Palouse River Map

Total Page:16

File Type:pdf, Size:1020Kb

Palouse River Map Palouse river map Continue <<< back to Palouse River homepage MAP LEGEND: Blue Dot = Put on, Red Point = Remove (Above the map supplied by Wanan W., copyright ©.) Putin Location GPS COORDINATES:Latitude: 46.66098Long: -118.22783Takeout Location COORDINATED GPS:Latitude: 46.59853Long: -118.21803 HIGH QUALITY TOPO MAP, CLICK HERE Best Western Plus Dayton Hotel && Suites, Dayton 22.4 miles from Best Western Bronco Inn, Ritzville 25.7 miles from Days Inn Ritzville, Ritzville 28.6 miles from Super 8 Walla Walla, Walla Walla 26.7 miles from Red Lion Inn && Suites Walla Wa, Walla Walla 27.6 miles from Quality Inn && Suites Walla Walla, Walla Walla 27.8 miles from Best Western Plus Walla Walla Suites Inn, Walla Walla 27.8 miles from Marcus Whitman Hotel And Conference Center, Walla Walla 27.9 miles from The Inn At Abe Walla Walla, Walla Walla 28.1 miles from Azure Mountain View Inn, Walla Walla 28.7 miles from Courtyard Walla Walla, Walla Walla 28.7 miles from Holiday Inn Express WALLA WALLA , Walla Walla 28.6 miles from Comfort Inn & Walla Suites, Walla Walla 28.6 miles from La Quinta Inn && Suites Walla Walla, Walla Walla 46 km from Hampton Inn - Suites Walla Walla, Walla Walla at 47 km * The distances listed are direct linear distances, the actual distance of the trip may be different. Palouse RiverSeveral miles downstream from its fork in Colfax; looking west in 2007The mouth of the RiverPalouse in WashingtonLocationCountryUnited StatesStateWashington, IdahoCountyFranklin, Whitman, Adams, Latah Physical featuresSource:Supplied -116.4587[1] MouthSnake River • coordinates46°35′24N 118°12′55O / 46.59000°N 118.21528°O / 46.59000; -118.21528Coordinates: 46°35′24N 118°12′55O / 46.59000°N 118.21528°O / 46.59000; -118.21528[1] • elevation of 165 meters (165 m) (269 km) Basin size of 8,550 km²[2] • average of 17.0 m3/s [3][5] • minimum 0 m3/s • maximum 33,500 feet/s (950 m3/s) The Palouse River is a tributary of the Snake River in Washington and Idaho in the northwestern United States. It flows for 269 km to the southwest, mainly through the Palouse region in southeast Washington. It is part of the Columbia River basin, as the Snake River is a tributary of the Columbia River. Its barrel was cut off by a fork in the catastrophic Missoula floods of the previous ice age, which spilled over the northern Columbia plateau and flowed into the Snake River, eroding the river's current course in a few thousand years. Palouse Falls Course in 2006 Palouse River entering the snake on the Lyon ferry near Starbuck, looking north in 2006 The Palouse River flows from northern Idaho to Southeast Washington the Palouse region, named for the river. The river originates in Idaho, northeast of Latah County, in the Hoodoo Mountains in the St. Joe's National Forest. In Washington, the river flows into Whitman County to Palouse and then to Colfax, where it meets its southern fork, which originates on the southern slopes of Moscow Mountain in the Palouse Range, flowing south from Moscow and west to Pullman. (Paradise Creek parallel to the South Fork, passing through Moscow to Pullman, accompanied by the Bill Chipman Palouse Trail and State Route 270.) From Colfax, the river meanders to the west and ends up on the lower Snake River southwest of Hooper, but not before falling over Palouse Falls. The Palouse River enters the Snake River below the Little Goose Dam and above the lower monumental dam. Basin and discharge The drainage basin of the Palouse River is 8,550 km². [2] Its average annual discharge, measured by USGS gage 13351000 at Hooper (river mile 19.6), is 599 cubic feet per second (17 m3/s), with a daily maximum recorded flow of 27,800 feet/s (787 m3/s), and a minimum zero flow. [3] Geology The Missoula floods that periodically spread across eastern Washington and across the Columbia River plateau during the Pleistocene era cut the canyon of the Palouse River, which is 300 meters deep in places. [8] The ancient Palouse River flowed through the now dry Washtucna Coulee directly into the Columbia River. The current canyon was created when the Missoula floods overcame the northern drainage divide of the ancestral Palouse River, diverting it to the current course to the Snake River eroding a new deeper channel. [10] The area is characterized by coulees, cataracts, plunge pools, kolk-created potholes, rock benches, butts and pinnacles typical of the scales. [9] See also rivers portal Palouse Falls State Park List of Idaho's longest streams List of Washington Tributaries rivers of the Columbia River References ^ a b c Palouse River. Geographic name information system. United States Geological Survey. September 10, 1979. Retrieved 30 June 2010. ^ 1,0 1,1 Palouse Subbasin Plan Archived 2012-02-13 at Wayback Machine, Northwest Power and Conservation Council ^ a b c Water Resources Data, Water Year 2005; Snake River basin including the Rio Grande Ronde, Asotin Creek, tucannon, and Palouse River basins; 13351000 Palouse River in Hooper, WA (PDF). United States Geological Survey. Retrieved 2 June 2009. ^ Usgs 13351000 Palouse River at Hooper, WA. USGS. Retrieved 16 May 2018. ^ Usgs 13351000 Palouse River at Hooper, WA. USGS. Retrieved 16 May 2018. ^ U.S. Geological Survey. Flow Data resolution of the national hydrography data set. The National Map, accessed 3 May 2011 ↑ ↑ b Carson, Robert J.; In 1996, Kevin R. was the first to do so. Basalt floods and glacier flooding: road geology in parts of Walla Walla, Franklin and Columbia counties, Washington. Washington State Department of Natural Resources (Washington Geology Division and Circular 90 Land Resources Information). ISBN boss. ^ Alt, David, United States of America Glacial Lake Missoula and its humongous floods. Mountain Press Publishing House. ^ Bjornstad, Bruce (2006). In the path of ice age flooding: a geological guide to the Middle Columbia Basin. Keokee Books; Sandpoint, Idaho. ^ David & David & 4.6 4.6 4.6 4.6 4.6 4.6 4.6 4.6 4.6 4.6 4.6 4.6 4.6 Hyndman, Donald (1984). Washington Road Geology. Mountain Press Publishing House. Wikimedia Commons has media related to Palouse River U.S. Geological Survey Geographic Names Information System: North Fork Palouse River U.S. Geological Survey Geographic Names Information System: South Fork Palouse River Palouse River Fishing Palouse Falls Soil Erosion at Palouse River Watershed Recovered from Palouse River is a tributary of the Snake River in Washington and Idaho in the northwestern United States. It flows for 167 miles to the southwest, mainly through the ﻧﻬﺮ ﺑﺎﻟﻮس :Palouse region of Southeast Washington. Type: Stream Description: river in the United States of America Category: river Location: Washington, Pacific Northwest, United States, North America Latitude: 46.5899° or 46° 35' 23.5 north Longitude: -118.2152° or 118° 12' 54.9 west Elevation: 165 metres (541 feet) GeoNames ID: 5806098 Arabic Irish: Abhainn Palouse Italian: Fiume Palouse Italian: Palouse Japanese: パルース川 Russian: Палус Ukrainian: Палус Welsh: Afon Palouse נהר פאלוז :French: Palouse French: Palouse River German: Palouse River Hebrew ﻧﻬﺮ ﭘﺎﻟﻮس :Cebuano: Palouse River Chinese: 帕卢斯河 Chinese: 帕盧斯河 Chuvash: Палус Dutch: Palouse River Egyptian Arabic Drewyers River Drouillard River Flag River Moh-Ha-Na-She North Fork Palouse River Pavilion River Pavion River Pelouse River Peluse River Matoo RiverStream, Manitoba, Canada KogaStream, Khantia-Mansia, Russia Chamabonda VleiStream, Zimbabwe Big Sheep CreekStream , Oregon, United States Little BranchStream, Florida, United States Sarty BrookStream, Nova Scotia, Canada A trip is best measured in friends, rather than miles. - Tim Cahill Seattle Puget Sound King County Kitsap Peninsula MapcartaThe world maps your world iswithout borders The Palouse River is a tributary of the Snake River located in the U.S. states of Washington and Idaho. It flows for 269 km to the southwest, mainly through the Palouse region, washington. It is part of the Columbia River basin, as the Snake River is a tributary of the Columbia River. Headquarters Headquarters It was cut off by a fork in the catastrophic Missoula floods of the previous ice age, which spilled over the northern Columbia plateau and flowed into the Snake River, eroding the river's current course in a few thousand years. Create custom printed map Print this map | View caption Map Provided by TopoZone.com Coordinates: 46.5898667°N, -118.2152421°W Approx. Elevation: 165 meters (165 meters) USGS Topo Quad Map: Starbuck West Feature Type: Stream Palouse River is in the Category of Streams for Franklin County in Washington State. Palouse River is shown on a four-topo map of Starbuck West USGS. Anyone interested in visiting the Palouse River can print the free topographic map and street map using the link above. The coordinates of latitude and longitude of the Palouse River are 46.5898667, -118.2152421 and the approximate elevation is 165 meters above sea level. If you have visited the Palouse River before, please tell us with a comment below. Comments NATIONAL WATER QUALITY MONITORING COUNCIL Working Together for Clean Water WQP Home > Providers > NWIS > USGS-WA > USGS-13348000 Data Provider: NWIS (More information about water quality portal data providers) This flow site, maintained by the USGS Washington Water Science Center (USGS-WA identifier), is named AFTER SOUTH FORK PALOUSE RIVER AT PULLMAN , WA and has ID USGS-13348000. This site is located in the basin defined by the 8-digit Hydrological Unit Code (HUC) 17060108. You can learn more about what's happening at this HUC on the EPA's surf site Your Watershed or on the USGS science site in your watershed.
Recommended publications
  • Washington Division of Geology and Earth Resources Open File Report
    RECONNAISSANCE SURFICIAL GEOLOGIC MAPPING OF THE LATE CENOZOIC SEDIMENTS OF THE COLUMBIA BASIN, WASHINGTON by James G. Rigby and Kurt Othberg with contributions from Newell Campbell Larry Hanson Eugene Kiver Dale Stradling Gary Webster Open File Report 79-3 September 1979 State of Washington Department of Natural Resources Division of Geology and Earth Resources Olympia, Washington CONTENTS Introduction Objectives Study Area Regional Setting 1 Mapping Procedure 4 Sample Collection 8 Description of Map Units 8 Pre-Miocene Rocks 8 Columbia River Basalt, Yakima Basalt Subgroup 9 Ellensburg Formation 9 Gravels of the Ancestral Columbia River 13 Ringold Formation 15 Thorp Gravel 17 Gravel of Terrace Remnants 19 Tieton Andesite 23 Palouse Formation and Other Loess Deposits 23 Glacial Deposits 25 Catastrophic Flood Deposits 28 Background and previous work 30 Description and interpretation of flood deposits 35 Distinctive geomorphic features 38 Terraces and other features of undetermined origin 40 Post-Pleistocene Deposits 43 Landslide Deposits 44 Alluvium 45 Alluvial Fan Deposits 45 Older Alluvial Fan Deposits 45 Colluvium 46 Sand Dunes 46 Mirna Mounds and Other Periglacial(?) Patterned Ground 47 Structural Geology 48 Southwest Quadrant 48 Toppenish Ridge 49 Ah tanum Ridge 52 Horse Heaven Hills 52 East Selah Fault 53 Northern Saddle Mountains and Smyrna Bench 54 Selah Butte Area 57 Miscellaneous Areas 58 Northwest Quadrant 58 Kittitas Valley 58 Beebe Terrace Disturbance 59 Winesap Lineament 60 Northeast Quadrant 60 Southeast Quadrant 61 Recommendations 62 Stratigraphy 62 Structure 63 Summary 64 References Cited 66 Appendix A - Tephrochronology and identification of collected datable materials 82 Appendix B - Description of field mapping units 88 Northeast Quadrant 89 Northwest Quadrant 90 Southwest Quadrant 91 Southeast Quadrant 92 ii ILLUSTRATIONS Figure 1.
    [Show full text]
  • Palouse River Tributaries Subbasin Assessment and TMDL
    Palouse River Tributaries Subbasin Assessment and TMDL Idaho Department of Environmental Quality January 2005 This Page Intentionally Left Blank. Palouse River Tributaries Subbasin Assessment and TMDL January 2005 Prepared by: Robert D. Henderson Lewiston Regional Office Idaho Department of Environmental Quality 1118 F. Street Lewiston, ID 83501 This Page Intentionally Left Blank. Palouse River Tributaries Subbasin Assessment and TMDL January 2005 Acknowledgments Completing this Subbasin Assessment and TMDL would not have been possible without the support of the following individuals and organizations: • Mark Shumar • Alan Monek • Brock Morgan • Barbara Anderson • Dennis Meier • Palouse River Watershed Advisory Group • Tom Dechert • Cary Myler • Jason Fales • William Kelly • John Cardwell • Ken Clark • Bill Dansart • Richard Lee • John Gravelle • Marti Bridges • Daniel Stewart Thank you! Cover photo by Robert D. Henderson i Palouse River Tributaries Subbasin Assessment and TMDL January 2005 This Page Intentionally Left Blank. ii Palouse River Tributaries Subbasin Assessment and TMDL January 2005 Table of Contents Abbreviations, Acronyms, and Symbols .......................................................xiii Executive Summary........................................................................................xvii Subbasin at a Glance .................................................................................................xvii Key Findings .............................................................................................................
    [Show full text]
  • Palouse River and Coulee City Rail Line
    Palouse River and Coulee City Rail Line Palouse River and Coulee City Rail Line For More Information: Mike Rowswell WSDOT State Rail and Marine Office [email protected] 360-705-7900 360-705-7930 www.wsdot.wa.gov/rail www.wsdot.wa.gov/projects/rail/PCC_Acquisition/ WSDOT State Rail and Marine Office The Palouse River and Coulee PO Box 47407 City (PCC) rail line is the state’s Olympia, WA 98504-7407 longest short-line freight rail system and spans four counties in eastern Washington. In 2007, the Washington State Department of Transportation (WSDOT) completed the purchase of this rail line to save it from abandonment. January 2008 Palouse River and Coulee City Rail Line What is the Palouse River and Coulee City deteriorated over time. After attempting to develop Who is going to operate these lines? (PCC) Rail Line? business for a number of years, Watco finally WSDOT is working with local governments to discuss considered abandoning the lines because they As part of the purchase agreement, Watco will formation of an intergovernmental entity to govern were not profitable. In making that determination, the three branches. When such an entity is formed, it The former Palouse River and Coulee City (PCC) continue to operate the PV Hooper Branch under a Watco cited the expensive maintenance conditions will assume responsibility for the former PCC system. rail line is a 300-mile short-line freight rail system lease signed with the state in November 2004 and mentioned above, increased competition from the WSDOT will continue to oversee rehabilitation work that provides direct rail service to shippers, modified in 2007.
    [Show full text]
  • Kitsap County Watershed Location Map Washington State Seems to Have an Abundance of Water
    KITSAP COUNTY INITIAL BASIN ASSESSMENT October 1997 With the multitudes of lakes, streams, and rivers, Kitsap County Watershed Location Map Washington State seems to have an abundance of water. The demand for water resources, however, has steadily increased each year, while the water supply has stayed the same, or in some cases, appears to have declined. This increased demand for limited water resources has made approving new water uses complex and controversial. To expedite decisions about pending water rights, it is vital to accurately assess the quality and quantity of our surface and ground water. The Washington State Department of Ecology (Ecology) recognizes that water right decisions must be based on accurate scientific information. Ecology is working with consultants and local governments to conduct special studies called Initial What do we know about the Kitsap County Watershed or Basin Assessments throughout the Basin? State. The assessments describe existing water rights, streamflows, precipitation, geology, hydrology, Kitsap County encompasses almost 400 square miles and water quality, fisheries resources, and land use occupies a peninsula and several islands in Puget Sound. patterns. It is bounded on the east and north by Puget Sound and The assessments evaluate existing data on water which Admiralty Inlet, and on the west by Hood Canal. The will assist Ecology to make decisions about pending County is adjoined by Pierce and Mason Counties on the water right applications. The assessments do not affect south, Jefferson County
    [Show full text]
  • Grizzly Face-Off the Yellowstone Grizzly Population Is Poised to Lose Federal Protections — for Better Or Worse by Gloria Dickie May 16, 2016 | $5 | Vol
    PURLOINED PATHS | LAYOFFS AND LESSONS | BOOKS FOR THE EREMOCENE High Country ForN people whoews care about the West Grizzly Face-Off The Yellowstone grizzly population is poised to lose federal protections — for better or worse By Gloria Dickie May 16, 2016 | $5 | Vol. 48 No. 8 | www.hcn.org 48 No. | $5 Vol. 2016 16, May CONTENTS Editor’s note Grizzly fascination The professor’s assignment was open-ended: Get together with another graduate student and write about a current natural resource dilemma, one with lots of competing players. Both topic and partner came readily to mind: The Yellowstone grizzly bear intrigued not only me, but also my vivacious, intelligent colleague, Ann Harvey. That was back in 1985. The other day, I found our report buried deep inside an old file cabinet. It’s not poetry, but it captures the flavor of the landscape, as well as the politics of a place that has been one of my journalistic foci for decades now. And I am still friends with Ann, who has lived in the greater Yellowstone ecosystem ever since, and who continues to be an ardent wildlife advocate. Here’s the thing about grizzly bears: They create a human ecosystem every bit as interesting as the natural one. And that system is also populated by fierce and persistent individuals. Ann is one of many who have remained in the grizzly-shaped system for Yellowstone Valley photo guide, outtter and hunter Jim Laybourn wears a bear costume to help send a message at the Yellowstone Ecosystem Subcommittee meeting in Teton Village last November.
    [Show full text]
  • Shoreline Restoration Plan
    Whitman County Coalition Shoreline Restoration Plan available on the City’s website expands on the previous goal in the Environment element with the following vision statement: “Maintain a system of habitat, recreation lands, and facilities in Palouse that defines and enhances the built and natural environment. Support and nurture plant and wildlife habitat, offer a well-balanced range of recreation opportunities which enriches the lives of Palouse's citizens.” Policies and strategies designed to achieve this vision are included in the plan which would significantly improve ecological function in the City. EXISTING AND ONGOING PLANS AND PROGRAMS State, regional, and local agencies and organizations are actively involved in shoreline restoration, conservation, and protection in and around Whitman County. These partners and their local roles in shoreline protection and/or restoration are identified below. 4.1 Whitman County Comprehensive Plan The County’s Comprehensive Plan contains an Environmental Quality and Conservation Element providing policies related to conservation of natural resources. The County has developed guidelines for implementing Comprehensive Plan goals (See Section 3) related to natural resource protection. These focus on policies, regulations, and procedures governing critical and sensitive areas and include: Designating and mapping critical environmental sites and ceasing exemption of dwellings within designated areas from Environmental Impact Statement requirements when a Threshold Determination of Significance is reached. Incorporating goals and guidelines into Whitman County ordinance governing SEPA review. Use the removal of the exemption (above) as an opportunity to evaluate impacts of single-family homes, employ mitigation measures, preserve vegetative cover, and modify locations of buildings and roads. The Plan presents implementation guidelines that incorporate procedural and regulatory frameworks.
    [Show full text]
  • Idaho Room Books by Date
    Boise Public Library - Idaho Room Books 2020 Trails of the Frank Church-River of No Return Wilderness Fuller, Margaret, 1935- 2020 Skiing Sun Valley : a history from Union Pacific to the Holdings Lundin John W. 2020 Sky Ranch : living on a remote ranch in Idaho Phelps, Bobbi, author. 2020 Tales and tails : a story runs through it : anthologies and previously Kleffner, Flip, author. 2020 little known fishing facts Symbols signs and songs Just, Rick, author. 2020 Sun Valley, Ketchum, and the Wood River Valley Lundin, John W. 2020 Anything Will Be Easy after This : A Western Identity Crisis Maile, Bethany, author. 2020 The Boise bucket list : 101 ways to explore the City of Trees DeJesus, Diana C, author. 2020 An eye for injustice : Robert C. Sims and Minidoka 2020 Betty the Washwoman : 2021 calendar. 2020 Best easy day hikes, Boise Bartley, Natalie L. 2020 The Castlewood Laboratory at Libuyu School : a team joins together O'Hara, Rich, author. 2020 Apple : writers in the attic Writers in the Attic (Contest) (2020), 2020 author. The flows : hidden wonders of Craters of the Moon National Boe, Roger, photographer. 2020 Monument and Preserve Educating : a memoir Westover, LaRee, author. 2020 Ghosts of Coeur d'Alene and the Silver Valley Cuyle, Deborah. 2020 Eat what we sow cook book 2020 5 kids on wild trails : a memoir Fuller, Margaret, 1935- 2020 Good time girls of the Rocky Mountains : a red-light history of Collins, Jan MacKell, 1962- 2020 Montana, Idaho, and Wyoming 100 Treasure Valley pollinator plants. 2020 A hundred little pieces on the end of the world Rember, John, author.
    [Show full text]
  • Miocene Evolution of the Moscow-Pullman Basin, Idaho and Washington
    Miocene Evolution of the Moscow-Pullman Basin, Idaho and Washington John H. Bush Pamela Dunlap Stephen P. Reidel Idaho Geological Survey University of Idaho Technical Report 18-3 Moscow, Idaho 83844-3014 December 2018 This Technical Report is a product of independent work from non-Idaho Geological Survey personnel. This report is published by the IGS to further future scientific studies. The IGS does not guarantee this report to be free of errors nor assume liability for interpretations made from this report, or decisions based thereon. TABLE OF CONTENTS Abstract 1 Introduction 1 Stratigraphic Framework and Previous Work 4 History of Regional Stratigraphic Framework 11 Previous Work in the Moscow-Pullman Area 11 Well Chips and Columbia River Basalt Group Stratigraphy 11 Latah Formation 12 Structual Setting 14 Paleogeography 15 Introduction and Pre-basalt Topography 15 Grande Ronde Basalt R1 Interval 17 Grande Ronde Basalt N1 Interval 17 Grande Ronde Basalt R2 Interval 20 Grande Ronde Basalt N2 Interval 23 Vantage and Wanapum Intervals 25 Saddle Mountains Time 29 Summary and Conclusions 31 Acknowledgments 31 References Cited 32 Appendix A. Geochemical Identification of Flow Units in the Columbia River Basalt Group 37 Introduction 37 Oldest Flows of the Columbia River Basalt Group 37 Grande Ronde Basalt Members and Flows 37 Wanapum Basalt 38 References Cited 41 Appendix B Regional Rock Samples 42 Figures Figure 1. Map showing the areal extent of the Columbia River flood basalt province. 2 Figure 2 Map showing Moscow-Pullman Basin, wells,
    [Show full text]
  • VKP Visitorguide-24X27-Side1.Pdf
    FREE FREE MAP Kitsap Peninsula MAP DESTINATIONS & ATTRACTIONS Visitors Guide INSIDE INSIDE Enjoy a variety of activities and attractions like a tour of the Suquamish Museum, located near the Chief Seattle grave site, that tell the story of local Native Americans Welcome and their contribution to the region’s history and culture. to the Kitsap Peninsula! The beautiful Kitsap Peninsula is located directly across Gardens, Galleries & Museums Naval & Military History Getting Around the Region from Seattle offering visitors easy access to the www.VisitKitsap.com/gardens & Memorials www.VisitKitsap.com/transportation Natural Side of Puget Sound. Hop aboard a famous www.VisitKitsap.com/arts-and-culture visitkitsap.com/military-historic-sites- www.VisitKitsap.com/plan-your-event www.VisitKitsap.com/international-visitors WA State Ferry or travel across the impressive Tacaoma Visitors will find many places and events that veterans-memorials The Kitsap Peninsula is conveniently located Narrows Bridge and in minutes you will be enjoying miles offer insights about the region’s rich and diverse There are many historic sites, memorials and directly across from Seattle and Tacoma and a short of shoreline, wide-open spaces and fresh air. Explore history, culture, arts and love of the natural museums that pay respect to Kitsap’s remarkable distance from the Seattle-Tacoma International waterfront communities lined with shops, art galleries, environment. You’ll find a few locations listed in Naval, military and maritime history. Some sites the City & Community section in this guide and many more choices date back to the Spanish-American War. Others honor fallen soldiers Airport. One of the most scenic ways to travel to the Kitsap Peninsula eateries and attractions.
    [Show full text]
  • TREATY MAPPING - Suquamish, Nisqually Traditional Lands
    TREATY MAPPING - Suquamish, Nisqually Traditional Lands On the accompanying map, draw in the boundaries of the traditional lands of the Suquamish. A blank WA map is provided as a worksheet and reference. STEP 1 – Read through Article 1 Point Elliott Treaty and get a basic understanding of the boundaries. STEP 2 – On the backside of the page, read the boundary descriptions that have contemporary names to replace the historical ones that are no longer used. This will help you locate particular boundary landmarks. Use Google Maps to locate contemporary landmarks. Also, check your e-mail for a nap of WA rivers. STEP 3 – Trace the tribal boundaries on a WA map. What needs to be turned in: A Suquamish tribal lands boundary map. You will draw boundaries on the map outline sheet. In addition to boundaries, you need to include the key landmarks on the map that are included in the description to direct the viewer. These boundaries are explained in Article 1 of the treaties and are provided below: Point Elliott Treaty -- Suquamish, 1855 ARTICLE 1. The said tribes and bands of Indians hereby cede, relinquish, and convey to the United States all their right, title, and interest in and to the lands and country occupied by them, bounded and described as follows: Commencing at a Pully Point on the eastern side of Admiralty Inlet [Puget Sound], about midway between Commencement and Elliott Bays; thence eastwardly, running along the north line of lands heretofore ceded to the United States by the Nisqually, Puyallup, and other Indians, to the summit of
    [Show full text]
  • Introduction .Of Washington Geographic Names, a Study
    NOTES ON EARLY SETTLEMENTS AND ON GEOGRAPHIC NAMES OF EASTERN WASHINGTON Introduction The article which follows is a by-product of several mmor studies in the economic history of eastern Washington. Although not intended as such, it turns out to be, in some respects, an appen­ dix, or perhaps a series of footnotes, to Professor Meany's Origin . of Washington Geographic Names, a study published serially in this magazine and subsequently brought out as a volume by the Uni­ versity of Washington Press in 1923. The article contains some names not included in Professor Meany's study, elaborations of a few of his entries, and, in rare instances, slight corrections of his work. To facilitate comparison, frequent references are made to the above-mentioned volume. But the present article is conceived in a different spirit from that of Professor Meany's study. His interest centered in the origins of names; mine has consisted primarily in assembling data relating to early settlements in one area of Washington. Other entries in my article are incidental. By means of the data herein assembled the story of the occupation of the area north of the Snake River in eastern Washington during the seventies and the eighties can be traced in outline, and the principal factors which determined the sites of pioneer towns can be seen in operation. Not the least important of these factors was transportation. During the decade of the seventies the pioneers of eastern Washington were in large measure economically dependent on the Columbia River system. Down the Snake and Columbia rivers was shipped the produce of the "upper country," and up these rivers were transported immi­ grants and equipment needed for the economic development of the Palouse and Spokane countries.* And to some extent settlers south of the Snake River were dependent on the navigation of that stream.
    [Show full text]
  • 90 Pacific Northwest Quarterly Cuthbert, Herbert
    Cuthbert, Herbert (Portland Chamber of in Washington,” 61(2):65-71; rev. of Dale, J. B., 18(1):62-65 Commerce), 64(1):25-26 Norwegian-American Studies, Vol. 26, Daley, Elisha B., 28(2):150 Cuthbert, Herbert (Victoria, B.C., alderman), 67(1):41-42 Daley, Heber C., 28(2):150 103(2):71 Dahlin, Ebba, French and German Public Daley, James, 28(2):150 Cuthbertson, Stuart, comp., A Preliminary Opinion on Declared War Aims, 1914- Daley, Shawn, rev. of Atkinson: Pioneer Bibliography of the American Fur Trade, 1918, 24(4):304-305; rev. of Canada’s Oregon Educator, 103(4):200-201 review, 31(4):463-64 Great Highway, 16(3):228-29; rev. Daley, Thomas J., 28(2):150 Cuthill, Mary-Catherine, ed., Overland of The Emigrants’ Guide to Oregon Dalkena, Wash., 9(2):107 Passages: A Guide to Overland and California, 24(3):232-33; rev. of Dall, William Healey, 77(3):82-83, 90, Documents in the Oregon Historical Granville Stuart: Forty Years on the 86(2):73, 79-80 Society, review, 85(2):77 Frontier, Vols. 1 and 2, 17(3):230; rev. works of: Spencer Fullerton Baird: A Cutler, Lyman A., 2(4):293, 23(2):136-37, of The Growth of the United States, Biography, review, 7(2):171 23(3):196, 62(2):62 17(1):68-69; rev. of Hall J. Kelley D’Allair (North West Company employee), Cutler, Thomas R., 57(3):101, 103 on Oregon, 24(3):232-33; rev. of 19(4):250-70 Cutright, Paul Russell, Elliott Coues: History of America, 17(1):68-69; rev.
    [Show full text]