DOCSLIB.ORG

New Stratigraphic Markers in the Late Pleistocene Palouse Loess: Novel Fossil Gastropods, Absolute Age Constraints and Non-Aeolian Facies

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
New Stratigraphic Markers in the Late Pleistocene Palouse Loess: Novel Fossil Gastropods, Absolute Age Constraints and Non-Aeolian Facies View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by RERO DOC Digital Library Sedimentology (2009) doi: 10.1111/j.1365-3091.2009.01085.x New stratigraphic markers in the late Pleistocene Palouse loess: novel fossil gastropods, absolute age constraints and non-aeolian facies PATRICK K. SPENCER and ANGELA N. KNAPP1 SHORT Department of Geology, Whitman College, 345 Boyer Avenue, Walla Walla, WA 99362, USA (E-mail: [email protected]) CONTRIBUTION Associate Editor – Nick Eyles ABSTRACT Four stratigraphic sections in the southern part of the Columbia Basin preserve a sequence of aeolian and non-aeolian sediments ranging in age from 9Æ43 to >47Æ0 14C ka based on accelerator mass spectrometry radiocarbon dating of fossil molluscs, geochemistry of Cascade Mountain-sourced tephra and association with formally recognized pedostratigraphic units (the Washtucna and Old Maid Coulee soils). Study sections are interpreted as representing concurrent deposition of loess and distal Missoula Flood rhythmites in valleys tributary to main drainages backflooded during the Missoula Floods, and formation of carbonate and iron-rich soils. Sediments belong to the formally recognized L-1 and L-2 loess units established for the Palouse loess, which were deposited in the Columbia Basin subsequent to events of glacial outburst flooding. Sediments associated with the Mount Saint Helens set S and set C tephras in the study sections preserve a fauna of five species of gastropod mollusc which have not been reported previously from sediments of late Pleistocene age in the Palouse region. The fossils comprise two distinct faunules stratigraphically separated by the Mount Saint Helens So tephra. Accelerator mass spectrometry radiocarbon dating of the fossils collected above the tephra in two of the sections yielded ages of 12Æ48 ± 0Æ06 and 9Æ43 ± 0Æ05 14C kyr. These ages suggest that independent determinations of the 13Æ35 14C kyr age of the So tephra in other areas where Missoula Flood sediments are preserved are probably accurate, and help to refine the age of the latest events in the most recent sequence of catastrophic glacial outburst flooding. Keywords Loess, Missoula Floods, mollusc, Mount Saint Helens, Pleistocene, soils. INTRODUCTION the relative chronology and absolute age of the sequences. While typical stratigraphic indicators Regions sculpted by Quaternary glaciations, such as fossil vertebrates are abundant in the including North America, commonly have cov- Pleistocene Palouse loess of Washington State, ers of thick, undifferentiated loess deposits left they are uncommon in other Quaternary units of behind as signatures of these events. These the north-western USA, such as the Missoula massive loess deposits can be a few to over Flood deposits (Rensberger et al., 1984; Spencer, 100 m thick, making it difficult to discern both 1989). Field work conducted for the present 1Present address: Marine and Atmospheric Chemistry, Rosenstiel School of Marine and Atmospheric Science, University of Miami, 4600 Rickenbacker Causeway, Miami, FL 33149, USA. Ó 2009 The Authors. Journal compilation Ó 2009 International Association of Sedimentologists 1 2 P. K. Spencer and A. N. Knapp report indicates that previously undocumented The sections studied are located approximately fossil terrestrial gastropods are common in cer- 25 km north of Walla Walla, Washington, and are tain facies of the Palouse loess, providing exposed in shallow, ephemeral stream valleys another tool with which to identify and correlate tributary to the Touchet River, and on the drain- geographically discrete loess outcrops. This age divide between the Touchet River and Eureka report provides age, stratigraphic and sedi- Flat to the north. Location of study sections and mentological data and interpretations for four physiographic features mentioned in the text are study sections in southern exposures of the shown in Fig. 1. Palouse loess and documents the stratigraphic and sedimentological context for five species of gastropod mollusc. In addition, absolute age REGIONAL GEOLOGICAL SETTING constraints are established for the gastropod- bearing intervals in the McFeely Road and Piper The bedrock of the Palouse Hills of south-eastern Canyon sections (Fig. 1) based on accelerator Washington comprises a thick sequence of basalt mass spectrometry (AMS) radiocarbon dating of flows assigned to the Miocene Columbia River shell material. Finally, the relationship between Basalt Group (CRBG), which is overlain by, and the study sections and the late Pleistocene interbedded with, several lithostratigraphic units. slackwater deposits generated by the Missoula The Ellensburg Formation (Miocene), exposed in Floods (the Touchet Beds) are interpreted. the western portion of the Columbia Plateau, Fig. 1. Index map of Washington state and study area showing the locations of the study sections in central Walla Walla County and physiographic features mentioned in the text. MSH, Mount St Helens; GP, Glacier Peak. Ó 2009 The Authors. Journal compilation Ó 2009 International Association of Sedimentologists, Sedimentology New stratigraphic markers in the Palouse loess 3 comprises a sequence of tuffaceous fluvial and on the occurrence of small mammal fossils in a lacustrine sediments derived from the rising section spanning at least the last 40 kyr and Cascade Mountains, which was distributed east- perhaps as much as the last 100 kyr. Busacca ward across the developing Yakima fold belt et al. (1992) and McDonald & Busacca (1992) (Smith, 1988). The Miocene to Pliocene Ringold developed a correlation scheme for outcrops of Formation overlies the CRBG in the Pasco Basin younger loess in the southern Channelled Scab- (Fig. 1) and is interpreted as representing depo- land (Fig. 1) based on stratigraphic and sedi- sition by rivers draining the Rocky Mountains mentological features, including stratigraphic (Lindsey, 1990). sequence, soil development and tephra chrono- The CRBG, the Ellensburg Formation and the logy. Busacca & McDonald (1994) recognized Ringold Formation are overlain by an extensive and named two loess units: the L-1 [strati- aeolian silt and sand deposit informally known graphically above the Mount St Helens (MSH) as the Palouse loess. The age of the Palouse set S tephra] and L-2 (stratigraphically below loess varies widely within the Pleistocene and the MSH set S, and including the MSH set C Holocene. Cascade-sourced tephras and palaeo- tephra near its base). The position of the loess magnetism provide absolute and relative age units was defined further with respect to markers in the unit; distinctive carbonate pal- distinctive carbonate palaeosols including the aeosols (for example, the Washtucna and Old Washtucna soil, which occurs beneath the MSH Maid Coulee soils of McDonald & Busacca, set S tephra, the Old Maid Coulee soil, which 1992; Busacca & McDonald, 1994) are useful contains the MSH set C tephra, and the Devil’s physical markers. Interbedded with the Palouse Canyon soil, which forms the lower boundary of loess are at least four, and perhaps as many as the L-2 loess unit. six, distinct sedimentary sequences representing periods of catastrophic glacial outburst flooding (McDonald & Busacca, 1988, 1992; Busacca & STRATIGRAPHIC AND McDonald, 1994; Bjornstadt et al., 2001; Spen- SEDIMENTOLOGICAL CONTEXT OF cer & Jaffee, 2002). The most recent flood STUDY SECTIONS sequence originated at glacial Lake Missoula in western Montana and is known as the Missoula Ayer Road section Floods; earlier flood sequences are of unknown origin. Flood sequences are distinguishable from The Ayer Road section (Figs 1 and 2) comprises each other by bounding unconformities (Spen- about 15 m of massive silt and fine sand with cer & Jaffee, 2002); sedimentary textures and multiple horizons of carbonate soil and three structures distinguish them from the associated recognizable tephras, exposed at an elevation of loess. about 385 m. Based on the identity of soils The Palouse loess comprises a thick and and associated tephras, the Ayer Road section monotonous sequence of fine-grained aeolian includes the L-1 and L-2 loess of Busacca & sediment derived from the Pasco Basin to the McDonald (1994), as well as the upper portion of west of the Palouse region (McDonald & Bus- an older, unnamed silt unit. acca, 1992; Busacca & McDonald, 1994). Sites One of the soils is identified as the Washtucna studied for this report show that, in central soil (of McDonald & Busacca, 1992) based on Walla Walla County, the loess is associated with distinctive morphological features, such as stage sediment deposited by non-aeolian processes; of soil development and close association of two stratification, graded bedding and variations in stacked soils, and its stratigraphic position above texture indicate aqueous deposition for these a tephra identified as an MSH set C and below a occurrences. tephra identified as an MSH set S (see Table 1 for tephra glass compositions). A second soil is identified as the Old Maid Coulee soil by its STRATIGRAPHIC AND association with the MSH set C tephra. A third PALAEONTOLOGICAL FRAMEWORK tephra consisting of a dark grey, fine-grained, FOR THE PALOUSE LOESS indistinct layer occurs beneath the MSH set C. The distinctive physical appearance and strati- Rensberger et al. (1984) established a biostrati- graphic position of this tephra beneath the set C graphic framework for the Palouse loess and tephra and the Old Maid Coulee soil make it a provided ecological and taxonomic data, based useful marker.
Load more

Recommended publications
  • 1922 Elizabeth T
    co.rYRIG HT, 192' The Moootainetro !scot1oror,d The MOUNTAINEER VOLUME FIFTEEN Number One D EC E M BER 15, 1 9 2 2 ffiount Adams, ffiount St. Helens and the (!oat Rocks I ncoq)Ora,tecl 1913 Organized 190!i EDITORlAL ST AitF 1922 Elizabeth T. Kirk,vood, Eclttor Margaret W. Hazard, Associate Editor· Fairman B. L�e, Publication Manager Arthur L. Loveless Effie L. Chapman Subsc1·iption Price. $2.00 per year. Annual ·(onl�') Se,·ent�·-Five Cents. Published by The Mountaineers lncorJ,orated Seattle, Washington Enlerecl as second-class matter December 15, 19t0. at the Post Office . at . eattle, "\Yash., under the .-\0t of March 3. 1879. .... I MOUNT ADAMS lllobcl Furrs AND REFLEC'rION POOL .. <§rtttings from Aristibes (. Jhoutribes Author of "ll3ith the <6obs on lltount ®l!!mµus" �. • � J� �·,,. ., .. e,..:,L....._d.L.. F_,,,.... cL.. ��-_, _..__ f.. pt",- 1-� r�._ '-';a_ ..ll.-�· t'� 1- tt.. �ti.. ..._.._....L- -.L.--e-- a';. ��c..L. 41- �. C4v(, � � �·,,-- �JL.,�f w/U. J/,--«---fi:( -A- -tr·�� �, : 'JJ! -, Y .,..._, e� .,...,____,� � � t-..__., ,..._ -u..,·,- .,..,_, ;-:.. � --r J /-e,-i L,J i-.,( '"'; 1..........,.- e..r- ,';z__ /-t.-.--,r� ;.,-.,.....__ � � ..-...,.,-<. ,.,.f--· :tL. ��- ''F.....- ,',L � .,.__ � 'f- f-� --"- ��7 � �. � �;')'... f ><- -a.c__ c/ � r v-f'.fl,'7'71.. I /!,,-e..-,K-// ,l...,"4/YL... t:l,._ c.J.� J..,_-...A 'f ',y-r/� �- lL.. ��•-/IC,/ ,V l j I '/ ;· , CONTENTS i Page Greetings .......................................................................tlristicles }!}, Phoiitricles ........ r The Mount Adams, Mount St. Helens, and the Goat Rocks Outing .......................................... B1/.ith Page Bennett 9 1 Selected References from Preceding Mount Adams and Mount St.
    [Show full text]
  • Washington Division of Geology and Earth Resources Open File Report 74-1
    TEPHRA OF SALMON SPRINGS AGE FROM THE SOUTHEASTERN OLYMPIC PENINSULA, WASHINGTON by R. U. BIRDSEYE and R. J. CARSON North Carolina State University WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES OPEN FILE REPORT 74-1 1974 This report has not been edited or reviewed for conformity with Division of Geology and Earth Resources standards and nomenclature Revised October, 1989 CONTENTS Page Abstract •.•................••......••........•.......•............• 1 Introduction ....................................................... 1 Acknowledgments •••••••••••••••••••••••••••••••••••••••••••••••••••• 1 Pleistocene climate, glaciation, and volcanism ••••••••••••••••••••• 2 The ashes: Their thickness, distribution, and stratigraphic position •••••••••••••••••••••••••••••••••••••••••• 7 Color and texture of the ash ••••••••••••••••••••••••••••••••••••••• 14 Deposition of the ash •••••••••••••••••••••••••••••••••••••••••••••• 14 Atmospheric conditions during deposition of the ash •••••••••••••••• 20 Usefulness of volcanic ash in stratigraphic determination •••••••••• 21 Canel us ion ....•••.•..••••.••..••......•.••••••.••••....•••••...••.. 21 References cited ••••••••••••••••••••••••••••••••••••••••••••••••••• 23 ILLUSTRATIONS Figure 1 - Maximum extent of the Cordilleran ice sheet •••••••••••• 3 Figure 2 - Summary of late Pleistocene events in western Washington ••••••••••••••••••••••••••••••••••••• 4 Figure 3 - Location map showing inferred extent of minimum areas of fallout of volcanic ash from eruptions of Mount Mazama and Glacier Peak •••••••••••••••••••••••
    [Show full text]
  • The Historic Winnemucca to the Sea Highway “Gateway to the Pacific Northwest”
    Feb 2004 WINNEMUCCA to the SEA Highway The Historic Winnemucca to the Sea Highway “Gateway to the Pacific Northwest” John Ryczkowski The Winnemucca to the Sea highway was developed to establish a continu- ous, improved all-weather highway from US-40 (I-80) at Winnemucca, Nevada through Medford, Oregon and on to the Pacific coast at Crescent City, California. In the mid 1950’s there was no direct route west from Northern Nevada across South- ern Oregon and into California’s Redwood Empire. Community leaders from points along this proposed link formed the Winnemucca to the Sea Highway Association. The association worked with state and local governments to fund the design, con- struction and upgrade of the paved roadway for this east to west link across three states. The association had envisioned one highway number 140 applied to the complete route, as the parent major US highway was coast-to-coast US-40, the Victory Highway. Nevada and Oregon used state route 140 for their respective sections of the Winnemucca to the Sea Highway. But the renumbering or cosigning of federal highways was an obstacle that the Winnemucca to the Sea Association never did overcome, thus the hope of a continuous 140 designation for this link was never realized. Currently the traveler will follow seven different highway numbers from Winnemucca to Crescent City, they are US-95, state route-140, US-395, state Association brochure circa 1960’s route-62, Interstate-5, US-199 and US-101. Winnemucca, named after a local Paiute chief, has always been a crossroads town.
    [Show full text]
  • Geology of the Northern Part of the Southeast Three Sisters
    AN ABSTRACT OF THE THESIS OF Karl C. Wozniak for the degree of Master of Science the Department cf Geology presented on February 8, 1982 Title: Geology of the Northern Part of the Southeast Three Sisters Quadrangle, Oregon Redacted for Privacy Abstract approved: E. M. Taylorc--_, The northern part of the Southeast Three Sisters quadrangle strad- dles the crest of the central High Cascades of Oregon. The area is covered by Pleistocene and Holocene volcanic and volcaniclastic rocks that were extruded from a number of composite cones, shield volcanoes, and cinder cones. The principal eruptive centers include Sphinx Butte, The Wife, The Husband, and South Sister volcanoes. Sphinx Butte, The Wife, and The Husband are typical High Cascade shield and composite vol- canoes whose compositions are limited to basalt and basaltic andesite. South Sister is a complex composite volcano composed of a diverse assem- blage of rocks. In contrast with earlier studies, the present investi- gation finds that South Sister is not a simple accumulation of andesite and dacite lavas; nor does the eruptive sequence display obvious evolu- tionary trends or late stage divergence to basalt and rhyolite. Rather, the field relations indicate that magmas of diverse composition have been extruded from South Sister vents throughout the lifespan of this volcano. The compositional variation at South Sister is. atypical of the Oregon High Cascade platform. This variation, however, represents part of a continued pattern of late Pliocene and Pleistocene magmatic diver- sity in a local region that includes Middle Sister, South Sister, and Broken Top volcanoes. Regional and local geologic constraints combined with chemical and petrographic criteria indicate that a local subcrustal process probably produced the magmas extruded fromSouth Sister, whereas a regional subcrustal process probably producedthe magmas extruded from Sphinx Butte, The Wife, and The Husband.
    [Show full text]
  • Rogue Valley Community Resource Directory
    211 Info & ADRC…………………………………………..……………………. Page 1 Advocacy …………………………………………..……………………………… Page 2 Children and Family Services …………………………………………….. Page 3 Clothing …………………………………………..………………………………… Page 5 Crisis Hotline …………………………………………..………………………… Page 6 Dental …………………………………............................................. Page 8 Drug & Alcohol Abuse …………………………..………………………….. Page 9 Emergency Services …………………………..……………………………… Page 12 Emergency Shelters & Meals ……………..……………………………… Page 14 Employment Resources …………………………..……………………….. Page 16 Energy/Weatherization Assistance ……………..……………………. Page 17 Family Resources …………………………..………………………………… Page 18 Farm Direct Program …..……………………………………………………. Page 24 Farmers Market …………………………..………………………………..… Page 26 Food Assistance & Pantry ………………..………………………………….. Page 27 General Mail Delivery Information …………………………………... Page 33 Health and Medical Services …………………………………............. Page 34 Human Services, Dept. …………………………………..................... Page 38 Legal Services Information …………………………………................ Page 40 Low Income Housing Information …………………………………..... Page 41 Non-Emergency Medical Care …..……………………………….......... Page 42 Organizations .………………………………….................................... Page 43 Rental & Utilities Assistance…………………………………............... Page 80 Soup Kitchens …………………………………..................................... Page 81 Transportation …………………………………................................... Page 82 Veterans Services…………………………………............................... Page 83 211 INFO & ADRC 211 INFO 211Info
    [Show full text]
  • Weather and Climate of the Rogue Valley by Gregory V
    Weather and Climate of the Rogue Valley By Gregory V. Jones, Ph.D., Southern Oregon University The Rogue Valley region is one of many intermountain valley areas along the west coast of the United States. Nestled in the southwestern portion of Oregon, the landscape of the Rogue Valley is extremely diverse, coming from the joining of three mountain ranges of varying ages and structure: the Klamath and Siskiyou Mountains to the southwest to southeast, the Coastal Range to the west, and the Cascades to the east and north. The region is drained mainly by the Rogue River and its major tributaries; the Applegate River, the Illinois River, and Bear Creek. At the largest scale, the weather and climate of the region is mainly influenced by the North Pacific Ocean and the westerly winds of the mid-latitudes. The maritime air masses that originate over the Pacific are cooled by the ocean currents offshore and moderate the climate of the region. Seasonally the west coast undergoes shifts between cooler, moister conditions in the winter with a strengthening of the Aleutian Low that brings storms into the region; to warmer, drier conditions in the summer that are associated with the dominance of the Pacific High. On a regional scale, the general north-south or northwest-southeast oriented valleys, with their proximity to the Pacific Ocean and the number and height of mountain barriers, help to create climate conditions of wetter and cooler areas in the western parts of the region and warmer and drier eastern areas. At the local scale, site differences in elevation, topography, and orientation to the sun influence the variation in gardening potential.
    [Show full text]
  • Crater Lake National Park Oregon
    DEPARTMENT OF THE INTERIOR HUBERT WORK. SECRETARY NATIONAL PARK SERVICE STEPHEN T. MATHER. DIRECTOR RULES AND REGULATIONS CRATER LAKE NATIONAL PARK OREGON PALISADE POINT, MOUNT SCOTT IN THE DISTANCE 1923 Season from July 1 to September 30 THE PHANTOM SHIP. FISHING IS EXCELLENT IN CRATER LAKE. THE NATIONAL PARKS AT A GLANCE. [Number, 19; total area, 11,372 square miles.] Area in National parks in Distinctive characteristics. order of creation. Location. squaro miles. Hot Springs Middle Arkansas li 40 hot springs possessing curative properties- 1832 Many hotels and boarding houses—20 bath­ houses under public control. Yellowstone Northwestern Wyo­ 3.348 More geysers than in all rest of world together- 1872 ming. Boiling springs—Mud volcanoes—Petrified for­ ests—Grand Canyon of the Yellowstone, remark­ able for gorgeous coloring—Large lakes—Many largo streams and waterfalls—Vast wilderness, greatest wild bird and animal preserve in world— Exceptional trout fishing. Sequoia. Middle eastern Cali­ 252 The Big Tree National Park—several hundred 1S90 fornia. sequoia trees over 10 feet in diameter, some 25 to 36 feet, hi diameter—Towering mountain ranges- Startling precipices—Mile long cave of delicate beauty." Yosemito Middle eastern Cali­ 1,125 Valley of world-famed beauty—Lofty chits—Ro­ 1890 fornia. mantic vistas—Many waterfalls of extraordinary height—3 groves of big trees—High Sierra— Waterwhcol falls—Good trout fishing. General Grant Middle eastern Cali­ 4 Created to preserve the celebrated General Grant 1S90 fornia. Tree, 3* feet in diameter—6 miles from Sequoia National Park. Mount Rainier ... West central Wash­ 321 Largest accessible single peak glacier system—28 1899 ington.
    [Show full text]
  • Volcanic Hazards • Washington State Is Home to Five Active Volcanoes Located in the Cascade Range, East of Seattle: Mt
    CITY OF SEATTLE CEMP – SHIVA GEOLOGIC HAZARDS Volcanic Hazards • Washington State is home to five active volcanoes located in the Cascade Range, east of Seattle: Mt. Baker, Glacier Peak, Mt. Rainier, Mt. Adams and Mt. St. Helens (see figure [Cascades volcanoes]). Washington and California are the only states in the lower 48 to experience a major volcanic eruption in the past 150 years. • Major hazards caused by eruptions are blast, pyroclastic flows, lahars, post-lahar sedimentation, and ashfall. Seattle is too far from any volcanoes to receive damage from blast and pyroclastic flows. o Ash falls could reach Seattle from any of the Cascades volcanoes, but prevailing weather patterns would typically blow ash away from Seattle, to the east side of the state. However, to underscore this uncertainty, ash deposits from multiple pre-historic eruptions have been found in Seattle, including Glacier Peak (less than 1 inch) and Mt. Mazama/Crater Lake (amount unknown) ash. o The City of Seattle depends on power, water, and transportation resources located in the Cascades and Eastern Washington where ash is more likely to fall. Seattle City Light operates dams directly east of Mt. Baker and in Pend Oreille County in eastern Washington. Seattle’s water comes from two reservoirs located on the western slopes of the Central Cascades, so they are outside the probable path of ashfall. o If heavy ash were to fall over Seattle it would create health problems, paralyze the transportation system, destroy many mechanical objects, endanger the utility networks and cost millions of dollars to clean up. Ash can be very dangerous to aviation.
    [Show full text]
  • Southern Oregon Development Opportunity Approximately 210 Acre Mixed-Use Development Property in Medford, Oregon
    Southern Oregon Development Opportunity Approximately 210 Acre Mixed-Use Development Property in Medford, Oregon William L. Leever | Principal Broker Mike Malepsy | Principal Broker/Owner Pulver & Leever Real Estate Company Windermere Trails End Real Estate, LLC Office: 541-773-5391 | Cell: 541-601-2752 Office: 541-878-2249 | Cell: 541-840-1424 [email protected] [email protected] Total Project Size: Approximately 210 Acres Developable Acreage: Approximately 166.5 Acres • 105 acres of residential development land • 61.5 acres of commercial development land • 20 acres to be donated to the Medford School District • 23.5 acres to be donated to the Medford Parks & Recreation Officially located within Medford’s Urban Growth Boundary The Offering Urbanization and Annexation process currently in progress One-of-a-kind development opportunity in beautiful Southern Oregon now available! The property is located within the newly-amended Coker Butte Development Urban Growth Boundary with a conceptual master development plan Price: $18,900,000 in place. Southern Oregon has experienced tremendous growth with extremely high demand for new housing and commercial property. 2 Coker Butte Development Opportunity Conceptual Site Plan Medford is located on Interstate 5, midway between San Francisco and Portland and serves as Southern Oregon’s anchor of commerce and tourism. LEGEND COKER BUTTE DEVELOPMENT Civil Engineering CONCEPTUAL SITE PLAN Water Rights Coker Butte Development Opportunity 3 Project Overview Project Summary Transportation Presenting a rare opportunity to acquire a sizeable mixed-use develop- The proposed Coker Butte Development is supported by a strong ment property in Southern Oregon! Known as Coker Butte Development, network of higher and lower order streets that intertwine to provide suffi- the project is the result of the recent culmination of a years-long regional cient capacity for a fully-developed residential and commercial mixed-use planning process.
    [Show full text]
  • Tour of Honor, Southern Oregon's Fabulous
    Court Boice, Commissioner David Brock Smith Oregon State Rep. Dist. 1 [email protected] [email protected] 541-247-3229 541-253-7506 Tour of Honor, Southern Oregon’s Fabulous Veteran Memorials … Visit the Curry “Veterans Memorial”. Then south into the tip of California, Hwy 97 through the California Redwoods to Hwy 199 following the Smith River Canyon. Next to Central Point’s “Fallen War Heroes Memorial”. From Central Point go to the Eagle Point’s Veterans National Cemetery. On to Merlin’s “Walk of Honor”, and then back to Interstate 5 and on to Roseburg’s “VFW Remembrance Wall”. Travel Highway 38 along the Umpqua River to the Oregon Coast and the North Bend Veterans Memorial. Finally head south, returning to Gold Beach via Hwy 101. Gold Beach Curry County Veterans MeMorial Location: 94199 Hwy 101 S., Gold Beach 97444 “Remember their sacrifice” Central Point oregon Fallen War Heroes MeMorial Location: 222 W Vilas Rd, Central Point 97520 “Honoring all those servicemen, living and dead, who served our nation” Eagle Point Veterans national CeMetery Location: 2763 Riley Rd. Eagle Point 97524 “A memorial dedicated to All known and Unknown Veterans” Merlin Veterans Walk oF Honor and MeMorial Location: Merlin-Galice Road, Merlin Community Park 97532 “We shall never forget” Roseburg Veterans oF Foreign Wars reMeMbranCe Wall Location: 127 Walnut Street, Roseburg 97470 “Honoring those who so honorably served the cause of freedom” North Bend daVid deWitt Veterans MeMorial Location: US Hwy 101, North Bend 97459 “Peace comes when the power of Love overcomes the Love of power” IMPORTANT ADDITIONAL VETERAN MEMORIALS AND PARKS IN SOUTHWEST OREGON … Rogue River A memorial in memory of veterans from Jackson County who were killed during the Vietnam War and also the Korean War Memorial.
    [Show full text]
  • Yakama-Cowlitz Trail: Ancient and Modern Paths Across the Mountains
    COLUMBIA THE MAGAZINE OF NORTHWEST HISTORY ■ SUMMER 2018 Yakama-Cowlitz Trail: Ancient and modern paths across the mountains North Cascades National Park celebrates 50 years • Explore WPA Legacies A quarterly publication of the Washington State Historical Society TWO CENTURIES OF GLASS 19 • JULY 14–DECEMBER 6, 2018 27 − Experience the beauty of transformed materials • − Explore innovative reuse from across WA − See dozens of unique objects created by upcycling, downcycling, recycling − Learn about enterprising makers in our region 18 – 1 • 8 • 9 WASHINGTON STATE HISTORY MUSEUM 1911 Pacific Avenue, Tacoma | 1-888-BE-THERE WashingtonHistory.org CONTENTS COLUMBIA The Magazine of Northwest History A quarterly publication of the VOLUME THIRTY-TWO, NUMBER TWO ■ Feliks Banel, Editor Theresa Cummins, Graphic Designer FOUNDING EDITOR COVER STORY John McClelland Jr. (1915–2010) ■ 4 The Yakama-Cowlitz Trail by Judy Bentley OFFICERS Judy Bentley searches the landscape, memories, old photos—and President: Larry Kopp, Tacoma occasionally, signage along the trail—to help tell the story of an Vice President: Ryan Pennington, Woodinville ancient footpath over the Cascades. Treasurer: Alex McGregor, Colfax Secretary/WSHS Director: Jennifer Kilmer EX OFFICIO TRUSTEES Jay Inslee, Governor Chris Reykdal, Superintendent of Public Instruction Kim Wyman, Secretary of State BOARD OF TRUSTEES Sally Barline, Lakewood Natalie Bowman, Tacoma Enrique Cerna, Seattle Senator Jeannie Darneille, Tacoma David Devine, Tacoma 14 Crown Jewel Wilderness of the North Cascades by Lauren Danner Suzie Dicks, Belfair Lauren14 Danner commemorates the 50th22 anniversary of one of John B. Dimmer, Tacoma Washington’s most special places in an excerpt from her book, Jim Garrison, Mount Vernon Representative Zack Hudgins, Tukwila Crown Jewel Wilderness: Creating North Cascades National Park.
    [Show full text]
  • Property for Sale in Coos Bay Oregon
    Property For Sale In Coos Bay Oregon Quality Francisco never instantiates so demurely or readdresses any vulgates sky-high. Inhuman Rad feoffs very imputatively while Manish remains supine and myrmecological. Sweet-tempered Tobe shedding her constitutionalist so subaerially that Woodrow utters very soapily. Possible for sale on bay oregon international realty family, cattle ranch land and number of. Down arrow keys to coos bay properties for! As well for sale includes childcare, oregon coast development council, duplex in this data based on. We would be with your best people. Find Coos Bay OR homes for figure and made other interesting real estate related information like from home prices average rent prices and home price to. You for sale includes business! When it occupies the properties for sale on the rogue valley mls of cottage grove, there is protected by selecting the. Coos County me Commercial Real Estate for Sale & Lease. Close by calapooia clay pottery studio, fishing vessels proudly owned and land is at the first home in the willamette town never before making sure the. Coos Bay homes for let range from 30K 14M with the avg price of a 2-bed single new home of 275K Coos Bay in real estate listings updated every 15min. Steve helped us decide to coos bay in oregon property for sale on large apartment above garage. This property sales for the property in place the current owner. With property in coos bay properties, negotiated and cares about site visitors: today for winter sports. Coos County Real Estate Listings Homes for god The hump is open.
    [Show full text]