheda gradient of 22 per cent, will appreciate traveling over thenew highway now open to traffic. The total length of grading completed in Baker County during the past biennium was 18.11 miles, of which 8.95 mileswere surfaced. in addition to this work there were 25.90 miles surveyed. The Baker County bond issue of 1918, amounting to $500,000,was in- sufficient to meet the State in cooperating to complete the state highways through the county, and on November 4, 1924,an additional $500,00G was voted to complete the Baker-Cornucopia and the Baker-Unity High- ways. -
Spawning Areas and Abundance of Chinook Salmon {Oncorhynchus Tshawytscha} in the Columbia River Basin--Past and Present By
UNITED STATES DEPARTMENT OF THE INTERIOR u.S. FISH AND WILDLIFE SERVICE BUREAU OF COMMERCIAL FISHERIES Spawning Areas and Abundance of Chinook Salmon {Oncorhynchus tshawytscha} in The Columbia River Basin--Past and Present By LEONARD A. FULTON United States Fish and Wildlife Service Special Scientific Report- - Fisheries No. 571 Washington, D.C. October 1968 CONTENTS Page Introduction........................ Spring- and summer-run chinook salmon. .. 3 Spawning areas . .. 3 Abundance of spring- and summer- run chinook salmon. 4 Fall-run chinook salmon. 16 Spawning areas . 16 Abundance of fall- run chinook salmon 20 Summary and conclusions 22 Acknowledgments. 23 Literature cited .. 24 Maps .............. .See Map Appendix iii Spawning Areas and Abundance of Chinook Salmon (Oncorhynchus tshawytscha) in The Columbia River Basin--Past and Present By LEONARD A. FULTON, Fishery Biologist Bureau of Commercial Fisheries 'Biological Laboratory Seattle, Washington 98102 ABSTRACT Chinook salmon, the most abundant species of salmon in the Columbia Basin, formerly spawned in nearly a11 tributaries ofthe Columbia River and in many areas of the main river. Over the past 60 years, the construction of dams has inundated, impeded, or blocke.d acces!, to spawning areas. Despite these heavy losses, large areas of spawning grounds in the middle and lower portions of the drainage are sti11 available to chinook salmon. Stream im provements by State and Federal fishery agencies have rehabilitated some areas and have brought others into production for the first time. Important spawning areas are listed and charted in this report according to their past use (before 1965) and present use (1966). Estimates of recent spawning populations in major tributaries and in segments of the main stem are also given. -
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 -
Final Results of the 2013 Oregon Sport Fishing Regulation Development Summary of Final Rules Adopted by the Commission on September 7Th, 2012
Oregon Department of Fish and Wildlife 3406 Cherry Avenue NE Salem, OR 97303 Final Results of the 2013 Oregon Sport Fishing Regulation Development Summary of Final Rules Adopted by the Commission on September 7th, 2012 This package contains the following: Index of adopted and rejected proposals from the September 7th Commission meeting in Hermiston Oregon. Summary of final rules adopted by the Fish and Wildlife Commission at their September 7th, 2012 meeting in Hermiston Oregon. Final rule-making decisions by the Fish and Wildlife Commission for development of the 2013 Oregon Sport Fishing Regulations. The Commission adopted rules for the 2013 angling regulations at their September 7th meeting in Hermiston Oregon. Proposals followed by the letter “S” are ODFW or Oregon State Police (OSP) staff proposals (example 012S). Proposals followed by the letter “P” are proposals submitted by the public (example 25P) Table 1. Summary Index of adopted and rejected proposals from the September 7th Commission meeting. Statewide Regulations 1S Change Free Fishing Weekend Dates Adopted 2S Add new definitions “bobber” and “leader” Adopted 5S Adopt new Statewide Anti-Snagging Rules Adopted 7S Hook-less “bait” attracters in Ocean Salmon fishery Adopted 65P Allow Disabled Anglers Use of Electric Reels Adopted 4S Redefine definition of “Take” Adopted 3S Redefine “Snagging” to help enforcement Adopted 6P Soft-plastic and rubber imitations defined as lures Rejected 64P/91P “Rack-Your-Rod-Rule” Tidal Waters Rejected 6S Possession of fish in the field- Statewide -
Wednesday, August 11, 2021
CLATSOP COUNTY BOARD OF COMMISSIONERS AGENDA WORK SESSION & REGULAR MEETING VIRTUAL MEETING Wednesday, August 11, 2021 BOARD OF COMMISSIONERS: CONTACT: Mark Kujala, Dist. 1 – Chair 800 Exchange, Suite 410 Lianne Thompson, Dist. 5 – Vice Chair Astoria, OR 97103 John Toyooka, Dist. 2 Phone (503) 325-1000 Pamela Wev, Dist. 3 Fax (503) 325-8325 Courtney Bangs, Dist. 4 [email protected] www.co.clatsop.or.us JOIN THE BOARD OF COMMISSIONERS VIRTUAL MEETINGS Clatsop County Board of Commissioners host virtual meetings on GoToMeeting During the COVID-19 pandemic, the Board remains committed to broad community engagement and transparency of government. To provide an opportunity for public testimony while physical distancing guidelines are in effect, the Board will host virtual meetings on GoToMeeting. To join the meeting from your computer, tablet or smartphone. https://global.gotomeeting.com/join/793513109 You can also dial in using your phone. United States (Toll Free): 1 877 309 2073 United States: +1 (646) 749-3129 Access Code: 793-513-109 Those wishing to provide testimony on public hearings or provide oral communication at the designated time must register in advance by calling 503-325-1000 or email [email protected]. Once registered, you will be notified when it is your opportunity to speak for a two-minute presentation. The public may also submit comments to [email protected] which will be provided to the Board and submitted into the record . WORK SESSION: 5:00 PM Work Sessions are an opportunity for Board members to discuss issues informally with staff and invited guests. -
Lewis & Clark Map No K.Indd
Y a Y Y k 49 a i 43 a The Corps established a defensive position here on both the Named for the Corps' Private Jean Baptiste k m Rock Fort Campsite LePage Park W A N A P U M k 43 49 i 43 The Corps established a defensive position here on both the 49 Named for the Corps' Private Jean Baptiste im a Rock Fort Campsite The Corps established a defensive position here on both the LePage Park Named for the Corps' Private Jean Baptiste W A N A P U M m R. 395 a R outbound and return journeys. Interpretive signs. LePage, whose name Lewis & Clark gave to today's John Day River. R. 182 395 outbound and return journeys. Interpretive signs. LePage, whose name Lewis & Clark gave to today's John Day River. 82 182 v e r Interpretive sign. 82 182 k e R i v e r Interpretive sign. a k e R i v Interpretive sign. 12 n a k 240 PASCO S n 44 The Dalles Murals At several locations in the downtown area, large murals depict PASCO 12 S 44 The Dalles Murals At several locations in the downtown area, large murals depict 240 S Lewis & Clark's arrival and the Indian trading center at Celilo. 50 Crow Butte Park The Corps camped nearby, traveling by 60 Lewis & Clark's arrival and the Indian trading center at Celilo. 50 Crow Butte Park The Corps camped nearby, traveling by 60 horseback on the return jouney, long before dam flooding created 16-17 Oct. -
Museum Or Cultural Columbia River Maritime Museum 1792 Marine Drive, Astoria, OR, 503-325-2323 (Lat/Long = 46.189272, -123.823177) Cowlitz Co
MileByMile.com Personal Road Trip Guide Oregon State Highway #202 Miles ITEM SUMMARY 0.0 Junction Junction Oregon Route #202 with United States Highway #26/101, on Youngs Bay, on Columbia River at Astoria, Oregon. This is where Oregon Highway #202 starts its southeasterly run towards Mist, Oregon. Altitude: 13 feet 1.3 Junction Junction Warrenton-Astoria Highway/United States Highway #101, crosses the Youngs Bay here over a bridge to Community of Miles Crossing, Oregon. Altitude: 39 feet 1.4 Astoria, Oregon 7th Street/8th Street, Astoria, Oregon, in Clatsop County, Oregon, Situated near the mouth of the Columbia River, the city is served by the Port of Astoria with a deep-water port. The Captain George Flavel House Museum, a house museum, Columbia River Maritime Museum, is also located in Astoria, Oregon. Altitude: 46 feet 2.4 Williamsport Road Williamsport Road, Shively Park Road, Shively Park Road, Astoria Column, Astoria Reservoir, Altitude: 33 feet 4.2 Walluski Loop Walluski Loop, runs along the Wallooskee River and rejoins with Oregon Route #202, Altitude: 26 feet 7.0 Walluski Loop Walluski Loop, runs along the Wallooskee River, Altitude: 62 feet 9.3 Olney, Oregon Youngs River Road, Olney Cutoff Road, Community of Olney, Oregon, Youngs River Falls, a scenic waterfall on the Youngs River along the Youngs River Road, off Oregon Route #202, in central Clatsop County, Oregon. Altitude: 75 feet 10.9 Lillenas Road Lillenas Road, Community of Lilleas, Oregon, Community of Estoos, Oregon Altitude: 49 feet 16.7 California Barrel Road California Barrel Road, Wickiup Spring Road, Pigpen Road Altitude: 676 feet 20.3 Saddle Mountain Road Saddle Mountain Road. -
Of the GEOLOGICAL SURVEY
UNITED SI of THE GEOLOGICAL SURVEY Of ULTB&^flBffDULIOUt B4TA FOR CUOQI STRXMB ?r«p«r«d In cooperative With; Or«9on Stat« Water B*M«r«a0 Board U.S. Bureau of Reclaoetion U.S. Ooorpa af Baglaeece U.S. Fubllc Baalth Service t.S. toil Oeasarvatlon Service Open-file report PertLend, Orefcpn 1914 CONTENTS Page Introduction ..** . ..*«*..» *.«..«*» ., ..............4....... 3 Cooperation .., .........,.............*....,...,.............. 4 Explanation of data ..........I.................*.............. 5 Station descriptions ..................................... 5 Location . ....,..... ..... ...,...*............«. 5 Drainage araa .......................«.,,*.......,*,. 6 Water-tawperature racorda available ................. 6 Remarks ..........»,.,....».....,.*»......*...«...,.. 7 Table* of water*taapa?ature data ......................... 7 Tharmograph records ................................. 7 Spot-obaarvatioa records .... ^....................... 8 Water*tawparaturc racords ..................................... 11 Indaoc .......,,,..,..,....,.,...,,............,....,,....,....* 132 ILLUSTRATION Flate 1. Map of Or«fon having site* where water*temperature data have obtained .......*.,............................In pocket. * . f a 'V GOMPIIATUK OF WATER -TWP1IATOIB DATA. FOt OUBOOH STREAMS By A* M» INTRODUCTION Practically all water -temperature data col lee tad through September 30, 1962, by varioua agendas, both public and private, are presented herein. Only those racords with ao fav observations as to ba of ao significant valua have beau -
Geology of the Green Mountain-Young's River Area, Clatsop County, Northwest Oregon Recicted for Privacy Abstract Approved: (Alan R
AN ABSTRACT OF THE THESIS OF Carolyn Pugh Peterson for the degree of Master of Science in Geology presented on December 12, 1983 Title: Geology of the Green Mountain-Young's River Area, Clatsop County, Northwest Oregon Recicted for Privacy Abstract Approved: (Alan R. Niem) The upper Eocene to lower Oligocene Oswald West mudstone is the oldest formation (informal) in the Green Mountain-Young's River area. This 1,663 meter thick hemipelagic sequence was depos- ited in a low-energy lower to upper slope environment in the Coast Range forearc basin. The formation ranges from the late Narizian to the early Zemorrian(?) in age and consists of thick-bedded bio- turbated foraminiferal claystone and tuffaceous siltstone. Rare glauconitic sandstone beds also occur. In the eastern part of the study area, the upper part of the Oswald West mudstone is inter- bedded with the upper Refugian Klaskanine siltstone tongue. This informal unit consists of thick bioturbated sandy siltstone and silty sandstone that is a lateral deep-marine correlative of the deltaic to shallow-marine Pittsburg Bluff Formation in the north- eastern Coast Range. Discontinuous underthrusting of the Juan de Fuca oceanic plate at the base of the continental slope of the North American plate caused extensive uplift and subsidence along the Oregon continental margin throughout the Cenozoic (Snavely et al., 1980). Initiation of Oregon Coast Range uplift and accompanying erosion in the early Miocene, coupled with a global low stand of sea level (Vail and Mitchum, 1979), stripped most of the Oligocene (Zemor- rian) Oswald West strata and in places much of the uppermost Eocene (upper Refugian) Oswald West strata in the field area, cre- ating an unconformity. -
Appendices (PDF)
Appendices Appendix A: Background Information for the Lewis and Clark Expedition ............................................................. 3 The Expedition: Making Ready ................................................................................................................................. 3 List of Supplies .......................................................................................................................................................... 5 Timeline for the Lewis and Clark Expedition ............................................................................................................. 9 Map of the Westward Route of the Lewis and Clark Expedition ............................................................................ 19 Map of the Eastbound Route of the Lewis and Clark Expedition ............................................................................ 20 The Expedition: Putting Away ................................................................................................................................ 21 Appendix B: People of the Lewis and Clark Expedition ....................................................................................... 23 President Thomas Jefferson ................................................................................................................................... 23 Captain Meriwether Lewis (Co-Leader) .................................................................................................................. 24 Seaman (Dog and Expedition -
Or Wild and Scenic Rivers System
Cascades Ecoregion ◆ Introduction 115 Young Volcanoes and Old Forests Cascades Ecoregion he Oregon portion of the Cascades Ecoregion encompasses 7.2 million growth forests. These include Roosevelt elk, black-tailed deer, beaver, black bear, coyote, acres and contains the highest mountains in the state. The Cascades marten, fisher, cougar, raccoon, rabbits, squirrels and (probably) lynx. Bird species Ecoregion is the backbone of Oregon, stretching lengthwise from the include the northern spotted owl and other owls, blue and ruffed grouse, band-tailed T Columbia River Gorge almost to the California border. Its width is pigeon, mountain quail, hawks, numerous songbirds, pileated woodpecker and other defined by the Willamette Valley and Klamath Mountains Ecoregions woodpeckers, bald eagle, golden eagle, osprey and peregrine falcon. Fish species include on the west and the Eastern Cascade Slope and Foothills Ecoregion on the east. The Pacific salmon stocks, bull trout and rainbow trout. Five of the eleven species endemic to highest peak is Mount Hood (11,239’). This ecoregion also extends northward into the ecoregion are amphibians: Pacific giant salamander, Cascade seep salamander, Washington and has three unusual outlier terrestrial “islands:” Paulina Mountains Oregon slender salamander, Larch Mountain salamander and the Cascades frog. southeast of Bend, Black Butte near Sisters and Mount Shasta in California. The effects of latitude on forest type are obvious in the Cascades as they range from Geologically, the ecoregion consists of two mountain ranges: the High Cascades the Columbia River to the California border. The effects of elevation are dramatic as well. and the Western (sometimes called “Old”) Cascades. Both are parallel north-south Beginning at the Willamette Valley margin and heading both eastward and ranges, but they are geologically distinct, as one is much older than the other. -
Obsidian Bulletin 2006 March 4A.Pub
VOLUME 66 MARCH 2006 NUMBER 3 Inside This Issue Summer Trips Committee Schedules Membership Updates 2 More Than 200 Outings for 2006 March Interim Potluck 3 The Right Gaiters 4 By Janet Jacobsen Construction Progress 4 OLISH THOSE HIKING BOOTS, pump Board Notes 8 P up those bicycle tires, search for those Trip Reports 9-14 binoculars…and sign up for an Obsidian Upcoming Events 15-19 trip! Obsidian Trips Schedule 17-18 This year’s summer schedule invites Features by Members every Obsidian to exclaim, “That looks interesting; I would like to go on that Over 200 Outings 1 trip.” Reward 3 Margaret Prentice and the 19 people on Gray Whale Encounters 5 the Summer Trips Committee have been Hikes at Camp Deetour 7 working since January, calling and Trip Sampler 15 emailing potential leaders. Their hard Insert work paid off with 102 leaders leading 202 trips (as the Bulletin went to press). Obsidian Membership Directory There are 169 hikes, 3 backpacks, 1 canoe trip, 4 nature walks, 2 field trips, trail maintenance outings and 22 bike trips, Dates to Remember some of which include birding, camping and hiking. The Summer Trips Committee Mar 18 Lodge Work Party has also facilitated activities sponsored by Mar 24 Program - Reuls - Spain the Conservation and the Science & Edu- Apr 5 Obsidian Board Meeting Margaret Prentice, Sullivan in hand, map at cation Committees, such as Beach Clean the ready, who along with her dedicated Apr 10 Trip Leaders Meeting Up Day on March 25. committee, put together a record setting IT IS NOT EASY calling an Obsidian in trips schedule.