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(Information taken from the US Forest Service view site information kiosk and from personal recollections.) |
Photos by Venita* |
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Above: This view from the US Forest Service view site at the top of the pass through Billy's Mountain reveals the size of the land movement. U.S. Geological Survey Post-disaster investigations revealed that the debris, a moderately plastic gravelly clay, slid on a trough-shaped depression in bedrock. The site has apparently been involved in repeated landslides and earthflow movement through historic and pre-historic time. However, there is good geoligic evidence that the 1983 land movement was unprecedented in at least the past several hundred years. |
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Above: View from the original road level at the bottom of the canyon, just north of the Spanish Fork River. The dirt road in the photo was used by equipment working to stabalize the dam. In five days, Thistle Slide created a lake 2.5 miles long and 200 feet deep covering an estimated 900 acres. With the stability of the natural dam in question, it was decided to stabalize the dam and drain the lake. Construction of an upper spillway tunnel [upper left] was completed in May while water was being piped over the dam from a temporary barge on the lake. Later, a lower drainage tunnel was constructed to drain the rest of the lake (Dec. 1983). This tunnel is the current passage under the dam for the river. |
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Above: View from the old canyon road alongside Spanish Fork River, now muddy with spring run off. Two Denver and Rio Grande railway lines were blocked as well as Highway 6 and 89. This view shows the two tunnels built through Billie's Mountain to re-route the rail lines, well above the previous river level location. |
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Above: Originally, the river, canyon road and railroad all flowed around the south end of Billy's Mountain which presented a steep and forbidding climb. Because of "Thistle Lake," Billy's was confronted. The railroad tunnels through the mountain are seen at the right where the train has just exited on its way down the canyon from the Carbon County coalfields in eastern Utah to industries in Utah County and beyond. New Highway 6/89 rises on a steeper grade to the huge gash at the top. Just beyond this summit the highways divide with Highway 6 continuing east and Highway 89 turning south to Sanpete County and beyond. Bottom: At the summit we see the angle of the man-made cut and various colors of the sand and sandstone that make up Billy's Mountain. The US Forest Service has provided a view site and information kiosk here for information about the landslip and for photo opportunities. |
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Many people hoped "Thistle Lake" could remain and become another water recreation and fishing site. However, the experts determined that the dam was unstable and would probably fail someday and flood the towns between it and Utah Lake. Not only that, the lake was filled with all sorts of dangerous debris of all sizes, including buildings from the small town of Thistle that it had drowned. All the Thistle residents were safely evacuated with the help of family, neighbors and volunteers, leaving behind their homes and flooded dreams. After the lake was drained, some residents returned to claim whatever they could and others never looked back. A few rebuilt and started over. Since 1984, Mother Nature has replanted much of the land with native grasses and sagebrush, but evidence of the disaster is still easily seen. Let's go over the hill and see some remains of the flood. |
*Unless otherwise noted, all photos on this website were taken by Venita, who also holds the copyright. Should you wish to download any of them for any reason (other than your own enjoyment), please credit Venita as the photographer and add my URL: http://www.venitap.com/home.html Comments are appreciated! |
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