The major fracture in the earth’s crust extends northwestward through southern and northern California for roughly 810 miles. According to the theory of plate tectonics, the San Andreas forms the tectonic boundary between the Pacific Plate and the North American Plate. Geologists describe the fault as right-lateral strike-slip, which means that the Pacific side of the fault is slowly moving horizontally northward, usually by an inch or two per year. Such movements deep in the earth produces earthquakes-and such movements along the San Andreas Fault have produced most of the largest earthquakes in American
The Rise of Earthquakes in Oklahoma
With earthquakes on the rise, we must figure out the cause of them and determine a solution to help limit or even prevent them from occurring. Since early 2009, earthquakes have been sweeping across the state of Oklahoma, causing many people to worry about their own well-being. Many scientists speculate the source of the earthquakes might be a result of Hydraulic Fracturing deep down in Earths’ crust. Hydraulic fracturing is a process in which oil and natural gas companies pump up to millions of gallons of wastewater, sand, and chemicals down drilled holes in order to release pockets of shale within the earth. This use of technology is in question of the potential cause or inducement of earthquakes in Oklahoma.
More profoundly people tabulated the first earthquake as: "it hurled my bed against an opposite wall," wrote Emma Burke, the wife of a local attorney. "It grew constantly worse, the noise deafening; the crash of dishes, falling pictures, the rattle of the flat tin roof, bookcases being overturned, the piano hurled across the parlor, the groaning and straining of the building itself, broken glass and falling plaster, made such a roar that no one noise could be distinguished."1 The first seismic shock also resulted in wooden houses being severely damaged, and decrepit brick buildings felled to the ground. The earthquake impacted the San Andreas Fault engendering buildings to crumble into pieces such as hotels. Hotels that were impacted included the Valencia Street Hotel.The powerful earthquake annihilated ...
...ncisco Earthquake, 1906." National Archives and Records Administration. National Archives and Records Administration, n.d. Web. 09 May 2014.
The science of the natural disaster has baffled many, but from studying the San Francisco earthquake, scientists have made a number of important discoveries and they have a better understanding of earthquakes. At 5:12 on a fateful April morning in 1906, the mammoth Pacific and North American plates sheared at an incredible twenty-one feet along the San Andreas fault, surpassing the annual average of two inches (“San Francisco Earthquake of 1906”)(“The Great 1906 Earthquake and Fires”). The shearing caused a loud rumble in the Californian city of San Francisco. A few seconds later, the destructive earthquake occurred. The ground shifted at almost five feet per second, and the shaking could be felt all the way from southern Oregon to southern Los Angeles to central Nevada (“Quick”)(“The Great 1906 San Francisco Earthquake”). Moreover, the earthquake could be recorded on a seismograph in Capetown, South Africa, an astounding 10,236 miles away from San Francisco (“San Francisco ea...
benchmark for the future, and integrated investigation into the effects of earthquakes in the U.S.
Dry weather combined with many wooden buildings, sidewalks and streets were open to catching fire and eventually led to it happening (Chicago Fire, 1). The fire spread uncontrollably to the northeast and central of the city. The downtown and north of Chicago was taken in flames but the stockyards on the south and west were not touched by the fire (Fire of 1871, 2). 17,500 buildings have been destroyed, a total of 78 miles of pavements were covered in flames (Murphy, 100). That night the wind was at 30 miles per hour, but there were many whirl flames that traveled to and across the city (Great Chicago Fire, 2). Amid the day and age of the fire the populace was assessed roughly around 324,000 individuals. Inside nine years after the decimation the populace was 500,000 (Chicago Fire, 2). Before the tragic event of the fire, the summer of 1871 was extremely hot, and Chicago went threw a horrific drought. From July to the day of the fire there was only three inches of rainfall in Chicago. In fact, one night before the great downfall a different fire began that was battled out by all fire companies to compose it. Many residents felt that Chicago was saved from disaster after putting the fire to rest (The Great Fire, 2). There was a myth that mention that the fire started by a cow tipping over a lantern
Before examining the Northridge event, understanding the naturally occurring hazard that is an earthquake will help to better understand exactly what happened and why it was such an important geological event. With four distinct layers, two layers, the crust and upper portion of the mantle, compose the skin that is the surface layer of the Earth. The crust is not a single, continuous piece. It is actually several different pieces, or plates, that come together to form the puzzle that comprises the surface of the Earth. These plates are in constant motion rubbing against one another. These areas, known as fault lines, where the plates rub up against one another have spots where one plate ”gets stuck while the rest of the plate keeps moving. When the plate has moved far enough, the edges unstick and is how most of the earthquakes around the world occur” (Wald, 2012). The energy stored from the friction of the two plate...
From studying the science behind the San Francisco earthquake, scientists have made a number of important discoveries involving how earthquakes function. At 5:12 on a fateful April morning in 1906, the mammoth Pacific and North American plates sheared each other at an incredible twenty-one feet along the San Andreas fault, surpassing the annual average of two inches (“San Francisco Earthquake of 1906”) (“The Great 1906 Earthquake and Fires”). A few seconds later, the destructive earthquake occurred. The ground shifted at almost five feet per second, and the shaking could be felt all the way from southern Oregon to southern Los Angeles to central Nevada (“Quick”) (“The Great 1906 San Francisco Earthquake”). In fact, the earthquake could be registered in a seismograph on Capetown, South Africa, an astounding 10,236 miles away...
Geological and Dispositional History of the Starved Rocks, Illinois
Describe the clastic and carbonate facies you have discovered.
Starved Rock State covers about 200 miles and some 470 million years, from Ordovician sandstones to Pleistocene glacial till. The Ordovician St. Peter Formation sandstone was deposited across the midcontinent during the second major marine transgression of the Paleozoic Era. The first transgression deposited Upper Cambrian to Lower Ordovician clastics and carbonates. The clastic to carbonate rock transition is consistent with gradual sea level rise over the North American craton.