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1. [Image] OIMB slide 5209


	daily temperature and salinity chart for Charleston
	Citation Citation Citation Abstract Copy Title: OIMB slide 5209 Author: unknown Year: 1972 daily temperature and salinity chart for Charleston Title: OIMB slide 5209 Author: unknown Year: 1972 daily temperature and salinity chart for Charleston

2. [Image] OSU Antarctic Station


	OSU oceanographers studied Antarctic under-ice water temperature, currents and salinity as part of a National Science Foundation research grant. The four-member team lived in one of the ten feet by twelve ...
	Citation Citation Citation Abstract Copy Title: OSU Antarctic Station Year: 1974 OSU oceanographers studied Antarctic under-ice water temperature, currents and salinity as part of a National Science Foundation research grant. The four-member team lived in one of the ten feet by twelve feet huts in the photo; the other served as their workspace. In September and October 1974, the crew experienced air temperatures with a wind chill of more than minus 100 degrees Fahrenheit. This photo first appeared in the January 1975 Oregon Stater. Title: OSU Antarctic Station Year: 1974 OSU oceanographers studied Antarctic under-ice water temperature, currents and salinity as part of a National Science Foundation research grant. The four-member team lived in one of the ten feet by twelve feet huts in the photo; the other served as their workspace. In September and October 1974, the crew experienced air temperatures with a wind chill of more than minus 100 degrees Fahrenheit. This photo first appeared in the January 1975 Oregon Stater.

3. [Image] Interior of a salmon canning establishment, Astoria, Oregon


	This shows the actual canning. Women are largely employed in the canneries for this particular part of the work. They become very skillful and are able to make very good wages, the sum usually depending ...
	Citation Citation Citation Abstract Copy Title: Interior of a salmon canning establishment, Astoria, Oregon Year: 1925 This shows the actual canning. Women are largely employed in the canneries for this particular part of the work. They become very skillful and are able to make very good wages, the sum usually depending upon the number of crates they are able to fill per day. Tests for weight are made while the cans are being filled and if any are found under weight they must be refilled. The lidding process follows. Some years ago the lids were placed by hand, then the cans run over a belt through a machine which soldered the lids. In late years most of the canneries have been provided with a new machine which entirely eliminates the soldering process. The lids are placed and crimped on automatically by one stroke of this machine. It is a most remarkable labor saving device, doing the work much more quickly and efficiently than the old soldering method. The cans are then stacked in crates and placed in a retort heated to the proper temperature. This drives the excess water and gases from the flesh, but the temperature is not hot enough to drive off the rich oils. The lids are then punctured and after the water and gas are freed the small holes are soldered and the cans again placed in a retort and the cooking process takes place. After cooking, the cans are cooled and stacked in the warehouse to await the lacquering, labeling and boxing for shipment. Title: Interior of a salmon canning establishment, Astoria, Oregon Year: 1925 This shows the actual canning. Women are largely employed in the canneries for this particular part of the work. They become very skillful and are able to make very good wages, the sum usually depending upon the number of crates they are able to fill per day. Tests for weight are made while the cans are being filled and if any are found under weight they must be refilled. The lidding process follows. Some years ago the lids were placed by hand, then the cans run over a belt through a machine which soldered the lids. In late years most of the canneries have been provided with a new machine which entirely eliminates the soldering process. The lids are placed and crimped on automatically by one stroke of this machine. It is a most remarkable labor saving device, doing the work much more quickly and efficiently than the old soldering method. The cans are then stacked in crates and placed in a retort heated to the proper temperature. This drives the excess water and gases from the flesh, but the temperature is not hot enough to drive off the rich oils. The lids are then punctured and after the water and gas are freed the small holes are soldered and the cans again placed in a retort and the cooking process takes place. After cooking, the cans are cooled and stacked in the warehouse to await the lacquering, labeling and boxing for shipment.

4. [Image] Roast Beef Experiment


	Mary Louise Armstrong (with knife) demonstrates differences between roast beef cooked at two different oven temperatures, circa 1945. Probably a demonstration by the Live Stock and Meat Board.
	Citation Citation Citation Abstract Copy Title: Roast Beef Experiment Year: 1945 Mary Louise Armstrong (with knife) demonstrates differences between roast beef cooked at two different oven temperatures, circa 1945. Probably a demonstration by the Live Stock and Meat Board. Title: Roast Beef Experiment Year: 1945 Mary Louise Armstrong (with knife) demonstrates differences between roast beef cooked at two different oven temperatures, circa 1945. Probably a demonstration by the Live Stock and Meat Board.

5. [Image] Snow scene with Fairbanks Hall, 1919


	This image shows Cauthorn Hall (now Fairbanks Hall) in the snow during the December 21, 1919 storm in which Corvallis received 22 inches of snow and recorded an all-time low temperature of -14 degrees ...
	Citation Citation Citation Abstract Copy Title: Snow scene with Fairbanks Hall, 1919 Author: Evans, Alice Kidder; Kidder, Andrew B. Year: 1919 This image shows Cauthorn Hall (now Fairbanks Hall) in the snow during the December 21, 1919 storm in which Corvallis received 22 inches of snow and recorded an all-time low temperature of -14 degrees F. Title: Snow scene with Fairbanks Hall, 1919 Author: Evans, Alice Kidder; Kidder, Andrew B. Year: 1919 This image shows Cauthorn Hall (now Fairbanks Hall) in the snow during the December 21, 1919 storm in which Corvallis received 22 inches of snow and recorded an all-time low temperature of -14 degrees F.

6. [Image] Snow field, Mt. Rainier


	Image Description from historic lecture booklet: "Where snow endures from year to year over any considerable area, it constitutes a snow-field. Snow-fields occur in mountains in nearly all latitudes. The ...
	Citation Citation Citation Abstract Copy Title: Snow field, Mt. Rainier Year: 1915 Image Description from historic lecture booklet: "Where snow endures from year to year over any considerable area, it constitutes a snow-field. Snow-fields occur in mountains in nearly all latitudes. The snow-line in the mountains is the line above which the snow is not all melted in summer. Its position is influenced by several conditions, one of which is temperature. Another is the amount of snowfall." Title: Snow field, Mt. Rainier Year: 1915 Image Description from historic lecture booklet: "Where snow endures from year to year over any considerable area, it constitutes a snow-field. Snow-fields occur in mountains in nearly all latitudes. The snow-line in the mountains is the line above which the snow is not all melted in summer. Its position is influenced by several conditions, one of which is temperature. Another is the amount of snowfall."

7. [Image] Best trout stream and trout surveys


	Two manuscripts are featured in this document. The first discusses how the Deschutes River is an ideal place for trout, not only for sport but for the fish to inhabit. The river benefits from the lack ...
	Citation Citation Citation Abstract Copy Title: Best trout stream and trout surveys Author: Finley, William L. (William Lovell), 1876-1953 Year: 1935 Two manuscripts are featured in this document. The first discusses how the Deschutes River is an ideal place for trout, not only for sport but for the fish to inhabit. The river benefits from the lack of silt in the water and protection from dumping pollutants. Also due to a lack of a paved road, access is limited to the area. The second manuscript discusses the importance of conducting surveys that determine what makes a place suitable for a fish to inhabit. Factors such as what are the food sources and water temperature are to be considered. The writer makes the point that one cannot gauge from mere visual observation the amount of fish in any given stream. To truly determine the population, in depth surveys must be done. Title: Best trout stream and trout surveys Author: Finley, William L. (William Lovell), 1876-1953 Year: 1935 Two manuscripts are featured in this document. The first discusses how the Deschutes River is an ideal place for trout, not only for sport but for the fish to inhabit. The river benefits from the lack of silt in the water and protection from dumping pollutants. Also due to a lack of a paved road, access is limited to the area. The second manuscript discusses the importance of conducting surveys that determine what makes a place suitable for a fish to inhabit. Factors such as what are the food sources and water temperature are to be considered. The writer makes the point that one cannot gauge from mere visual observation the amount of fish in any given stream. To truly determine the population, in depth surveys must be done.

8. [Image] Arlington, Ore. Jan. 12, 1909, 20 below zero. Columbia River Frozen over, The first time in 24 years.


	A view of the Columbia River shore at Arlington, Oregon, on January 12, 1909. The Columbia River is frozen. In the foreground is the white riverbank, with a large boulder to the left. Near the shore on ...
	Citation Citation Citation Abstract Copy Title: Arlington, Ore. Jan. 12, 1909, 20 below zero. Columbia River Frozen over, The first time in 24 years. A view of the Columbia River shore at Arlington, Oregon, on January 12, 1909. The Columbia River is frozen. In the foreground is the white riverbank, with a large boulder to the left. Near the shore on the right of the photo is a pier, with a sailboat at its end. In the center we see a stern-wheeler. A long rope leads out from it and is coiled on the frozen river. A group of five men stand nearby, close to a rectangular area of water that has been freed of ice. Their attention is on a sixth man who is standing in a rowboat pushing at the ice with a long pole. One of the group on the river also carries a long pole. The writing on the photograph says the temperature is 20 below zero and the first time in 24 years the river had frozen over. Title: Arlington, Ore. Jan. 12, 1909, 20 below zero. Columbia River Frozen over, The first time in 24 years. A view of the Columbia River shore at Arlington, Oregon, on January 12, 1909. The Columbia River is frozen. In the foreground is the white riverbank, with a large boulder to the left. Near the shore on the right of the photo is a pier, with a sailboat at its end. In the center we see a stern-wheeler. A long rope leads out from it and is coiled on the frozen river. A group of five men stand nearby, close to a rectangular area of water that has been freed of ice. Their attention is on a sixth man who is standing in a rowboat pushing at the ice with a long pole. One of the group on the river also carries a long pole. The writing on the photograph says the temperature is 20 below zero and the first time in 24 years the river had frozen over.

9. [Image] Arlington, Ore. Jan. 12, 1909, 20 below zero. Columbia River Frozen over, The first time in 24 years.


	A view of the Columbia River shore at Arlington, Oregon, on January 12, 1909. The Columbia River is frozen. In the foreground is the white riverbank, with a large boulder to the left. Near the shore on ...
	Citation Citation Citation Abstract Copy Title: Arlington, Ore. Jan. 12, 1909, 20 below zero. Columbia River Frozen over, The first time in 24 years. A view of the Columbia River shore at Arlington, Oregon, on January 12, 1909. The Columbia River is frozen. In the foreground is the white riverbank, with a large boulder to the left. Near the shore on the right of the photo is a pier, with a sailboat at its end. In the center we see a stern-wheeler. A long rope leads out from it and is coiled on the frozen river. A group of five men stand nearby, close to a rectangular area of water that has been freed of ice. Their attention is on a sixth man who is standing in a rowboat pushing at the ice with a long pole. One of the group on the river also carries a long pole. The writing on the photograph says the temperature is 20 below zero and the first time in 24 years the river had frozen over. Title: Arlington, Ore. Jan. 12, 1909, 20 below zero. Columbia River Frozen over, The first time in 24 years. A view of the Columbia River shore at Arlington, Oregon, on January 12, 1909. The Columbia River is frozen. In the foreground is the white riverbank, with a large boulder to the left. Near the shore on the right of the photo is a pier, with a sailboat at its end. In the center we see a stern-wheeler. A long rope leads out from it and is coiled on the frozen river. A group of five men stand nearby, close to a rectangular area of water that has been freed of ice. Their attention is on a sixth man who is standing in a rowboat pushing at the ice with a long pole. One of the group on the river also carries a long pole. The writing on the photograph says the temperature is 20 below zero and the first time in 24 years the river had frozen over.

10. [Image] Alpine Glaciers


	Image Description from historic lecture booklet: "Of the three great classes referred to above, the most widely known is the alpine type, which derives its name from the mountains of central Europe, where ...
	Citation Citation Citation Abstract Copy Title: Alpine Glaciers Year: 1915 Image Description from historic lecture booklet: "Of the three great classes referred to above, the most widely known is the alpine type, which derives its name from the mountains of central Europe, where it was first studied. Alpine glaciers occur about high peak and on the summits and flanks of mountain ranges in many parts of the world, but reach their most perfect development in temperate regions. The Himalayas, the Alps, the mountains of Scandinavia, the Southern Alps of New Zealand, the Cordilleras, etc., furnish well-known examples. Glaciers of this type originate as a rule in amphitheaters and cirques, partially surrounded by lofty peaks and overshadowing precipices, and flow through rugged valleys leading from them as winding ice rivers which carry the excess of snow falling on the mountains into the lower regions, where a higher mean annual temperature causes it to melt. They are essentially streams of ice, formed usually by the union of many branches, and end abruptly when the drainage changes from a solid to a liquid form." Title: Alpine Glaciers Year: 1915 Image Description from historic lecture booklet: "Of the three great classes referred to above, the most widely known is the alpine type, which derives its name from the mountains of central Europe, where it was first studied. Alpine glaciers occur about high peak and on the summits and flanks of mountain ranges in many parts of the world, but reach their most perfect development in temperate regions. The Himalayas, the Alps, the mountains of Scandinavia, the Southern Alps of New Zealand, the Cordilleras, etc., furnish well-known examples. Glaciers of this type originate as a rule in amphitheaters and cirques, partially surrounded by lofty peaks and overshadowing precipices, and flow through rugged valleys leading from them as winding ice rivers which carry the excess of snow falling on the mountains into the lower regions, where a higher mean annual temperature causes it to melt. They are essentially streams of ice, formed usually by the union of many branches, and end abruptly when the drainage changes from a solid to a liquid form."