Earth`s crust, the surface layer of the planet, is
... response to pressure underground. One block may move up while the other moves down. Sometimes the movement is enough to form valleys or mountains. Other times that movement is not vertical but horizontal, as one block slips along the fault relative to the block on the other side. Movement of crustal ...
... response to pressure underground. One block may move up while the other moves down. Sometimes the movement is enough to form valleys or mountains. Other times that movement is not vertical but horizontal, as one block slips along the fault relative to the block on the other side. Movement of crustal ...
Mountain Building
... gravitational balance (Isostatic Adjustment.) • This can cause uplift in the crust. ...
... gravitational balance (Isostatic Adjustment.) • This can cause uplift in the crust. ...
Rocks Get Stressed
... occurs when tectonic forces cause tension that pulls rocks apart. • Reverse Fault - causes the hanging wall to move up relative to the footwall. This occurs when tectonic forces cause compression that pushes rocks together. ...
... occurs when tectonic forces cause tension that pulls rocks apart. • Reverse Fault - causes the hanging wall to move up relative to the footwall. This occurs when tectonic forces cause compression that pushes rocks together. ...
Chapter 4 lesson 1
... Two normal faults cause the hanging walls to fall downward creating valleys. The block in between now stands higher, creating fault-block mountains. Forces in Earth’s crust can also push up large, flat blocks of rock. Plateau- A large landform that has a high elevation and a more or less flat ...
... Two normal faults cause the hanging walls to fall downward creating valleys. The block in between now stands higher, creating fault-block mountains. Forces in Earth’s crust can also push up large, flat blocks of rock. Plateau- A large landform that has a high elevation and a more or less flat ...
Date: Block
... 3. Strike-Slip Fault: form when opposing forces cause rock to break and move horizontally. IV. Plate Tectonics and Mountain Building A. Folded Mountains: form when rock layers are squeezed together and pushed upward. They form at convergent boundaries. B. Fault-Block Mountains: form when this tensi ...
... 3. Strike-Slip Fault: form when opposing forces cause rock to break and move horizontally. IV. Plate Tectonics and Mountain Building A. Folded Mountains: form when rock layers are squeezed together and pushed upward. They form at convergent boundaries. B. Fault-Block Mountains: form when this tensi ...
File - Wildcat Earth Science
... Rock above the normal fault line is called the hanging wall and the rock below the normal fault line is called the foot wall. Occurs along divergent boundaries because of tension stress. ...
... Rock above the normal fault line is called the hanging wall and the rock below the normal fault line is called the foot wall. Occurs along divergent boundaries because of tension stress. ...
Chap7Sect4 - Cobb Learning
... New 7.4 Tech Terms: 1. deformation – the change in the shape of rock in response to stress. 2. stress – a force that acts on rock to change its shape or volume. ...
... New 7.4 Tech Terms: 1. deformation – the change in the shape of rock in response to stress. 2. stress – a force that acts on rock to change its shape or volume. ...
Geology_101_Homework_2
... 2) What is the difference between ductile and brittle behavior for rocks? 3) There are two important brittle-ductile transitions in the upper 600 km of the Earth. In what layers or between which layers are they located? 4) Draw pictures of normal, reverse, and strike-slip faults using arrows to show ...
... 2) What is the difference between ductile and brittle behavior for rocks? 3) There are two important brittle-ductile transitions in the upper 600 km of the Earth. In what layers or between which layers are they located? 4) Draw pictures of normal, reverse, and strike-slip faults using arrows to show ...
Inside Earth Ch. 2 Sec. 1 Notes
... Stress: A force that acts on rocks to change its shape or volume -Stress adds energy to rock -Energy is stored until rock changes shape or breaks 3 Types of Stress 1. Tension -Pulls on the crust stretching it so it is thinner in the middle -Occurs where plates move apart 2. Compression -Squeezes roc ...
... Stress: A force that acts on rocks to change its shape or volume -Stress adds energy to rock -Energy is stored until rock changes shape or breaks 3 Types of Stress 1. Tension -Pulls on the crust stretching it so it is thinner in the middle -Occurs where plates move apart 2. Compression -Squeezes roc ...
Metamorphic Fabric Solid-state Crystal Growth Nucleation
... • Migration facilitated by an intergranular fluid • Driving mechanism is a chemical potential • Evidenced by growth into pressure shadows ...
... • Migration facilitated by an intergranular fluid • Driving mechanism is a chemical potential • Evidenced by growth into pressure shadows ...
Earthquakes - collazocove
... 1. They form when plates move apart. 2. It depends how far the plates move apart to how powerful the earthquake will be. ...
... 1. They form when plates move apart. 2. It depends how far the plates move apart to how powerful the earthquake will be. ...
Unit 1.4 Earthquakes
... • Stress: Force that acts on rock to change its shape or volume • Fault: When enough stress builds up and rock breaks • Tension: Stress force that pulls on Earth’s crust causing rock to stretch in the middle • Compression: Stress force that squeezes rock until it folds or breaks • Epicenter: The poi ...
... • Stress: Force that acts on rock to change its shape or volume • Fault: When enough stress builds up and rock breaks • Tension: Stress force that pulls on Earth’s crust causing rock to stretch in the middle • Compression: Stress force that squeezes rock until it folds or breaks • Epicenter: The poi ...
What is isostasy? The balancing downward force of the crust and the
... How do rift valley’s form? ...
... How do rift valley’s form? ...
Current Tectonic Stress Field in the Northeastern Margin of Tibetan
... Xianrui Li, Zuoxun Zeng, and Qingqin Dai School of Earth sciences, China University of Geosciences, Wuhan, China ...
... Xianrui Li, Zuoxun Zeng, and Qingqin Dai School of Earth sciences, China University of Geosciences, Wuhan, China ...
