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Geologic Map of the Sauvie Island Quadrangle, Multnomah and Columbia Counties, Oregon, and Clark County, Washington
Geologic Map of the Sauvie Island Quadrangle, Multnomah and Columbia Counties, Oregon, and Clark County, Washington By Russell C. Evarts, Jim E. O'Connor, and Charles M. Cannon Pamphlet to accompany Scientific Investigations Map 3349 2016 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Director U.S. Geological Survey, Reston, Virginia: 2016 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov or call 1–888–ASK–USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. Suggested citation: Evarts, R.C., O'Connor, J.E., and Cannon, C.M., 2016, Geologic map of the Sauvie Island quadrangle, Multnomah and Columbia Counties, Oregon, and Clark County, Washington: U.S. Geological Survey Scientific Investigations Map 3349, scale 1:24,000, pamphlet 34 p., http://dx.doi.org/10.3133/sim3349. ISSN 2329-132X (online) Contents Introduction ................................................................................................................................................................... -
Marriage of Basalt and His Wife River by Rick Rubin ©2001
The Marriage of Basalt and his Wife River By Rick Rubin ©2001 Sixteen million years ago, a vast outpouring of lava from eastern Oregon began. The greatest lava flow in North America, that lava covered 80,000 square miles with molten rock. At that time, the Columbia River had her bed where Salem is now. A (miocene) basalt path, covered by (Quaternary) alluvial sediment just south of Salem shows the place. Her bed reached the sea north of the present Lincoln City. That lava outpouring got into her bed. Filled it up. Got hard. Became grass covered Cascade Head, north of Lincoln City. Husband-like, Basalt shouldered his river/wife north and west. She had to make a new bed for herself. Time and again those cracks to the east poured out lava, which flowed down the river’s new bed, which was always to the north of the earlier one, and came to the sea, or perhaps simply stopped, for the sea was as much as 300 miles farther west than it is now some of the time. (That was Ice Age’s doing. The Earth’s water was all tied up in glacier ice). The next time fiery Basalt poured out from east of where the Cascade mountains are now, and coming into Columbia River’s bed flowed down to the sea, it cooled into slim, steep sided, jutting Cape Lookout A million or so years later, Basalt flowed into the river’s attractive bed again, and this time, when he reached the sea, became blocky Cape Meares, just south of Tillamook Bay Later Basalt may have made a cape at the north entrance to Great Basin petroglyphs from Petroglyphs of Oregon, Luther Cressmann, Tillamook Bay of which some basalt rocks near the shore are the only relics. -
Tualatin Hills and the Laurelwood District Are Oregon's Newest
171 views | Jun 10, 2020, 12:24pm EDT Tualatin Hills And The Laurelwood District Are Oregon’s Newest American Viticultural Areas Joseph V Micallef Contributor Spirits I write about wines and spirits and the hidden corners of the world Ponzi Vineyard, View from Aurora Vineyard PHOTO COURTESY PONZI VINEYARDS/ANDREA JOHNSON AERIALS Two new American Viticultural Areas (AVA) have been announced by the Alcohol and Tobacco Tax and Trade Bureau (TTB). Located in the northern end of Oregon’s Willamette Valley, in the heart of Oregon’s Pinot Noir producing zone, the two new AVAs are Tualatin Hills and the Laurelwood District. The two AVAs, which are partially adjacent to one another, are notable for containing among the highest concentrations of Laurelwood soils in Oregon. Laurelwood soils consist of an exceptionally fine windblown soil called loess. It consists predominantly of silt-sized sediment that was formed by the accumulation of wind-blown dust and was produced by the grinding down of basaltic and other volcanic rocks by glaciers during the last ice age. Most Popular In: Spirits Father’s Day Gift Guide: The World’s Best Whiskey (And Whisky) Under $100 Father’s Day Gift Guide: Essential BBQ And Grilling Tools Father’s Day Gift Guide: The 20 Best Scotch Whisky Gifts The Tualatin Hills and Laurelwood District AVAs PHOTO, COURTESY OREGON WINE BOARD This soil produces very Burgundian styled Pinot Noir wines. They emphasize flavors of cherry, blackberry and spice. These wines offer a lighter, elegant style and texture with well-defined tannins, which is markedly different than the earthier, more robust, black fruit centered styles typical of Oregon’s sedimentary soils. -
Tualatin Valley Scenic Bikeway Management Plan Washington County, Oregon March 1, 2013
Tualatin Valley Scenic Bikeway Management Plan Washington County, Oregon March 1, 2013 Revised March 20, 2013 TABLE OF CONTENTS Page 1 Proponent contact information 2 Route map 3-4 Sign plan introduction 5 Sign location table 6-9 Field-checked turn-by-turn cue sheet 10-11 Final letters of support from all road jurisdictions 12-25 Records of public notification 26 Map features 27-28 State Congressional representatives 28 Overarching objectives 29 Business target markets 29-30 Cyclist categories 31 Web action items / Ongoing Web communications 31-32 General marketing action items 32 Ride description 33 Talking points 33-34 Measurable objectives 34 Electronic photos 34 Preservation and enhancement goals 35-37 Tualatin Valley Scenic Bikeway Management Plan 1 | Page Proponent Contact Information Contact Name, Agency Contact Info Role Carolyn McCormick 11000 SW Stratus St., Ste. 170 Coordinates marketing and President/CEO, Washington Beaverton, OR 97008 promotion, steering County Visitors Association Phone: 503-644-5555 committee, signage, Email: [email protected] jurisdiction involvement Allison George 11000 SW Stratus St., Ste. 170 Coordinates outreach and Stakeholder Development Beaverton, OR 97008 engagement of local Manager, Washington County Phone: 503-644-5555 tourism-related businesses Visitors Association Email: [email protected] along the route Joy Lalic Chang 155 N. First Ave., Ste. 350-14 Traffic engineering and Associate Planner Hillsboro, OR 97124 coordination with Washington County Long Phone: 503-846-3873 maintenance/operations on Range Planning Email: [email protected] Washington County roads Jolynn Becker 13680 NW Main St. Interim City Manager Banks, OR 97106 Point of contact for Banks City of Banks Phone: 503-324-5112 ext. -
Willamette Valley Avas, Making Them Well-Drained and Extending Hang Time for Fruit During Final Ripening
Oregon Wine Board WILLAMETTE VALLEY UPDATED 4.1.17 This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/. Oregon Wine Board OREGON IN CONTEXT CELEBRATED, RENOWNED, EXQUISITE. Oregon's Willamette Valley is, at this point, synonymous with glorious Pinot noir. No other grape is as reflective of climatic and site differences, and small distances in the valley can yield wines of distinctly different character, each captivating in its own way. Oregon Wine Board OREGONOREGON IN IN CONTEXT CONTEXT WHERE IN THE WORLD IS OREGON? The world's premier winegrowing regions are found between the latitudes of 30-50°. Oregon is located in the northwestern United States at a northerly latitude between 42-46° N. BURGUNDY, OREGON, FRANCE UNITED STATES 50° N 45TH PARALLEL 30° N BORDEAUX, FRANCE NAPA VALLEY CALIFORNIA UNITED STATES 0° EQUATOR MENDOZA, 30° S ARGENTINA MARGARET RIVER, AUSTRALIA STELLENBOSCH, SOUTH AFRICA CENTRAL OTAGO, 50° S NEW ZEALAND Oregon Wine Board OREGONOREGON IN IN CONTEXT CONTEXT WALLA WALLA WASHINGTON VALLEY 46° N COLUMBIA WINE-PRODUCING GORGE WILLAMETTE REGIONS OF THE VALLEY WEST COAST SOUTHERN OREGON OREGON IDAHO Oregon is bordered by 42° N Washington to the north and California to the south. CALIFORNIA From northern Washington to NAPA VALLEY southern California, West Coast NEVADA winegrowing spans more than UTAH 1,200 miles (1,900 km) north SONOMA COUNTY to south. ARIZONA Oregon Wine BoardBoard OREGONOREGON IN IN CONTEXT CONTEXT WASHINGTON ER 17 RIV A BI C OLU M 15 14 16 PORTLAND MOUNT HOOD2 3 SALEM 6 4 PACIFIC 1 5 OCEAN 7 COAST RANGE 18 IDAHO 11 10 9 CASCADE RANGE 8 SISKIYOU MTS 12 13 CALIFORNIA NEVADA 1. -
Dam Failure (Scoggins)
IA 6 – Dam Failure (Scoggins) Final: January 2017 THIS PAGE LEFT BLANK INTENTIONALLY Clackamas County EOP Support Annex IA 6. Dam Failure (Scoggins) Table of Contents 1 Introduction ................................................................................. IA 6-1 1.1 Purpose ....................................................................................................... IA 6-1 1.2 Scope .......................................................................................................... IA 6-1 1.3 Policies and Authorities ............................................................................... IA 6-1 2 Situation and Assumptions ........................................................ IA 6-2 2.1 Situation ...................................................................................................... IA 6-2 2.2 Failure Conditions ....................................................................................... IA 6-3 2.3 Assumptions................................................................................................ IA 6-3 3 Roles and Responsibilities of Tasked Agencies ....................... IA 6-4 3.1 On-Scene Incident Command/Command Center ........................................ IA 6-4 3.2 Law Enforcement Agencies......................................................................... IA 6-5 3.3 Fire Agencies .............................................................................................. IA 6-5 3.4 County Emergency Operations Center ...................................................... -
Landscape Change in the Tualatin Basin Following Euro-America N
Landscape Change in the Tualatin Basin Following Euro-American Oregon Water Resources Research Institut e Oregon State University October 1993 LANDSCAPE CHANGE IN THE TUALATIN BASI N FOLLOWING EURO-AMERICAN SETTLEMEN T by David D. Shively Department of Geosciences Oregon State University The Tualatin River Basin studies are being done under a grant from the Oregon Department of Environmental Quality to the Oregon Water Resources Research Institute . Tualatin River Basin Water Resources Management Report Number 6 TUALATIN RIVER BASIN SPECIAL REPORT S The Tualatin River Basin in Washington County, Oregon, is a complex area wit h highly developed agricultural, forestry, industrial, commercial, and residential activities. Population has grown in the past thirty years from fifty to over 270 thousand . Accompanying this population growth have been the associated increases i n transportation, construction, and recreational activities . Major improvements have occurred in treatment of wastewater discharges from communities and industries in th e area. A surface water runoff management plan is in operation, Agricultural and forestr y operations have adopted practices designed to reduce water quality impacts . In spite of efforts to-date, the standards required to protect appropriate beneficial uses of water hav e not been met in the slow-moving river . The Oregon Department of Environmental Quality awarded a grant in 1992 to the Oregon Water Resources Research Institute (OWRRI) at Oregon State University to review existing information on the Tualatin, organize that information so that it can be- readily evaluated, develop a method to examine effectiveness, costs and benefits of alternative pollution abatement strl ategies., and allow -for the evaluation of various scenarios proposed for water management in the Tualatin Basin . -
Gales Creek WS Assess.Pdf
GALES CREEK WATERSHED ASSESSMENT PROJECT Prepared by Nancy Breuner Resource Assistance for Rural Environments Tualatin River Watershed Council September 1998 Abstract This document is the Gales Creek Watershed Assessment Report prepared for the Tualatin River Watershed Council. This report contains detailed information about the Gales Creek Watershed and follows the guidelines described in the 1997 Draft Governor’s Watershed Enhancement Board’s Oregon Watershed Assessment Manual. It was written to partially satisfy the watershed assessment action item #1described in the Tualatin River Watershed Council’s Action Plan. This report should be periodically updated, as new information becomes available. Acknowledgement The completion of the Gales Creek Watershed Assessment Project was accomplished through the combined efforts of private citizens, students, private and non-profit organizations, and local and state agencies. Production of this document was made possible with assistance from the Washington County Soil and Water Conservation District and Unified Sewerage Agency. Geographic Information System maps were compiled by Interrain Pacific. Technical advice for the report was provided by the Tualatin River Watershed Council’s Technical Assistance Committee made up of local and regional experts. For more information about the Gales Creek Watershed Assessment Project or to obtain copies of this report, contact: Tualatin River Watershed Council PO Box 338 Hillsboro, OR 97123-0338 (503) 846-4810 Gales Creek Watershed Assessment Project ii Gales -
Henry Hagg Lake Resource Management Plan
Henry Hagg Lake Resource Management Plan U.S. Department of the Interior Bureau of Reclamation Pacific Northwest Region Lower Columbia Area Office May 2004 Cowlitz ClatsopRegional Context MONTANA WASHINGTON Columbia %&'(I5 Clark IDAHO OREGON WA O S R I205 CALIFORNIA H %&'( NEVADA E I N G G O T N O N Multnomah Vancouver W il la Washington m Columbia e Tillamook t Henry Hagg Lake Study Area OP26 te %&'(I5 R iver Forest %&'(I84 Grove Hillsboro Cornelius Portland %&'(I205 Gresham Aloha uala Powellhurst-Centennial T tin R Beaverton iv er R iv e r Gaston Milwaukie Tigard Lake Oswego Oatfield OP47 Tualatin West Linn %&'(I205 Oregon City Yamhill Clackamas r Wi e v l lam ette Ri %&'(I5 McMinnville Marion Highway County Boundary Regional Location Map Stream State Boundary V Henry Hagg Lake RMP 0510 Miles 1:530,000 Source: ESRI, USBR, USGS, EDAW, 2003 P:\1e41401_Henry_Hagg\GIS\Project\mxd\RMP\Figure_Regional_Location.mxd HENRY HAGG LAKE Resource Management Plan U.S. Department of the Interior Bureau of Reclamation Approved: This Resource Management Plan was prepared by EDAW and JPA under contract for the Department of the Interior, Bureau of Reclamation, Pacific Northwest Region. Point of Contact: Karen Blakney U.S. Bureau of Reclamation Lower Columbia Area Office 825 NE Multnomah Street, Suite 110 Portland, OR 97232-2135 (503) 872-2796 Cowlitz ClatsopRegional Context MONTANA WASHINGTON Columbia '%&(I5 Clark IDAHO OREGON WA O S R I205 CALIFORNIA H &%'( NEVADA E I N G G O T N O N Multnomah Vancouver W il la Washington m Columbia e Tillamook t Henry -
The Petrology and Stratigraphy of the Portland Hills Silt Portland Hills Silt, Which Once Covered Much of This Area
OREGON GEOLOGY published by the Oregon Department of Geology and Mineral Industries VOLUME 43 , NUMBER 1 JANUARY 1981 DOGAMI laboratory policy revised OREGON GEOLOGY (ISSN 0164-3304) The greatly increased need for systematic rock-chemistry data for Oregon has prompted the Oregon Department of VOLUME 43, NUMBER 1 JANUARY 1981 Geology and Mineral Industries to enlarge the scope of its laboratory facilities. The Department lab is managed by Published monthly by the State of Oregon Department of Assayer-Spectroscopist Gary Baxter. Geology and Mineral Industries (Volumes 1 through 40 were en Effective January 1, 1981, the Department's revised pur titled The Ore Bin). poses and procedures include the following: The laboratory will be primarily research oriented, with the view of providing necessary support for staff geologists in Governing Board a manner analogous to the library, cartographic, and editorial John L. Schwabe, Chairman ................... Portland C. Stanley Rasmussen ........ .. Baker sections of the Department. Allen P. Stinchfield ........................ North Bend The laboratory is continuing its service to the public on routine assays and analyses, but it can no longer perform the State Geologist . .. Donald A. Hull analyses in-house. Instead, gold and silver assays and heavy metal and other analyses are now being farmed 'Out to com Deputy State Geologist ..................... John D. Beaulieu merciallabs on an annual-bid basis. The Department performs random quality-control checks and crushing and grinding. A Editor ................................... BeverlyF. Vogt new price list, schedule, and other procedural instructions will be published at a later date. Main Office: 1005 State Office Building, Portland 97201, phone (503) 229-5580. Departmental lab capabilities continue to be ,oriented toward fire assay, geochemical analysis of metals, future im Baker Field Office: 2033 First Street, Baker 97814, phone (503) provement of geochemical capabilities for soil and rock, and 523-3133. -
Henry Hagg Lake Environmental Assessment and FONSI
FINDING OF NO SIGNIFICANT IMPACT PN FONSI -04-01 ENVIRONMENTAL ASSESSMENT FOR HENRY HAGG LAKE RESOURCE MANAGEMENT PLAN Introduction The U.S. Bureau of Reclamation (Reclamation) has completed a mUlti-year planning and public involvement program for the purpose of preparing a Resource Management Plan (RMP) for Henry Hagg Lake and the surrounding Reclamation lands, known as Scoggins Valley Park. The RMP program is authorized under Title 28 of Public Law 102-575. Reclamation has prepared an Environmental Assessment (EA) of the plan in compliance with the National Environmental Policy Act (NEPA) of 1969. The purpose of the RMP is to manage natural and cultural resources, facilities, and access on Reclamation's lands at Henry Hagg Lake for the next 10 years. This RMP will also serve as guidance for Washington County's (WACO) management of Scoggins Valley Park, Reclamation's public entity, and non-Federal managing partner. Alternatives Considered The National Environmental Policy Act requires Reclamation to explore a reasonable range of alternative management approaches and to evaluate the environmental effects of these alternatives. Three alternatives are evaluated and compared in this document, including a No Action Alternative and a Preferred Alternative. Alternative A - No Action - Continuation of Existing Management Practices. Management would be conducted according to the priorities and projects proposed under the preferred alternative in the 1994 EA for Scoggins Valley Park/Henry Hagg Lake Recreation Development, including camping. Reclamation would continue to adhere to all applicable Federal and State laws, regulations, and executive orders, including those enacted since the 1994 EA was adopted. Alternative B - Minimal Recreation Development with Resource Enhancement_ Alternative B accommodates the increasing demands for recreation at Henry Hagg Lake primarily by expanding and upgrading existing facilities. -
Geologic Formations of Western Oregon
BULLETIN 70 GEOLOGIC fORMATION§ OF WESTERN OREGON WEST OF LONGITUDE 121° 30' STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES 1971 STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES 1069 Stal·e Office Building Portland, Oregon 97201 BULLETIN 70 GEOLOGIC FORMATIONS OF WESTERN OREGON (WEST OF LONGITUDE 12 1 °30') By John D. Beaulieu 1971 GOVERNING BOARD Fayette I. Bristol, Rogue River, Chairman R. W. deWeese, Portland Harold Banta, Baker STATE GEOLOGIST R. E. Corcoran CONTENTS Introduction . Acknowledgements 2 Geologic formations 3 Quadrang I es. 53 Corre I ation charts. 60 Bibliography. 63 ii GE OLOGIC FORMA T IONS OF WESTERN OR EGON (W E ST OF LONG ITUD E 12 1°30') By John D. Beaulieu* INTRODUCTION It is the purpose of th is publi cation to provide a concise , yet comprehensive discussion of the for mations of western Oregon. It is the further aim that the data for each of the formations be as current as possi ble. Consequently, the emphasis has been placed on th e recent literature . Although this paper should not be viewed as a discussion of the historical development of each of the fo rmations, the original reference for each of the units is given . Also, in cases where the historical development of the formation has a direct bearing on present-day problems it is included in the discussion . A wide variety of published literature and unpublished reports , theses, and dissertations was con sul ted and several professional opin ions regarding specific problems were so licited . In recent years re search has been concentrated in the Klamath Mountains and the southern Coast Range and for these regions literature was volumi nous.