PLATE TECTONICS Plate tectonics is the scientific theory that explains how the Earth’s outer shell is divided into large plates that move over the mantle. Their movements create earthquakes, build mountains, and form volcanoes, shaping the surface of our planet. Understanding plate tectonics helps us make sense of Earth’s past and prepare for natural hazards in the future. Follow Geomark Geoscience Education for more fascinating geological insights and discoveries. #Geology #EarthScience #PlateT
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THE GEOLOGICAL PROCESS OF MOUNTAIN RANGE FORMATION Mountain ranges are formed through complex geological processes, mainly driven by the movement and collision of tectonic plates. When two continental plates collide, immense pressure forces the Earth's crust to buckle and fold, pushing rocks upward and forming towering mountain belts. This process can take millions of years and often involves earthquakes, metamorphism, and volcanic activity. Such formations are key indicators of Earth's dynamic
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A transform boundary is a fault along a plate boundary where the motion between tectonic plates is predominantly horizontal. Unlike other boundaries, it ends abruptly where it connects to another type of plate boundary, such as another transform fault, a spreading ridge, or a subduction zone. These boundaries are often associated with intense seismic activity due to the friction and pressure that builds up as the plates slide past each other. Follow Geomark Seismics Survey and Drilling Services.
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