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• 1. [Article] Residential Solar Photovoltaics: A Financial Decision Support Tool for Northwestern Oregon

  This paper describes the benefits of the utilization of solar photovoltaics (PV) in northwestern Oregon and describes a newly developed interactive financial decision support model created for residential ...

  Citation × Citation Citation Abstract Copy Title: Residential Solar Photovoltaics: A Financial Decision Support Tool for Northwestern Oregon Author: Brand, Marius, Easton, John, Sairafi, Badr, Sughi, Hithem, Jan, Fahad Year: 2008 This paper describes the benefits of the utilization of solar photovoltaics (PV) in northwestern Oregon and describes a newly developed interactive financial decision support model created for residential PV installation in northwestern Oregon. Advantages of this model over existing standards include fewer assumptions made regarding locality-specific circumstances, including utility rate increase forecasts, local incentive and tax credit information, region specific electricity generation efficiencies, and the provision of unique inputs and outputs such as user-defined financing options and variable sensitivity analysis. Title: Residential Solar Photovoltaics: A Financial Decision Support Tool for Northwestern Oregon Author: Brand, Marius, Easton, John, Sairafi, Badr, Sughi, Hithem, Jan, Fahad Year: 2008 This paper describes the benefits of the utilization of solar photovoltaics (PV) in northwestern Oregon and describes a newly developed interactive financial decision support model created for residential PV installation in northwestern Oregon. Advantages of this model over existing standards include fewer assumptions made regarding locality-specific circumstances, including utility rate increase forecasts, local incentive and tax credit information, region specific electricity generation efficiencies, and the provision of unique inputs and outputs such as user-defined financing options and variable sensitivity analysis. Close

• 2. [Article] Indicators of the Metroscape: Self-Sufficiency

  Overview of annual median income and self-sufficiency standards for various household types in 2014, for several Oregon counties in Northwestern Oregon.

  Citation × Citation Citation Abstract Copy Title: Indicators of the Metroscape: Self-Sufficiency Author: Institute of Portland Metropolitan Studies Year: 2015 Overview of annual median income and self-sufficiency standards for various household types in 2014, for several Oregon counties in Northwestern Oregon. Title: Indicators of the Metroscape: Self-Sufficiency Author: Institute of Portland Metropolitan Studies Year: 2015 Overview of annual median income and self-sufficiency standards for various household types in 2014, for several Oregon counties in Northwestern Oregon. Close

• 3. [Article] Stratigraphic relationships of the Tillamook Volcanics and the Cowlitz Formation in the upper Nehalem River-Wolf Creek area, northwestern Oregon

  The upper Nehalem River-Wolf Creek area is located on the northeastern flank of the Tillamook Highlands in the northern Oregon Coast Range. Three rock stratigraphic units underlie the thesis area, and ...

  Citation × Citation Citation Abstract Copy Title: Stratigraphic relationships of the Tillamook Volcanics and the Cowlitz Formation in the upper Nehalem River-Wolf Creek area, northwestern Oregon Author: Jackson, Michael Keith Year: 1983 The upper Nehalem River-Wolf Creek area is located on the northeastern flank of the Tillamook Highlands in the northern Oregon Coast Range. Three rock stratigraphic units underlie the thesis area, and these units range from late Eocene to Oligocene in age. Title: Stratigraphic relationships of the Tillamook Volcanics and the Cowlitz Formation in the upper Nehalem River-Wolf Creek area, northwestern Oregon Author: Jackson, Michael Keith Year: 1983 The upper Nehalem River-Wolf Creek area is located on the northeastern flank of the Tillamook Highlands in the northern Oregon Coast Range. Three rock stratigraphic units underlie the thesis area, and these units range from late Eocene to Oligocene in age. Close

• 4. [Article] A stratigraphic and geochemical investigation of ferruginous bauxite deposits in the Salem Hills, Marion County, Oregon

  Pacific Northwest ferruginous bauxite deposits have formed in four main areas of northwestern Oregon and southwestern Washington by laterization of flows of the Columbia River Basalt Group (CRBG). The ...

  Citation × Citation Citation Abstract Copy Title: A stratigraphic and geochemical investigation of ferruginous bauxite deposits in the Salem Hills, Marion County, Oregon Author: Hoffman, Charles William Year: 1981 Pacific Northwest ferruginous bauxite deposits have formed in four main areas of northwestern Oregon and southwestern Washington by laterization of flows of the Columbia River Basalt Group (CRBG). The deposits, averaging 36.3% Al2O3 , 31.8% Fe2O3 , and 5.9% Sio2, generally occur near the surface of hilltops in gently rolling areas. Two very different views have been advanced regarding the setting in which the deposits have formed. The first hypothesis calls for a blanket-type laterization by erosion of much of the original deposit upon uplift and dissection of the area. Title: A stratigraphic and geochemical investigation of ferruginous bauxite deposits in the Salem Hills, Marion County, Oregon Author: Hoffman, Charles William Year: 1981 Pacific Northwest ferruginous bauxite deposits have formed in four main areas of northwestern Oregon and southwestern Washington by laterization of flows of the Columbia River Basalt Group (CRBG). The deposits, averaging 36.3% Al2O3 , 31.8% Fe2O3 , and 5.9% Sio2, generally occur near the surface of hilltops in gently rolling areas. Two very different views have been advanced regarding the setting in which the deposits have formed. The first hypothesis calls for a blanket-type laterization by erosion of much of the original deposit upon uplift and dissection of the area. Close

• 5. [Article] Scappoose School District Population and Enrollment Forecasts, 2006-07 to 2020-21

  The Scappoose School District (SSD) in northwestern Oregon serves the City of Scappoose and the southeastern portion of Columbia County, as well as the extreme northwestern portion of Multnomah County ...

  Citation × Citation Citation Abstract Copy Title: Scappoose School District Population and Enrollment Forecasts, 2006-07 to 2020-21 Author: Portland State University. Population Research Center, Rynerson, Charles, Siu, Vivian Year: 2006 The Scappoose School District (SSD) in northwestern Oregon serves the City of Scappoose and the southeastern portion of Columbia County, as well as the extreme northwestern portion of Multnomah County and a small piece of Washington County. The area served by the District has experienced population growth in recent years, but overall school enrollment losses in two of the past five years have negated the gains in the other three years. This report presents the results of a forecast conducted by the Portland State University Population Research Center (PRC) indicating that SSD enrollment will increase during the next fifteen years, with relatively slow growth in the first five years and faster growth during the 2010 to 2020 period. PRC’s methodology links enrollment trends with the area’s population dynamics. Population and housing are closely related to access to jobs. In the context of expected employment, population, and housing growth, enrollment is likely to increase at all grade levels. Title: Scappoose School District Population and Enrollment Forecasts, 2006-07 to 2020-21 Author: Portland State University. Population Research Center, Rynerson, Charles, Siu, Vivian Year: 2006 The Scappoose School District (SSD) in northwestern Oregon serves the City of Scappoose and the southeastern portion of Columbia County, as well as the extreme northwestern portion of Multnomah County and a small piece of Washington County. The area served by the District has experienced population growth in recent years, but overall school enrollment losses in two of the past five years have negated the gains in the other three years. This report presents the results of a forecast conducted by the Portland State University Population Research Center (PRC) indicating that SSD enrollment will increase during the next fifteen years, with relatively slow growth in the first five years and faster growth during the 2010 to 2020 period. PRC’s methodology links enrollment trends with the area’s population dynamics. Population and housing are closely related to access to jobs. In the context of expected employment, population, and housing growth, enrollment is likely to increase at all grade levels. Close

• 6. [Article] The Making of Seaside’s “Indian Place”: Contested and Enduring Native Spaces on the Nineteenth Century Oregon Coast

  During the mid nineteenth century, non-Native settlement and activities disrupted and changed historic Chinook and Clatsop communities at the mouth of the Columbia River. Indian Place in what would be ...

  Citation × Citation Citation Abstract Copy Title: The Making of Seaside’s “Indian Place”: Contested and Enduring Native Spaces on the Nineteenth Century Oregon Coast Author: Deur, Douglas Year: 2016 During the mid nineteenth century, non-Native settlement and activities disrupted and changed historic Chinook and Clatsop communities at the mouth of the Columbia River. Indian Place in what would be Seaside, Oregon, became home to a number of displaced peoples and an enclave where “the living gathered with the remains of the dead,” for “modest protection from the apocalyptic changes that so radically disrupted tribal lands, lives, and worldviews.” Douglas Deur documents tribal migration to the Indian Place during the late nineteenth and early twentieth centuries and calls attention to many of its significant early residents. Transitional communities such as Indian Place, Deur attests, “defined the nineteenth- and early-twentieth-century Native experience in northwestern Oregon and beyond.” While the Indian Place no longer exists, it remains an “important [conduit] for tribal cultural knowledge, values, and practices that endure today.” Title: The Making of Seaside’s “Indian Place”: Contested and Enduring Native Spaces on the Nineteenth Century Oregon Coast Author: Deur, Douglas Year: 2016 During the mid nineteenth century, non-Native settlement and activities disrupted and changed historic Chinook and Clatsop communities at the mouth of the Columbia River. Indian Place in what would be Seaside, Oregon, became home to a number of displaced peoples and an enclave where “the living gathered with the remains of the dead,” for “modest protection from the apocalyptic changes that so radically disrupted tribal lands, lives, and worldviews.” Douglas Deur documents tribal migration to the Indian Place during the late nineteenth and early twentieth centuries and calls attention to many of its significant early residents. Transitional communities such as Indian Place, Deur attests, “defined the nineteenth- and early-twentieth-century Native experience in northwestern Oregon and beyond.” While the Indian Place no longer exists, it remains an “important [conduit] for tribal cultural knowledge, values, and practices that endure today.” Close

• 7. [Article] Geophysical and geochemical analyses of selected Miocene coastal basalt features, Clatsop County, Oregon

  The proximity of Miocene Columbia River basalts to the "locally-erupted" coastal Miocene basalts in northwestern Oregon, and the compelling similarities between the two groups, suggest that the coastal ...

  Citation × Citation Citation Abstract Copy Title: Geophysical and geochemical analyses of selected Miocene coastal basalt features, Clatsop County, Oregon Author: Pfaff, Virginia Josette Year: 1980 The proximity of Miocene Columbia River basalts to the "locally-erupted" coastal Miocene basalts in northwestern Oregon, and the compelling similarities between the two groups, suggest that the coastal basalts, rather than being locally erupted, may be the westward extension of plateau basalts derived from eastern Oregon and Washington. The local-origin hypothesis is based largely on the interpretation of coastal dikes and sills as representing vent areas; however, a complex mechanism, as yet unsatisfactorily defined, would be required to cause the eruption of virtually identical magmas simultaneously from source areas 500 km apart. This study, therefore, has investigated the coastal basalt intrusions both laterally and vertically. Geochemical and paleomagnetic analysis was used to determine the occurrence and distribution of basalt units; gravity surveys enabled an examination of the subsurface extensions of basalt intrusions in sedimentary rocks. Title: Geophysical and geochemical analyses of selected Miocene coastal basalt features, Clatsop County, Oregon Author: Pfaff, Virginia Josette Year: 1980 The proximity of Miocene Columbia River basalts to the "locally-erupted" coastal Miocene basalts in northwestern Oregon, and the compelling similarities between the two groups, suggest that the coastal basalts, rather than being locally erupted, may be the westward extension of plateau basalts derived from eastern Oregon and Washington. The local-origin hypothesis is based largely on the interpretation of coastal dikes and sills as representing vent areas; however, a complex mechanism, as yet unsatisfactorily defined, would be required to cause the eruption of virtually identical magmas simultaneously from source areas 500 km apart. This study, therefore, has investigated the coastal basalt intrusions both laterally and vertically. Geochemical and paleomagnetic analysis was used to determine the occurrence and distribution of basalt units; gravity surveys enabled an examination of the subsurface extensions of basalt intrusions in sedimentary rocks. Close

• 8. [Article] Long Trails Project: Identifying Opportunities, Solving Problems, and Exploring Implementation

  This document presents the final report of the Long Trails Project, a partnership with the Oregon Parks Department and USP 549: Regional Planning and Metropolitan Growth Management, a course offered to ...

  Citation × Citation Citation Abstract Copy Title: Long Trails Project: Identifying Opportunities, Solving Problems, and Exploring Implementation Author: Portland State University Year: 2012 This document presents the final report of the Long Trails Project, a partnership with the Oregon Parks Department and USP 549: Regional Planning and Metropolitan Growth Management, a course offered to graduate planning students in the Toulan School of Urban Studies and Planning at Portland State University. It is divided into 5 sections: (1.) History of Long Trails and Regional Trail Networks (2.) Long Trails in Northwestern Oregon (3.) The Demand for Long Trails-based Recreation (4.) Long Trails and Community Economic Development (5.) Long Trails Implementation. This technical report is edited by Dr. Ethan Seltzer Title: Long Trails Project: Identifying Opportunities, Solving Problems, and Exploring Implementation Author: Portland State University Year: 2012 This document presents the final report of the Long Trails Project, a partnership with the Oregon Parks Department and USP 549: Regional Planning and Metropolitan Growth Management, a course offered to graduate planning students in the Toulan School of Urban Studies and Planning at Portland State University. It is divided into 5 sections: (1.) History of Long Trails and Regional Trail Networks (2.) Long Trails in Northwestern Oregon (3.) The Demand for Long Trails-based Recreation (4.) Long Trails and Community Economic Development (5.) Long Trails Implementation. This technical report is edited by Dr. Ethan Seltzer Close

• 9. [Article] Geochemical Evolution of Ferruginous Bauxite Deposits in Northwestern Oregon and Southwestern Washington

  Ferruginous bauxite deposits developed from flows of the Columbia River Basalt Group in northwestern Oregon and southwestern Washington. Samples of the iron pisolite and the gibbsite nodular zones from ...

  Citation × Citation Citation Abstract Copy Title: Geochemical Evolution of Ferruginous Bauxite Deposits in Northwestern Oregon and Southwestern Washington Author: Fassio, Joseph Michael Year: 1990 Ferruginous bauxite deposits developed from flows of the Columbia River Basalt Group in northwestern Oregon and southwestern Washington. Samples of the iron pisolite and the gibbsite nodular zones from the upper portion of the weathering profile of drill core from Columbia County, Oregon and Cowlitz County, Washington, were analyzed by instrumental neutron activation. The mineralogy was determined using Xray diffraction and Mossbauer spectroscopy. The gibbsite nodular zone is above the clay-rich saprolite or relic basalt zone. The nodules contain relic vesicles and well preserved relic plagioclase microlites. Gibbsite occurs with poorly crystalline goethite and hematite in the gibbsite nodular zone. Clays are absent in this part of the profile . The iron pisolite zone is at the top of the profile above the gibbsite nodular zone. Both maghemite and goethite pisolites occur in the lower part of the zone while maghemite pisolites are dominant in the upper part of the pisolite zone. The parent flow is the Frenchman Springs Member of the Wanapum Basalt for the Columbia County profile and the Pomona Member of the Saddle Mountains Basalt for the Cowlitz County profile. Distribution of the major, minor and trace elements through the profile shows three distinct sympathetic patterns consisting of lanthanide elements and Na; As, Sbi Th, Hf, and Ta; and transition metals Fe, Ti, V, and Cr. Ratios between the high-field strength elements Ta and Hf are nearly constant through the profile, and Hf appears to be the least mobile elements of the elements analyzed in the profile. Ratios of other elements were calculated against Hf, based on the assumption that it has remained largely immobile during weathering, to show element enrichment and depletion in the profile independent of mass-volume changes. Transition metals and Al show a progressive depletion through the upper gibbsite nodular and iron pisolite zone due to leaching in the profile. Lanthanide elements (except Ce), As, and Sb show an obvious enrichment in the iron pisolite zone relative to the gibbsite nodular zone. Volume reduction during weathering was calculated based on the immobility of Hf. In the gibbsite nodular zone, the volume reduction calculated for bulk samples is greater than for gibbsite nodule separates suggesting that a greater volume reduction occurred the matrix material surrounding the nodules. Ratios between gibbsite nodules and parent basalt of the immobile elements Hf, Ta, Fe, Ti, Th and Cr suggest that the nodules, where the relic textures are preserved, have undergone volume reduction. Based on the immobility of Hf, the gibbsite nodules lost approximately 40% of the original volume. The volume factors based on the immobility of Hf show that the pisolite zone experienced a greater volume reduction than the gibbsite nodular zone. Absolute gains and losses relative to the parent basalt show the following relative order of depletion: Na > La > Eu > Sm > Co > Mn > Ce > Sc > Ta > V > Cr > Lu > Th > Fe > Ga > Al. The lesser mobility of Ce and Lu relative to other lanthanide elements suggests fractionation of lanthanide elements in the bauxite profile. Aluminum is both enriched and depleted at different depths in the gibbsite nodular zone suggesting that Al is mobilized from the matrix and possibly the pisolite zone into Al enriched gibbsite nodules. Volume reduction and destruction of relic textures in the pisolite zone is accompanied by small-scale mobilization of Th, Cr, Fe, Hf, Ga, Sc, and Ta during the formation of iron pisolites. Formation of the iron pisolite zone above the gibbsite nodular zone may indicate a change in climate from a heavy year round to a seasonal rainfall pattern. Title: Geochemical Evolution of Ferruginous Bauxite Deposits in Northwestern Oregon and Southwestern Washington Author: Fassio, Joseph Michael Year: 1990 Ferruginous bauxite deposits developed from flows of the Columbia River Basalt Group in northwestern Oregon and southwestern Washington. Samples of the iron pisolite and the gibbsite nodular zones from the upper portion of the weathering profile of drill core from Columbia County, Oregon and Cowlitz County, Washington, were analyzed by instrumental neutron activation. The mineralogy was determined using Xray diffraction and Mossbauer spectroscopy. The gibbsite nodular zone is above the clay-rich saprolite or relic basalt zone. The nodules contain relic vesicles and well preserved relic plagioclase microlites. Gibbsite occurs with poorly crystalline goethite and hematite in the gibbsite nodular zone. Clays are absent in this part of the profile . The iron pisolite zone is at the top of the profile above the gibbsite nodular zone. Both maghemite and goethite pisolites occur in the lower part of the zone while maghemite pisolites are dominant in the upper part of the pisolite zone. The parent flow is the Frenchman Springs Member of the Wanapum Basalt for the Columbia County profile and the Pomona Member of the Saddle Mountains Basalt for the Cowlitz County profile. Distribution of the major, minor and trace elements through the profile shows three distinct sympathetic patterns consisting of lanthanide elements and Na; As, Sbi Th, Hf, and Ta; and transition metals Fe, Ti, V, and Cr. Ratios between the high-field strength elements Ta and Hf are nearly constant through the profile, and Hf appears to be the least mobile elements of the elements analyzed in the profile. Ratios of other elements were calculated against Hf, based on the assumption that it has remained largely immobile during weathering, to show element enrichment and depletion in the profile independent of mass-volume changes. Transition metals and Al show a progressive depletion through the upper gibbsite nodular and iron pisolite zone due to leaching in the profile. Lanthanide elements (except Ce), As, and Sb show an obvious enrichment in the iron pisolite zone relative to the gibbsite nodular zone. Volume reduction during weathering was calculated based on the immobility of Hf. In the gibbsite nodular zone, the volume reduction calculated for bulk samples is greater than for gibbsite nodule separates suggesting that a greater volume reduction occurred the matrix material surrounding the nodules. Ratios between gibbsite nodules and parent basalt of the immobile elements Hf, Ta, Fe, Ti, Th and Cr suggest that the nodules, where the relic textures are preserved, have undergone volume reduction. Based on the immobility of Hf, the gibbsite nodules lost approximately 40% of the original volume. The volume factors based on the immobility of Hf show that the pisolite zone experienced a greater volume reduction than the gibbsite nodular zone. Absolute gains and losses relative to the parent basalt show the following relative order of depletion: Na > La > Eu > Sm > Co > Mn > Ce > Sc > Ta > V > Cr > Lu > Th > Fe > Ga > Al. The lesser mobility of Ce and Lu relative to other lanthanide elements suggests fractionation of lanthanide elements in the bauxite profile. Aluminum is both enriched and depleted at different depths in the gibbsite nodular zone suggesting that Al is mobilized from the matrix and possibly the pisolite zone into Al enriched gibbsite nodules. Volume reduction and destruction of relic textures in the pisolite zone is accompanied by small-scale mobilization of Th, Cr, Fe, Hf, Ga, Sc, and Ta during the formation of iron pisolites. Formation of the iron pisolite zone above the gibbsite nodular zone may indicate a change in climate from a heavy year round to a seasonal rainfall pattern. Close

• 10. [Article] Winter Precipitation Intensity and ENSO/PDO Variability in the Willamette Valley of Oregon

  There is growing concern about the effects of inter-annual climatic variability, such as the El-Niño Southern Oscillation (ENSO) and the Pacific Decadal Oscillation (PDO), on regional hydrology and water ...

  Citation × Citation Citation Abstract Copy Title: Winter Precipitation Intensity and ENSO/PDO Variability in the Willamette Valley of Oregon Author: Praskievicz, Sarah, Chang, Heejun Year: 2009 There is growing concern about the effects of inter-annual climatic variability, such as the El-Niño Southern Oscillation (ENSO) and the Pacific Decadal Oscillation (PDO), on regional hydrology and water resources. We analyzed patterns of wintertime precipitation intensity, using both simple intensity and number of heavy precipitation days per year, for eight stations in northwestern Oregon’s Willamette Valley for the period 1972–2006, and examined the separate and combined influence of ENSO and PDO on precipitation intensity. The analysis was accomplished using Kendall’s tau and analysis of variance (ANOVA) to determine differences in precipitation intensity among combinations of positive and negative ENSO and PDO phases. The results suggest that the relation between ENSO phase and precipitation intensity is negative in November and positive in April, while the relation between PDO and intensity is negative and strongest in January and March. These varying seasonal associations with ENSO/PDO phase may be related to the Willamette Valley’s location in the transitional zone between positive and negative El Niño response and to the moderating effects of out-of-phase ENSO/PDO. This seasonal variability of heavy rainfall has implications for the quantity and quality of regional water resources. Title: Winter Precipitation Intensity and ENSO/PDO Variability in the Willamette Valley of Oregon Author: Praskievicz, Sarah, Chang, Heejun Year: 2009 There is growing concern about the effects of inter-annual climatic variability, such as the El-Niño Southern Oscillation (ENSO) and the Pacific Decadal Oscillation (PDO), on regional hydrology and water resources. We analyzed patterns of wintertime precipitation intensity, using both simple intensity and number of heavy precipitation days per year, for eight stations in northwestern Oregon’s Willamette Valley for the period 1972–2006, and examined the separate and combined influence of ENSO and PDO on precipitation intensity. The analysis was accomplished using Kendall’s tau and analysis of variance (ANOVA) to determine differences in precipitation intensity among combinations of positive and negative ENSO and PDO phases. The results suggest that the relation between ENSO phase and precipitation intensity is negative in November and positive in April, while the relation between PDO and intensity is negative and strongest in January and March. These varying seasonal associations with ENSO/PDO phase may be related to the Willamette Valley’s location in the transitional zone between positive and negative El Niño response and to the moderating effects of out-of-phase ENSO/PDO. This seasonal variability of heavy rainfall has implications for the quantity and quality of regional water resources. Close