Search

Search Results

• 21. [Image] South Carolina Geothermal Program Final Report; Tectogenesis of the Rocks Surrounding the Winnsboro Intrusive Complex and Reconnaissance and Petrography of the Pageland Pluton

  	Major post-tectonic plutons of the easternmost Piedmont in the southern Appalachians have been of primary interest because of their high radiogenic heat production. Such heat production comes from a linear ...
  	Citation × Citation Citation Abstract Copy Title: South Carolina Geothermal Program Final Report; Tectogenesis of the Rocks Surrounding the Winnsboro Intrusive Complex and Reconnaissance and Petrography of the Pageland Pluton Author: Bourland, W.C. Year: 1978 Major post-tectonic plutons of the easternmost Piedmont in the southern Appalachians have been of primary interest because of their high radiogenic heat production. Such heat production comes from a linear map trend including the Winnsboro, Liberty Hill, Pageland, and Lilesville plutons which parallel the proposed eastern Piedmont Fault system of Hatcher and others (1977). This study, in examining regional versus contact metamorphism and crosscutting relationships between the Winnsboro and Pageland complexes and the major folds and mylonitic zones of this area, provides a relative time framework for the tectonic and plutonic events Title: South Carolina Geothermal Program Final Report; Tectogenesis of the Rocks Surrounding the Winnsboro Intrusive Complex and Reconnaissance and Petrography of the Pageland Pluton Author: Bourland, W.C. Year: 1978 Major post-tectonic plutons of the easternmost Piedmont in the southern Appalachians have been of primary interest because of their high radiogenic heat production. Such heat production comes from a linear map trend including the Winnsboro, Liberty Hill, Pageland, and Lilesville plutons which parallel the proposed eastern Piedmont Fault system of Hatcher and others (1977). This study, in examining regional versus contact metamorphism and crosscutting relationships between the Winnsboro and Pageland complexes and the major folds and mylonitic zones of this area, provides a relative time framework for the tectonic and plutonic events Close

• 22. [Image] Wet Geothermal Potential of the Kingman-Williams Region, Arizona

  	The Kingman-Williams region, Arizona, possesses few thermal waters of deep origin. Evaluation of 33 waters (8 thermal) reveals that thermal waters are restricted to the Basin and Range tectonic province; ...
  	Citation × Citation Citation Abstract Copy Title: Wet Geothermal Potential of the Kingman-Williams Region, Arizona Author: Goff, F.E. Year: 1979 The Kingman-Williams region, Arizona, possesses few thermal waters of deep origin. Evaluation of 33 waters (8 thermal) reveals that thermal waters are restricted to the Basin and Range tectonic province; no thermal waters were found on the west margin of the Colorado Plateau. The thermal waters appear to rise along north-trending normal faults or flow in deep aquifers in Quaternary sedimentary basins of the Basin and Range province. All thermal waters have distinctive chemistry and discharge at temperatures ranjinj from 28-46°C. They Apparently issue from small isolated jeothermal reservoirs. Geothermometry and chemistry indicate that these are low-temperature reservoirs that probably do not exceed 115°C Title: Wet Geothermal Potential of the Kingman-Williams Region, Arizona Author: Goff, F.E. Year: 1979 The Kingman-Williams region, Arizona, possesses few thermal waters of deep origin. Evaluation of 33 waters (8 thermal) reveals that thermal waters are restricted to the Basin and Range tectonic province; no thermal waters were found on the west margin of the Colorado Plateau. The thermal waters appear to rise along north-trending normal faults or flow in deep aquifers in Quaternary sedimentary basins of the Basin and Range province. All thermal waters have distinctive chemistry and discharge at temperatures ranjinj from 28-46°C. They Apparently issue from small isolated jeothermal reservoirs. Geothermometry and chemistry indicate that these are low-temperature reservoirs that probably do not exceed 115°C Close

• 23. [Image] The geology and geochemistry of thirteen cinder cones at Crater Lake National Park, Oregon

  	ill.; maps; Thesis (M.S.)--University of Oregon, 1985; Includes vita and abstract; Includes bibliographical references (leaves 154-158)
  	Citation × Citation Citation Abstract Copy Title: The geology and geochemistry of thirteen cinder cones at Crater Lake National Park, Oregon Author: Prueher, Elizabeth M., 1957- Year: 1985, 2009 ill.; maps; Thesis (M.S.)--University of Oregon, 1985; Includes vita and abstract; Includes bibliographical references (leaves 154-158) Title: The geology and geochemistry of thirteen cinder cones at Crater Lake National Park, Oregon Author: Prueher, Elizabeth M., 1957- Year: 1985, 2009 ill.; maps; Thesis (M.S.)--University of Oregon, 1985; Includes vita and abstract; Includes bibliographical references (leaves 154-158) Close

• 24. [Image] A Time Domain Survey of the Los Alamos Region, New Mexico

  	A time domain electromagnetic sounding survey of the region surrounding the city of Los Alamos, New Mexico was carried out. The results show that a linear trough, trending northeast--southwest runs beneath ...
  	Citation × Citation Citation Abstract Copy Title: A Time Domain Survey of the Los Alamos Region, New Mexico Author: Williston, McNeiI and Associates Year: 1979 A time domain electromagnetic sounding survey of the region surrounding the city of Los Alamos, New Mexico was carried out. The results show that a linear trough, trending northeast--southwest runs beneath the city. The southern boundary is somewhat to the south of the city, the northern boundary was not established. The geoelectric section consists of three layers and the total thickness of the section is in excess of 3 000 m. The resistivities of the second layer are as low as 2.5 ..cap omega.. m. If the salinities are in the region of 7 000 ppm, the resistivities could indicate that water with a temperature of 150/sup 0/C may be found at a depth of 3 000 m. Title: A Time Domain Survey of the Los Alamos Region, New Mexico Author: Williston, McNeiI and Associates Year: 1979 A time domain electromagnetic sounding survey of the region surrounding the city of Los Alamos, New Mexico was carried out. The results show that a linear trough, trending northeast--southwest runs beneath the city. The southern boundary is somewhat to the south of the city, the northern boundary was not established. The geoelectric section consists of three layers and the total thickness of the section is in excess of 3 000 m. The resistivities of the second layer are as low as 2.5 ..cap omega.. m. If the salinities are in the region of 7 000 ppm, the resistivities could indicate that water with a temperature of 150/sup 0/C may be found at a depth of 3 000 m. Close

• 25. [Image] Geothermal Progress Monitor. Progress Report No. 4, September 1980

  	The following are included: geothermal power plants proposed and on-line; direct heat applications proposed and operational; trends in drilling activities; exploration; leases; outreach and technical assistance; ...
  	Citation × Citation Citation Abstract Copy Title: Geothermal Progress Monitor. Progress Report No. 4, September 1980 Author: Assistant Secretary for Resource Applications, Division of Geothermal Resource Management Year: 1980 The following are included: geothermal power plants proposed and on-line; direct heat applications proposed and operational; trends in drilling activities; exploration; leases; outreach and technical assistance; feasibility studies and application demonstrations; geothermal loan guaranty program; research and development activities; legal, institutional, and regulatory activities; environmental activities; reports and publications; and a directory (MHR) Title: Geothermal Progress Monitor. Progress Report No. 4, September 1980 Author: Assistant Secretary for Resource Applications, Division of Geothermal Resource Management Year: 1980 The following are included: geothermal power plants proposed and on-line; direct heat applications proposed and operational; trends in drilling activities; exploration; leases; outreach and technical assistance; feasibility studies and application demonstrations; geothermal loan guaranty program; research and development activities; legal, institutional, and regulatory activities; environmental activities; reports and publications; and a directory (MHR) Close

• 26. [Image] Oil Sands and Heavy Oils of Alberta

  	About 82 percent of the oil produced in Canada comes from Alberta. For a number of years following major discoveries in 1947, additions to reserves exceeded production in the province. In 1970, however, ...
  	Citation × Citation Citation Abstract Copy Title: Oil Sands and Heavy Oils of Alberta Author: McRory, R. E. Year: 1982 About 82 percent of the oil produced in Canada comes from Alberta. For a number of years following major discoveries in 1947, additions to reserves exceeded production in the province. In 1970, however, this trend was reversed and has continued for the past 11 years. As a result, the Alberta Energy Resources Conservation Board (ERCB) reported that remaining established reserves at the end of 1980 had declined to 4.53 billion barrels. At 1980 rates of production these reserves could be fully depleted by 1992 Title: Oil Sands and Heavy Oils of Alberta Author: McRory, R. E. Year: 1982 About 82 percent of the oil produced in Canada comes from Alberta. For a number of years following major discoveries in 1947, additions to reserves exceeded production in the province. In 1970, however, this trend was reversed and has continued for the past 11 years. As a result, the Alberta Energy Resources Conservation Board (ERCB) reported that remaining established reserves at the end of 1980 had declined to 4.53 billion barrels. At 1980 rates of production these reserves could be fully depleted by 1992 Close

• 27. [Image] Theodore Roosevelt Junior High School (Eugene, Oregon)

  	The 1949–1950 International Style Roosevelt Junior High (Middle) School, in Eugene, Lane County, Oregon, was designed by Portland architects Wolff and Phillips. Built to its current configuration over ...
  	Citation × Citation Citation Abstract Copy Title: Theodore Roosevelt Junior High School (Eugene, Oregon) Author: Wolff, George M.; Phillips, Truman E.; Wolff & Phillips Year: 1949 The 1949–1950 International Style Roosevelt Junior High (Middle) School, in Eugene, Lane County, Oregon, was designed by Portland architects Wolff and Phillips. Built to its current configuration over a period of years, it replaced the 1924 Roosevelt Junior High, which was converted to Condon Elementary School in 1953 and is now owned by the University of Oregon, known as Agate Hall. The subject school is representative of the community’s response to post-World War II population growth as well as the changing architectural trends of the mid-twentieth century. The building was razed in 2016 and replaced by a new school building, Roosevelt Middle School. Title: Theodore Roosevelt Junior High School (Eugene, Oregon) Author: Wolff, George M.; Phillips, Truman E.; Wolff & Phillips Year: 1949 The 1949–1950 International Style Roosevelt Junior High (Middle) School, in Eugene, Lane County, Oregon, was designed by Portland architects Wolff and Phillips. Built to its current configuration over a period of years, it replaced the 1924 Roosevelt Junior High, which was converted to Condon Elementary School in 1953 and is now owned by the University of Oregon, known as Agate Hall. The subject school is representative of the community’s response to post-World War II population growth as well as the changing architectural trends of the mid-twentieth century. The building was razed in 2016 and replaced by a new school building, Roosevelt Middle School. Close

• 28. [Image] Theodore Roosevelt Junior High School (Eugene, Oregon)

  	The 1949–1950 International Style Roosevelt Junior High (Middle) School, in Eugene, Lane County, Oregon, was designed by Portland architects Wolff and Phillips. Built to its current configuration over ...
  	Citation × Citation Citation Abstract Copy Title: Theodore Roosevelt Junior High School (Eugene, Oregon) Author: Wolff, George M.; Phillips, Truman E.; Wolff & Phillips Year: 1949 The 1949–1950 International Style Roosevelt Junior High (Middle) School, in Eugene, Lane County, Oregon, was designed by Portland architects Wolff and Phillips. Built to its current configuration over a period of years, it replaced the 1924 Roosevelt Junior High, which was converted to Condon Elementary School in 1953 and is now owned by the University of Oregon, known as Agate Hall. The subject school is representative of the community’s response to post-World War II population growth as well as the changing architectural trends of the mid-twentieth century. The building was razed in 2016 and replaced by a new school building, Roosevelt Middle School. Title: Theodore Roosevelt Junior High School (Eugene, Oregon) Author: Wolff, George M.; Phillips, Truman E.; Wolff & Phillips Year: 1949 The 1949–1950 International Style Roosevelt Junior High (Middle) School, in Eugene, Lane County, Oregon, was designed by Portland architects Wolff and Phillips. Built to its current configuration over a period of years, it replaced the 1924 Roosevelt Junior High, which was converted to Condon Elementary School in 1953 and is now owned by the University of Oregon, known as Agate Hall. The subject school is representative of the community’s response to post-World War II population growth as well as the changing architectural trends of the mid-twentieth century. The building was razed in 2016 and replaced by a new school building, Roosevelt Middle School. Close

• 29. [Image] Theodore Roosevelt Junior High School (Eugene, Oregon)

  	The 1949–1950 International Style Roosevelt Junior High (Middle) School, in Eugene, Lane County, Oregon, was designed by Portland architects Wolff and Phillips. Built to its current configuration over ...
  	Citation × Citation Citation Abstract Copy Title: Theodore Roosevelt Junior High School (Eugene, Oregon) Author: Wolff, George M.; Phillips, Truman E.; Wolff & Phillips Year: 1949 The 1949–1950 International Style Roosevelt Junior High (Middle) School, in Eugene, Lane County, Oregon, was designed by Portland architects Wolff and Phillips. Built to its current configuration over a period of years, it replaced the 1924 Roosevelt Junior High, which was converted to Condon Elementary School in 1953 and is now owned by the University of Oregon, known as Agate Hall. The subject school is representative of the community’s response to post-World War II population growth as well as the changing architectural trends of the mid-twentieth century. The building was razed in 2016 and replaced by a new school building, Roosevelt Middle School. Title: Theodore Roosevelt Junior High School (Eugene, Oregon) Author: Wolff, George M.; Phillips, Truman E.; Wolff & Phillips Year: 1949 The 1949–1950 International Style Roosevelt Junior High (Middle) School, in Eugene, Lane County, Oregon, was designed by Portland architects Wolff and Phillips. Built to its current configuration over a period of years, it replaced the 1924 Roosevelt Junior High, which was converted to Condon Elementary School in 1953 and is now owned by the University of Oregon, known as Agate Hall. The subject school is representative of the community’s response to post-World War II population growth as well as the changing architectural trends of the mid-twentieth century. The building was razed in 2016 and replaced by a new school building, Roosevelt Middle School. Close

• 30. [Image] Theodore Roosevelt Junior High School (Eugene, Oregon)

  	The 1949–1950 International Style Roosevelt Junior High (Middle) School, in Eugene, Lane County, Oregon, was designed by Portland architects Wolff and Phillips. Built to its current configuration over ...
  	Citation × Citation Citation Abstract Copy Title: Theodore Roosevelt Junior High School (Eugene, Oregon) Author: Wolff, George M.; Phillips, Truman E.; Wolff & Phillips Year: 1949 The 1949–1950 International Style Roosevelt Junior High (Middle) School, in Eugene, Lane County, Oregon, was designed by Portland architects Wolff and Phillips. Built to its current configuration over a period of years, it replaced the 1924 Roosevelt Junior High, which was converted to Condon Elementary School in 1953 and is now owned by the University of Oregon, known as Agate Hall. The subject school is representative of the community’s response to post-World War II population growth as well as the changing architectural trends of the mid-twentieth century. The building was razed in 2016 and replaced by a new school building, Roosevelt Middle School. Title: Theodore Roosevelt Junior High School (Eugene, Oregon) Author: Wolff, George M.; Phillips, Truman E.; Wolff & Phillips Year: 1949 The 1949–1950 International Style Roosevelt Junior High (Middle) School, in Eugene, Lane County, Oregon, was designed by Portland architects Wolff and Phillips. Built to its current configuration over a period of years, it replaced the 1924 Roosevelt Junior High, which was converted to Condon Elementary School in 1953 and is now owned by the University of Oregon, known as Agate Hall. The subject school is representative of the community’s response to post-World War II population growth as well as the changing architectural trends of the mid-twentieth century. The building was razed in 2016 and replaced by a new school building, Roosevelt Middle School. Close