![]() ![]() EaseUS MobiMover Free helps to manage your iPhone content with simple steps so that you can transfer, add, delete and edit the items on your iPhone/iPad easily and freely. More comprehensive and smarter than you think.ĮaseUS MobiMover supports backup iPhone contents regularly and restores them to your new iPhone or another device when needed. EaseUS MobiMover Free is a robust iOS data transfer and management tool that helps to access your iPhone, iPad, or iPod data from a computer and transfer data from one iDevice to another, which replaces iTunes perfectly.īesides, it is a free video and audio downloader to download videos & audio files from more than 1000 sites, and fully supports WhatsApp messages backup, restore, and transfer. Whether you want to transfer all supported files at once or copy items selectively, it will help.ĮaseUS MobiMover Free is the best free iPhone data transfer software which moves your mobile data between iPhones, or from iPhone to iPhone. Besides, you are able to transfer data from one iOS device to another using this tool. With it, you can not only transfer files from your iPhone to a PC but also add contents to your iPhone from a computer. The height of their seismic activity in one game came during a touchdown run.Ĭorrection: The original story misplaced the focal center of the earthquake, which was 10 miles underneath the surface of the Pacific Ocean.As professional iOS data transfer software, one of the main features of EaseUS MobiMover is to transfer files between iPhone and computer, be it a PC or Mac. Temblors can be triggered by pumping wastewater onto faults in deep disposal wells, as seen in quakes that occurred in Oklahoma, Texas, and Ohio in recent years.Īnd Seattle Seahawks football fans have gained their own notoriety during a NFL Superbowl-winning playoff run this year, triggering " Beast Quakes" detected by seismologists across the Pacific Northwest. But humanity has figured out ways to trigger small quakes as well. It really takes the movement of crustal plates to uncork a massive earthquake, such as the magnitude 9.0 quake off the coast of Japan in 2011, which was caused by the Pacific plate moving under Asia. The Santa Clara Valley south of San Francisco holds a fault prone to oblique motions, for example, seen in a 1999 quake. Obliqueįaults that combine sideways with up-and-down motions are called oblique by seismologists. Geological Survey sees the fault as posing a risk of more magnitude 7.0 earthquakes. ![]() One magnitude 7.0 quake along the fault perhaps 550 years ago dropped the ground on one side of the fault by three feet (a meter). ![]() A reverse is, well, just the reverse.Īn example of a normal fault is the 150-mile-long (240-kilometer-long) Wasatch Fault underlying parts of Utah and Idaho, again caused by the Pacific plate driving under western North America. A normal fault occurs where the deeper part of the crust is pulling away from an overlying part. Up-and-down motions in earthquakes occur over so-called " dip-slip" faults, where the ground above the fault zone either drops (a normal fault) or is pushed up (a reverse fault). The sideways motion of the fault's branches is caused by the Pacific Ocean's crustal plate moving to the northwest under North America's continental crust. The most famous example is California's San Andreas Fault, which stretches some 600 miles (1,000 kilometers) from southern California to north of San Francisco. When portions of the Earth's crust moves sideways, the result is a horizontal motion along a "strike-slip" fault. Here are a list of the various ways Earth can shake. California, United States has had: (M1. The ground first bends and then snaps-an earthquake-to release energy along faults. ![]() Most earthquakes arise along such fault zones. Maps of recent earthquakes and ShakeMaps of the intensity of earthquake shaking are available from California Integrated Seismic Network. Along the Ring of Fire girding the Pacific Ocean, for example, the seafloor plunges beneath Asia and the Americas, building mountains, feeding volcanoes, and triggering earthquakes. The Earth's crust is made of a jigsaw puzzle of continental and oceanic plates that are constantly ramming each other, sliding past each other, or pulling apart. Learn about the geophysics behind earthquakes, how they are measured, and where the most powerful earthquake ever witnessed occurred. Earthquakes can leave behind incredible devastation, while also creating some of the planet's most magnificent formations. ![]()
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