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Horizontal displacements and crooked fences along highway 287 north of Hebgen Lake. Hebgen Lake, Montana Earthquake. 1959.

Typed information on back of photograph: (Hall) 8/18/59, afternoon. Horizontal displacements and crooked fences along highway 287 north of Hebgen Lake. Looking westerly.

Categories: Image; Types: Map Service, OGC WFS Layer, OGC WMS Layer, OGC WMS Service; Tags: Earthquakes, Hall, W.B. Collection, Hebgen Lake, Montana Earthquake 1959, Menlo Park Collection, Montana (MT), All tags...

Stereo view of the slide. Hebgen Lake, Montana Earthquake. 1959.

Typed information on back of photograph: (Hall) 8/21/59. A stereo pair of the slide taken from the same hill as in S (hall_s).

Bear investigating items left behind by campers, taken from the north shore of Quake Lake. Hebgen Lake, Montana Earthquake. 1959.

Typed information on back of photograph: (Hall) 8/21/59. Taken from the north shore of Quake Lake. For location of this hill with respect to the slide see #66. The lake was very muddy. There is a bear investigating some camping equipment left by people when they were rescued. He also investigated the pack-sack containing Mr. Hall's cameras.

A closeup of broken pavement near one of the places where Highway 287 fell into the lake. Hebgen Lake, Montana Earthquake. 1959.

Typed information on back of photograph: (Hall) 8/21/59. A closeup of broken pavement near one of the places where the highway 287 fell into the lake. See hall_i.

Oblique aerial view of flood deposits below the junction of Lamar River with the Yellowstone. Yellowstone National Park, Wyoming. 1970.

Album caption: History and Dynamics of Glaciation in the Northern Yellowstone National Park. Oblique aerial view of flood deposits below the junction of Lamar River with the Yellowstone. Floodwaters more than 50 m deep from the Lamar River left deposits in the wider parts of the Yellowstone valley. A bedrock constriction at the downstream edge of the photograph caused hydraulic damming of the floodwater, resulting in lower velocities and deposition of floodgravels, especially against the valley walls and downstream from spurs. A shallow channel on the flood deposits parallels the near side of the Yellowstone River. Photograph by W.B. Hall, 1970. Wyoming, ca. 1968. No index card. Published as...

Categories: Image; Types: Map Service, OGC WFS Layer, OGC WMS Layer, OGC WMS Service; Tags: Hall, W.B. Collection, National Parks, Photographers, Pierce, K.L. Collection, Yellowstone National Park, All tags...

Looking northwest along the fault in front of the Highway department buildings. Hebgen Lake, Montana Earthquake. 1959.

Typed information on back of photograph: (Hall) 8/18/59 afternoon. Looking northwest along the fault in front of the Highway department buildings. The highway is beyond the sign.

Discarded camping gear and slide. Hebgen Lake, Montana Earthquake. 1959.

Typed information on back of photograph V: (Hall) 8/21/59. Much the same as U. Typed information on back of photograph U (missing during accession): (Hall) 8/21/59. From the same hill as S (hall_s). Discarded camping gear and slide.

Panorama of Hebgen Dam. Hebgen Lake, Montana Earthquake. 1959.

Typed information on back of photograph: K, L, M. (Hall) 8/21/59. These form a panorama of Hebgen dam and the fault scarp on the hill northeast of it. (If I had realized that was what they were I could have printed them so they fitted together better). Note: Hall_k, hall_l, hall_m form a panorama.

Oblique view, looking northward, of the southeastern part of the Washburn Range, showing its smoothed and rounded appearance. Yellowstone National Park, Wyoming. Circa 1968.

Album caption: History and Dynamics of Glaciation in the Northern Yellowstone National Park. Oblique view, looking northward, of the southeastern part of the Washburn Range, showing its smoothed and rounded appearance. This form is thought to reflect overriding of the entire range by a Pinedale icecap whose axis lay just south of the range (pl. 1A). Bedrock is commonly present within 0.3 m or so of the surface at altitudes above 2,680 m (8,800 ft), and fresh striations indicating glacial flow to the north occur all along the range crest. Dunraven Pass has a glacially rounded, U-shaped form, and striations on the north side of the pass indicate flow northward through the pass. Photograph by W.B. Hall. Wyoming, ca....

Highway 287 disappearing into the growing Quake Lake. Hebgen Lake, Montana Earthquake. 1959.

Typed information on back of photograph: (Hall) 8/21/59. Highway 287 disappearing into the growing Quake Lake. The mountain from which the slide came can be seen downstream (between the two groups of trees to the left).

Slide at the southwest end of Hebgen dam. Hebgen Lake, Montana Earthquake. 1959.

Typed information on back of photograph: (Hall) 8/21/59. Slide at the southwest end of Hebgen dam. The end of the concrete core shows at the lower left. At least part of this slide was new.

Looking west along highway 287 along the north shore of Hebgen Lake at the easternmost of four places where the road fell into the lake. Hebgen Lake, Montana Earthquake. 1959.

Typed information on back of photograph: (Hall) 8/21/59. Looking west along highway 287 along the north shore of Hebgen Lake at the easternmost of 4 places where the road fell into the lake due to quake-triggered slumps of unconsolidated material along the lake shore. The fault scarps here are higher on the hill in the trees. The material in the right foreground was pushed there by road machines making the emergency road around this slump. This road can be seen joining the highway.

Highway under water. Hebgen Lake, Montana Earthquake. 1959.

Typed information on back of photograph: (Hall) 8/21/59. Highway under water. See hall_i.

Close view of the lake and the highway sign for Rock Creek Campground. Hebgen Lake, Montana Earthquake. 1959.

Typed information on back of photograph: (Hall) 8/21/59. Taken from closer to the lake from the same hill as S (hall_s). Note the highway sign for the Rock Creek campground.

Panorama of Hebgen Dam. Hebgen Lake, Montana Earthquake. 1959.

Looking west along highway 287 along the north shore of Hebgen Lake at the easternmost of four places where the road fell into the lake. Hebgen Lake, Montana Earthquake. 1959.

Typed information on back of photograph: (Hall) 8/21/59. Another view of the same place as in I (hall_i).

Oblique view northwest over drumloid topography in Gardners Hole. Yellowstone National Park, Wyoming. Circa 1968.

Album caption: History and Dynamics of Glaciation in the Northern Yellowstone National Park. Oblique view northwest over drumloid topography in Gardners Hole. Flow direction is from left to right. A weakly developed soil of Pinedale age is developed on the surface till, but a clayey reddish weathering zone on an underlying till of inferred Bull Lake age is exposed where the Gardiner River has cut into the core of some drumlins. Photograph by W.B. Hall. Wyoming, ca. 1968. No index card. Published as Figure 22 in U.S. Geological Survey. Professional Paper 729-F. 1979.

Glacial scour features on Dome Mountain divide, 600 m above the Yellowstone River. Yellowstone National Park, Wyoming. Circa 1968.

Album caption: History and Dynamics of Glaciation in the Northern Yellowstone National Park. Glacial scour features on Dome Mountain divide, 600 m above the Yellowstone River. The northern Yellowstone outlet glacier filled Yankee Jim Canyon (pl. 1A) and spilled across the high pass in upper right and flowed towards left side of photograph. Note drumloid topography formed on scoured bedrock of Precambrian gneisses and Eocene volcanic rocks. Glacial polish is still apparent on roches moutonnées on the divide. Oblique aerial photograph by W.B. Hall. Wyoming, ca. 1968. No index card. Published as Figure 18 in U.S. Geological Survey. Professional Paper 729-F. 1979.

Oblique view to south of morainal backfill in Tom Miner Basin. Yellowstone National Park, Wyoming. Circa 1968.

Album caption: History and Dynamics of Glaciation in the Northern Yellowstone National Park. Oblique view to south of morainal backfill in Tom Miner Basin. Moraines sloping from left to right into Tom Miner Basin were deposited by the northern Yellowstone outlet glacier where it debouched from Yankee Jim Canyon (left of photograph). The outlet glacier carried erratics of Precambrian rocks far into Tom Miner Basin. When the highest level of the backfill was deposited, glaciers in Horse Creek valley, which lies beyond the right side of the photograph, had retreated well upvalley. Photograph by W.B. Hall. Wyoming, ca. 1968. No index card. Published as Figure 38 in U.S. Geological Survey. Professional...