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Leroy Radanovich's Mariposa Life
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THE ECONOMY OF MARIPOSA COUNTY AND THE FERGUSON ROCK SLIDE (Part Two) A number of issues come together with the announcement of the availability of issuance of an Environmental Assessment/Initial Study and the date of a Public Hearing on the Ferguson Slide Restoration Project. The documents will be available at the Mariposa County Library from Monday, November 19, 2007 to January 3, 2008 with the Public Hearing from 5:30 PM to 8:00 PM at the Board Chambers of the Mariposa County Board of Supervisors on November 28, 2007. Copies of the documents will also be available at the El Portal Post Office and from CalTrans at the District Office, 1976 E. Charter Way, Stockton, CA 95201. This begins the process of correcting the effects of the devastating Ferguson Slide that occurred April 29, 2006, closing Hwy 140 into Yosemite for four and one half months. Detour bridges reopened the highway with restrictions which included one way traffic and vehicles no more than 28ft in length. The economic impact of this slide on Mariposa County residents and businesses has been significant and variable. While the average visitor and resident has been able to use Hwy 140 with only short delays, it has been the lack of access by the larger vehicles, emergency vehicles, school busses, motor homes, and larger trucks that has caused a great deal of costs. The significant increase in costs to deliver goods and supplies to Yosemite Valley, plus the increased fuel costs, has added to the cost of visiting Yosemite. This will be made more difficult by the winter weather. We (the Lodging Industry) have been working diligently to increase visitation to Yosemite to assist the economic problems that Mariposa County has. It is the increase in TOT (Bed Tax) that offers the greatest opportunity for the county to meet its obligations. Three alternative projects will be offered in the documents, both requiring bridges to cross the river above and below the slide, one using a tunnel, another a cut in the mountain, and a third using a viaduct which access a notch in the shoulder of the hill opposite the slide. Congressman Radanovich has announced that funds for the reconstruction will be available from the Federal Government. A few weeks ago, and unreported in the local press, an important study by the U.S. Geological Survey was delivered to the Board of Supervisors by Ken Gosting, Executive Director of TIE, the public interest organization with close ties to transportation of all aspects in California. The study crafted by Federal Geologist Roger P. Denlinger, covers the potential effects of the slide moving into the Merced River canyon at some future date. Denlinger does not predict if and when that will happen, or to what degree, although he has been studying this body of rock extensively and finds that in all likelihood it will move. As stated in the report, the purpose of the study was to assess the hazard posed by the Ferguson rockslide by simulating the run out and deposition of a portions of the slide if rapid failure occurs. As stated, the report does not address the likelihood of rapid failure. The rockslide is described as having a number of large tension cracks transecting the body from toe to head wall. This means that the slide could move in sections at different rates with the toe moving faster than the middle portion or the near the headwall. The study then states its purpose to delineate the hazards created by the potential rapid release of all or part of the mass. A major contributing factor in the possible slippage will be the content of water from rain or snow. The angle of the slope is an important factor. If there is a maximum deposition of talus and it fans out, the depth of debris would be 22 meters or 67.1 ft., somewhat less than the depth that had been speculated by earlier estimations. In a less than full slide the toe of the slide would be estimated to cover about 2/3 of the river with no full blockage. In other words the fan would not cross the river. In any case, significant enough material would continue to cause the inability to restore the original road bed, necessitating crossing the river with the repair. The maximum depth of debris would be about 100 ft if all of the material available were to come down at once. It appears that a smaller slide would reduce the opportunity for a catastrophic event none the less would continue to occur in stages for a longer period of time. If one were prepared to remove 780,000 cubic meters of material and store it at a nearby location, then restoration of the present roadway might be possible but it seems that it is no longer a consideration because of a number of factors which include safety, possibility of future events and the cost of removing the material and transporting it to some location away from the river. Environmental considerations enter into this non-option. The hearing on November 28, 2007 will result in the adoption of a Negative Declaration/Finding of No Significant Impact and the Initial Study/Environmental Assessment leading to the constructing of one of four alternative projects or possibly a no project option (Right). The three alternatives given at the beginning of this article are the ones being considered. It can not come too soon. We have worked hard to keep the primary economic asset of Mariposa County viable. There are other challenges for the future based on taking too long to complete the project, but at least the road should not be one of them. Leroy Radanovich Leroy Radanovich Email: Leroy Radanovich To Read More By Leroy Radanovich: Leroy Radanovich's Mariposa Life Archives |
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November 20, 2007
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