Oswego Lake Watershed Council
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Historical Overview
HISTORIC CONTEXT STATEMENT The following is a brief history of Oregon City. The intent is to provide a general overview, rather than a comprehensive history. Setting Oregon City, the county seat of Clackamas County, is located southeast of Portland on the east side of the Willamette River, just below the falls. Its unique topography includes three terraces, which rise above the river, creating an elevation range from about 50 feet above sea level at the riverbank to more than 250 feet above sea level on the upper terrace. The lowest terrace, on which the earliest development occurred, is only two blocks or three streets wide, but stretches northward from the falls for several blocks. Originally, industry was located primarily at the south end of Main Street nearest the falls, which provided power. Commercial, governmental and social/fraternal entities developed along Main Street north of the industrial area. Religious and educational structures also appeared along Main Street, but tended to be grouped north of the commercial core. Residential structures filled in along Main Street, as well as along the side and cross streets. As the city grew, the commercial, governmental and social/fraternal structures expanded northward first, and with time eastward and westward to the side and cross streets. Before the turn of the century, residential neighborhoods and schools were developing on the bluff. Some commercial development also occurred on this middle terrace, but the business center of the city continued to be situated on the lower terrace. Between the 1930s and 1950s, many of the downtown churches relocated to the bluff as well. -
Timing of In-Water Work to Protect Fish and Wildlife Resources
OREGON GUIDELINES FOR TIMING OF IN-WATER WORK TO PROTECT FISH AND WILDLIFE RESOURCES June, 2008 Purpose of Guidelines - The Oregon Department of Fish and Wildlife, (ODFW), “The guidelines are to assist under its authority to manage Oregon’s fish and wildlife resources has updated the following guidelines for timing of in-water work. The guidelines are to assist the the public in minimizing public in minimizing potential impacts to important fish, wildlife and habitat potential impacts...”. resources. Developing the Guidelines - The guidelines are based on ODFW district fish “The guidelines are based biologists’ recommendations. Primary considerations were given to important fish species including anadromous and other game fish and threatened, endangered, or on ODFW district fish sensitive species (coded list of species included in the guidelines). Time periods were biologists’ established to avoid the vulnerable life stages of these fish including migration, recommendations”. spawning and rearing. The preferred work period applies to the listed streams, unlisted upstream tributaries, and associated reservoirs and lakes. Using the Guidelines - These guidelines provide the public a way of planning in-water “These guidelines provide work during periods of time that would have the least impact on important fish, wildlife, and habitat resources. ODFW will use the guidelines as a basis for the public a way of planning commenting on planning and regulatory processes. There are some circumstances where in-water work during it may be appropriate to perform in-water work outside of the preferred work period periods of time that would indicated in the guidelines. ODFW, on a project by project basis, may consider variations in climate, location, and category of work that would allow more specific have the least impact on in-water work timing recommendations. -
Clackamas County
EXHIBIT A - Invisible Walls: Housing Discrimination in Clackamas County 94 Table of Contents A Note About This Project ………………………………………………………………………………………………………. 1 Class Bios ………………………………………………………………………………………………………………………………… 2 Project Introduction and Methods Statement …………………………………………………………………………. 3 Timeline ………………………………………………………………………………………………………………………………….. 8 Historic Property Deed Research …………………………………………………………………………………………… 13 Metropolitan Setting of the Suburban Zone ………………………………………………………………………….. 21 Community Highlights: - Lake Oswego ……………………………………………………………………………………………………………… 24 - Milwaukie ………………………………………………………………………………………………………………….. 28 - Oregon City ………………………………………………………………………………………………………………… 34 Land and Conflict: The Genesis of Housing Discrimination in Clackamas County ……………………. 38 Migrant Labor in Oregon: 1958 Snapshot ………………………………………………………………………………. 41 Migrant Labor in Oregon: Valley Migrant League …………………………………………………………………… 43 Chinese in Clackamas County ………………………………………………………………………………………………… 48 Japanese in Clackamas County ………………………………………………………………………………………………. 51 Direct Violence: …………………………………………………………………………………………………………………….. 54 - Richardson Family ……………………………………………………………………………………………………… 55 - Perry Ellis …………………………………………………………………………………………………………………… 56 Resistance in Lane County …………………………………………………………………………………………………….. 57 John Livingston ……………………………………………………………………………………………………………………… 58 Political Structure: - Zoning in Clackamas County ………………………………………………………………………………………. 59 - Urban Growth Boundary ……………………………………………………………………………………………. -
A Wild in the City Ramble Lowe R Willamette River Loop Sellwood Riverfront Park to Oregon City Fa Lls
Bike A Wild in the City Ramble Lower Willamette River Loop Sellwood Riverfront Park to Oregon City Falls Before setting out on this twenty-five-mile loop ride, Sellwood Riverfront Park 1 is worth a brief look. When I visited the site with Portland Park staff in the early 1980s, it was a heap of Himalayan-blackberry-covered sawdust, having once been an old mill site. It’s a tribute to the landscape architects who transformed a truly ugly landscape into a fine neighborhood park and a great place to access the Willamette. The funky little wetland feature in the park’s northeast corner, abutting the black cottonwood forest, has a short boardwalk from which you can see native wetland plants like spirea, blue elderberry, creek dogwood, willow, and wapato, and kids can catch polliwogs. Green heron sometimes skulk about looking for frogs, one of which is the rare north- ern red-legged frog (Rana aurora). From the park, I jump on the Springwater on the Willamette trail and head out to Milwaukie and the Jefferson Street Boat Ramp 2 , where there are great views of the Johnson Creek confluence with the Willamette River 3 and a distant view of Elk Rock Island. The route south is along the paved bicycle-pedestrian path that winds riverward of the Kellogg Creek Wastewater Treatment Plant. The short path abruptly dumps you onto SE 19th Avenue and SE Eagle Street. Ride straight south to SE Sparrow Street. All the streets in this quiet neighborhood are named after birds. At the end of Sparrow Street is the entrance to Milwaukie’s Spring Park 4 and access to Elk Rock Island. -
Note: for Properties 35 Years Old and Newer, Starred (*) Sections Are the Only Required Fields
OREGON INVENTORY OF HISTORIC PROPERTIES HISTORIC RESOURCE SURVEY FORM Note: For properties 35 years old and newer, starred (*) sections are the only required fields. *County: Clackamas *Street Address: *City Situs Address 16500 S. Old River Road Lake Oswego USGS Quad Name: GPS Reading, UTM Format (Universal Transverse Mercator): Lake Oswego Longitude: 122°39'21.18"W Latitude: 45°24'28.20"N Township: Range: Section: Block/Lot: Tax Lot #: 2S 1E 11CB N/A 790 Historic Name: Grouping or Cluster Name: The Crown Willamette Log Loading Station *Date of Construction: Other Name: ca. 1915 Log Hoist Historic Use or Function: *Current Use: Associated Archaeological Site: Industrial Abandoned Unknown Architectural Classification(s): Plan Type/Shape: Number of stories: Structure Rectangular N/A Foundation Material: Structural Framing: Moved? Concrete Concrete No Roof Type/Material: Window Type/Material: N/A N/A Exterior Surface Materials Primary: Secondary: Decorative: Concrete N/A Exterior Alterations or Additions, Approximate Date: One Story addition w/band of windows across façade added to top of structure when converted to residential use (date unknown, but possibly around 1978) Number and Type of Associated Resources: None Integrity: Condition: Local Eligibility National Register Listed? Good Fair On LDL Yes No Unknown Preliminary National Register Findings:air Potentially Eligible: Individually or As a contributing resource in a District Not Eligible: Intact but lacks distinction or Not 50 years old or Altered - Choose one: Reversible/ potentially -
CITY of LAKE OSWEGO CLACKAMAS, MULTNOMAH and WASHINGTON COUNTIES, OREGON $75,290,000 Full Faith and Credit Obligations, Series 2013
OFFICIAL STATEMENT DATED AUGUST 27, 2013 NEW ISSUE -- COMPETITIVE RATINGS: Moody’s: Aa1 Book-Entry-Only S&P: AAA See “RATINGS” herein. In the opinion of Orrick, Herrington & Sutcliffe LLP, Special Counsel to the City (“Special Counsel”), based upon an analysis of existing laws, regulations, rulings and court decisions, and assuming, among other matters, the accuracy of certain representations and compliance with certain covenants, that portion of the payments received by holders of the Obligations with respect to the obligations of the City under the Financing Agreement (the “Financing Obligations”) designated as and constituting interest on the Financing Obligations is excluded from gross income for federal income tax purposes under Section 103 of the Internal Revenue Code of 1986 (the “Code”). In the further opinion of Special Counsel, interest on the Financing Obligations is not a specific preference item for purposes of the federal individual or corporate alternative minimum taxes, although Bond Counsel observes that such interest is included in adjusted current earnings when calculating corporate alternative minimum taxable income. In the further opinion of Special Counsel, based upon an analysis of existing laws, regulations, rulings and court decisions, that portion of the payments received by holders of the Financing Obligations that are designated as and constituting interest is exempt from personal income taxation imposed by the State of Oregon. Special Counsel expresses no opinion regarding any other tax consequences related -
Appendix E: the City's Natural Environment
APPENDIX E The City’s Natural Environment APPENDIX E The City’s Natural Environment The City’s Environmental Setting General Characteristics Portland is situated at 20 feet above sea level, near the confluence of the Columbia and Willamette rivers, about 65 miles inland from the Pacific Ocean. It lies midway between the lower Coast Range to the west and the high Cascades Range to the east, each about 30 miles distant. Portland’s varied topography includes steep hills, isolated volcanic cones, low rolling hills and extensive flat areas. The area is composed primarily of alluvial deposits and Columbia River basalts. Much of the city is located in the Willamette Valley Plains ecoregion, although steeper portions of the Tualatin Hills on the west side are characteristic of Willamette Valley Hills and Coastal Mountains ecoregions (Clarke and others 1991). Portland has a mild marine climate that is heavily influenced by the mountain ranges east and west of the city. The Coast Range protects the Portland area from Pacific storms, while the Cascades prevent colder continental air masses from invading western Oregon. In winter, the average temperature is 40°F and the average minimum temperature is 34°F. In summer the average temperature is 65°F with an average daily maximum of 74 to 78°F (Rockey 2002). The Cascades also lift moisture-laden westerly winds from the Pacific, driving local rainfall patterns. Average annual rainfall in the Portland area is approximately 37 inches. Nearly 90 percent of the annual rainfall occurs from October through May. Only 9 percent of the annual rainfall occurs between June and September, with 3 percent in July and August. -
Willamette Basin Total Maximum Daily Loads (Tmdls)
Willamette Basin TMDL: Clackamas Subbasin September 2006 CHAPTER 6: CLACKAMAS SUBBASIN TMDL Table of Contents WATER QUALITY SUMMARY......................................................................................... 3 Reason for action ........................................................................................................................................................... 3 Who helped us................................................................................................................................................................ 3 Subbasin 303(d) Listed Parameters Addressed by a TMDL ..................................................................................... 4 SUBBASIN OVERVIEW ................................................................................................... 5 Land Use and Ownership.............................................................................................................................................. 6 Watershed Descriptions ................................................................................................................................................ 7 Upper Clackamas Watershed....................................................................................................................................... 7 Collawash River and Hot Springs Fork Drainages ...................................................................................................... 8 Oak Grove Fork.......................................................................................................................................................... -
An Abstract of the Dissertation Of
AN ABSTRACT OF THE DISSERTATION OF Peter J. Wampler for the degree of Doctor of Philosophy in Geology presented on July 14, 2004. Title: Contrasting Geomorphic Responses to Climatic, Anthropogenic, and Fluvial Change Across Modern to Millennial Time Scales, Clackamas River, Oregon. Abstract approved: Gordon E. Grant Geomorphic change along the lower Clackamas River is occurring at a millennial scale due to climate change; a decadal scale as a result River Mill Dam operation; and at an annual scale since 1996 due to a meander cutoff. Channel response to these three mechanisms is incision. Holocene strath terraces, inset into Pleistocene terraces, are broadly synchronous with other terraces in the Pacific Northwest, suggesting a regional aggradational event at the Pleistocene/Holocene boundary. A maximum incision rate of 4.3 mm/year occurs where the river emerges from the Western Cascade Mountains and decreases to 1.4 mm/year near the river mouth. Tectonic uplift, bedrock erodibility, rapid base-level change downstream, or a systematic decrease in Holocene sediment flux may be contributing to the extremely rapid incision rates observed. The River Island mining site experienced a meander cutoff during flooding in 1996, resulting in channel length reduction of 1,100 meters as the river began flowing through a series of gravel pits. Within two days of the peak flow, 3.5 hectares of land and 105,500 m3 of gravel were eroded from the river bank just above the cutoff location. Reach slope increased from 0.0022 to approximately 0.0035 in the cutoff reach. The knick point from the meander cutoff migrated 2,290 meters upstream between 1996 and 2003, resulting in increased bed load transport, incision of 1 to 2 meters, and rapid water table lowering. -
State Waterway Navigability Determination
BODY OF WATER & LOCATION NAV CG NON-NAV CG REMARKS yellow highlight = apply to USCG for permit up to RM stipulated Alsea Bay, OR X Estuary of Pacific Ocean. Alsea River, OR X Flows into Alsea Bay, Waldport, OR. Navigable to mile 13. Ash Creek, OR X Tributary of Willamette River at Independence, OR. Barrett Slough, OR X Tributary of Lewis and Clark River. Bayou St. John, OR X Court decision, 1935 AMC 594, 10 Mile Lake, Coos County, OR. Bear Creek (Coos County), OR X Tributary of Coquille River (tidal at mile 0.5) Beaver Creek, OR X Tributary of Nestucca River. Beaver Slough, OR X See Clatskanie River. Big Creek (Lane County), OR X At U.S. 101 bridge (tidal). Big Creek (Lincoln County), OR X Flows into Pacific Ocean. Big Creek Slough, OR X Upstream end at Knappa, OR (tidal). At site of Birch Creek (Sparks) Bridge on Canyon Road near Birch Creek, OR X Pendleton, OR. Side channel of Yaquina River. 3 mi. downstream from Toledo, Blind Slough, OR X OR (tidal). Tributary of Knappa Slough. 10 mi. upstream from Astoria, OR Blind Slough/ Gnat Creek, OR X (tidal at mile 2.0). Boone Slough, OR X Tributary of Yaquina River between Newport and Toledo, OR. Side channel of Willamette River. 3 miles upstream from Booneville Channel, OR X Corvallis, OR. Boulder Creek, OR X 7 miles N of Lake Quinalt. Side channel of Columbia River. 5 miles N of Clatskanie, OR Bradbury Slough, OR X (tidal). Brownlee Reservoir, ID /OR X See Snake River. Also known as South Channel. -
A Storypath Exploring the Lasting Legacy of Celilo Falls by Shana Brown
Living in Celilo A Storypath Exploring the Lasting Legacy of Celilo Falls by Shana Brown Office of Native Education Office of the Superintendent of Public Instruction Washington State Trillium Publishing, Inc. Acknowledgements Contents Shana Brown would like to thank: Carol Craig, Yakama Elder, writer, and historian, for her photos of Celilo as well as her Introduction to Storypath ..................... 2 expertise and her children’s story “I Wish I Had Seen the Falls.” Chucky is really her first grandson (and my cousin!). Episode 1: Creating the Setting ...............22 The Columbia River Inter-Tribal Fish Commission for providing information about their organization and granting permission to use articles, including a piece from their Episode 2: Creating the Characters............42 magazine Wana Chinook Tymoo. Episode 3: Building Context ..................54 HistoryLink.org for granting permission to use the article “Dorothea Nordstrand Recalls Old Celilo Falls.” Episode 4: Authorizing the Dam ..............68 The Northwest Power and Conservation Council for granting permission to use an excerpt from the article “Celilo Falls.” Episode 5: Negotiations .....................86 Ritchie Graves, Chief of the NW Region Hydropower Division’s FCRPS Branch, NOAA Fisheries, for providing information on survival rates of salmon through the Episode 6: Broken Promises ................118 dams on the Columbia River system. Episode 7: Inundation .....................142 Sally Thompson, PhD., for granting permission to use her articles. Se-Ah-Dom Edmo, Shoshone-Bannock/Nez Perce/ Yakama, Coordinator of the Classroom-Based Assessment ...............154 Indigenous Ways of Knowing Program at Lewis & Clark College, Columbia River Board Member, and Vice President of the Oregon Indian Education Association, for providing invaluable feedback and guidance as well as copies of the actual notes and letters from the Celilo Falls Community Club. -
The Burnett Site : a Cascade Phase Camp on the Lower Willamette River
Portland State University PDXScholar Dissertations and Theses Dissertations and Theses 1991 The Burnett Site : a Cascade Phase camp on the lower Willamette River Robert M. Burnett Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Part of the Archaeological Anthropology Commons Let us know how access to this document benefits ou.y Recommended Citation Burnett, Robert M., "The Burnett Site : a Cascade Phase camp on the lower Willamette River" (1991). Dissertations and Theses. Paper 4171. https://doi.org/10.15760/etd.6055 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 Robert M. Burnett for the Master of Arts in Anthropology presented May 3, 1991. Title: The Burnett Site: A Cascade Phase Camp on the Lower Willamette River. APPROVED BY THE MEMBERS OF THE THESIS COMMITTEE: Kenneth M. Ames, Chair Jofut Fagan ;f Artifacts recovered from archaeological excavations near the Willamette River in Lake Oswego, Oregon indicate the presence there of a Late Windust- Early Cascade Phase site possibly dating to 9,000 B.P. The assemblage includes 137 projectile points, bifaces or point fragments, nearly all of the Cascade-type. Two stem fragments and one complete point which are similar to those of the 2 Windust Phase which dates 10,000-8,000 B.P. in the southern Columbia Plateau also were found. Stone knives, choppers, scrapers, hammerstones, cores and microblades also are included in the assemblage.