WebHowever, friction between the rocks prevents smooth motion along the fault plane. Instead, the rocks near the fault plane bend and store elastic energy. The elastic energy is released when the rock bodies suddenly move along the fault and the bending rocks straighten, which causes an earthquake. Arrange the diagrams below in chronological order. WebCompression is the force that squeezes rock together. Tension is the force that pulls rocks apart. Shearing is the force that causes rocks on either side of a fault to slide past each other. normal fault. caused by tensional forces, pulling rocks apart. rock above the fault moves downward in relation to rock below the fault.
Faults, Stresses & Movements Earth Sciences Quiz - Quizizz
WebFeb 4, 2024 · Compressional stress occurs when two blocks of rock move toward and push against one another, creating a reverse fault. A reverse fault is also a dip-slip fault that forms at a convergent boundary . WebJan 17, 2024 · There are different types of faults: reverse faults, strike-slip faults, oblique faults, and normal faults. In essence, faults are large cracks in the Earth's surface where parts of the crust move in relation to one another. The crack itself does not make it a fault, but rather the movement of the plates on either side is what designates it as ... hood canal cottages
Faults HowStuffWorks
WebLive. Shows. Explore WebApr 9, 2024 · letter box 255 views, 1 likes, 9 loves, 77 comments, 7 shares, Facebook Watch Videos from Oakland Avenue Missionary Baptist Church: Ways to give -Mail... Webfracture in crustal rock involving the displacement of rock on one side of the fracture with respect to the rock on the other side. Three types of tectonic stress that result in faulting (compression, tension, or lateral movement) Compression: push the crust together. Tension: pull the crust apart. Lateral movement: hood canal bridge openings