Quake, Rattle and Roll | SierraSun.com

Quake, Rattle and Roll

The devastating earthquake that ripped along Californias San Andreas Fault on April 18, 1906, ranks as a legendary seismic event in the annals of western history. The violent 7.8-magnitude temblor shook most of California, parts of western Nevada and southern Oregon, and spiked seismographs as far away as Germany and Japan. The San Andreas Fault is the result of tectonic plate movement near the California Coast, but growing mountain ranges like the Sierra Nevada are also home to frequent shakes. The 1872 Lone Pine earthquake is recognized as the most impressive example of mountain building since the first settlements along the Eastern Sierra Front.

In the Far West, terra firma is an illusion. Alaska experiences the most earthquakes in the country, but California and Nevada rank second and third respectively. Together they account for about 80 percent of all quakes in the 48 contiguous states. The magnificent Sierra Nevada is roughly 400 miles long and 45 miles wide, sculpted by glacial ice into steep, deep canyons and elevated peaks exceeding 14,000 feet high. To the casual hiker, climber or skier, the range may seem stable, but it is really in a constant state of uplift. This helps offset the weathering process that would otherwise slowly wear the mountains down. Mountains rise along faults, and earthquakes result from this building process. Lake Tahoe lies on the western rim of the Basin and Range province, one of the most seismically active regions in the United States. The Tahoe basin was formed about 3.6 million years ago when a fault on the eastern margin created the Carson Range, and a massive upthrust to the west forced the Sierra Nevada up out of a shallow sea. The landmass between these two ranges collapsed and over time filled with water. The Sierra is actually enormous blocks of granite tilted toward the Pacific Ocean, which produce a 35-mile gradual slope on the west, and a steep, 10-mile descent on the east. The westward tilt of the large fault blocks in the Sierra uplift generated towering walls of granite along its eastern edge, which today represent the highest peaks in the Tahoe Basin, such as Freel Peak (10,881), Pyramid Peak (9,983 in Desolation Wilderness), and Mt. Tallac (9,735).

Scientists studying the bottom of Lake Tahoe have found evidence of huge landslides they think were triggered by ancient earthquakes of magnitude 7.0 or larger. Chunks of rock and dirt the size of city blocks may have loosened from surrounding mountains and smashed into the lake during powerful temblors thousands of years ago. Geologists have also warned that several faults that lie directly beneath Lake Tahoe are thought capable of generating a 7.1-magnitude quake and enough movement to produce tsunami waves exceeding 30 feet high. But dont panic and sell your lakefront home scientists estimate the risk of a magnitude 7 quake under Lake Tahoe in the next 50 years to be between three and four percent, far less than the perennial dangers of forest fires and floods in the region. Experts do suggest, however, that if you are near the lakes shoreline and feel a severe tremor that last for more than 10 seconds, first duck and cover and then sprint 30 feet in elevation.

Few people ever see a mountain range grow, but on March 26, 1872, the 300 residents of Lone Pine, Calif., did. The small hamlet is located on the Sierra east slope near the Owens Valley, about 350 miles south of Reno. This extraordinary seismic event occurred on a clear calm night under a bright full moon. At 2:30 a.m. sleeping residents in Lone Pine were awakened by a sound like rumbling thunder accompanied by the crash of falling dishes, mirrors and glassware. The heaving ground broke plaster from ceilings and tossed water pitchers six feet into the air. Citizens grabbed what clothes they could and ran from their collapsing homes in stark terror. Timber is very scarce in this region and all the dwellings were built of adobe brick. The brittle adobe construction offered no safety in the severe quake and the destruction in Lone Pine was nearly total. Out of the 62 buildings lining Main Street, 52 crashed to the ground in piles of rubble. Falling bricks and debris killed 27 people. Four miles south of Lone Pine, a small lake disappeared and the Owens River decreased in volume. The cloud of dust that rose over the disaster could be seen from 20 miles away. Witnesses reported that every few minutes heavy shocks of a few seconds duration occurred. From 2:30 to 6:30 a.m. there were not less than 50 distinct shocks and the earth seemed to vibrate all the time. The first tremor cracked and threw down many walls and buildings, but the succeeding aftershocks leveled the town. At Big Pine, 43 miles to the north, the tectonic violence injured many and tore the land apart. A large fissure opened from 50 to 200 feet wide and 20 feet deep, running close along the base of the Sierra Nevada. Along several sections of the road the earth was thrown up five to 10 feet, and in many places water was forced out of the barren ground. Springs failed that were never known to be dry before. Several people saw flashes of fire from the mountainsides at points between Bishops Creek and Independence. (Quake lights are believed to be masses of charged plasma, a high-temperature ionized gas composed of electrons and positive ions, which is theorized to form when earthquakes generate electrical charges that escape through rock layers and into the air.) Rockslides blocked the road with boulders as big as a two-story house. When the stagecoach finally arrived the exhausted driver gasped, there was not a brick or adobe or chimney left standing between Bishops Creek and Independence. The great earthquake, estimated at magnitude 8.3 on the Richter scale, was felt from Winnemucca, Nev., to Oakland, Calif. and all points in between. The jolt was severe enough to stop clocks in Truckee, Blue Canyon and all along the Sierra west slope. In Sacramento where the shaking lasted for a minute and a half, buildings rocked alarmingly and panicked residents poured into the streets in fear. At the Sacramento County Jail, prisoners begged and prayed with tears in their eyes to the jailer in charge to let them out. Their pleas were ignored. Hard rock miners working the night shift far below in the dark shafts beneath Virginia City claimed the sensations in the bowels of the Earth were very disagreeable and they would infinitely prefer to being on the surface during earthquakes a typical Comstock understatement.The dramatic 1872 Lone Pine earthquake represents powerful geologic forces that can literally move mountains. Vertical displacement was measured at nearly 17 feet. It left no doubt in the minds of California and Nevada residents their shared mountain range could still grow in leaps and bounds.Mark McLaughlin’s column, “Weather Window,” appears every other week in the Sierra Sun. He is a nationally published writer and photographer whose award-winning books, “The Donner Party: Weathering the Storm,” “Sierra Stories: True Tales of Tahoe, Vol. 1 andamp; 2,” and “Western Train Adventures: The Good, the Bad andamp; the Ugly” are available at local stores. Mark, a Carnelian Bay resident, can be reached at mark@thestormking.com