Understanding the Geological Cycle and Its Impact on Landforms

Geological Cycle: Processing fee of construction and destruction of land relief. Relief: The arc of volcanoes and surface forms of internal and external actors involved. Internal: Through volcanic activity and plate tectonics, the rise and land subsidence occur. External: Generates initial relief; actuates the living climate and water wear away the upper part of the relief, depositing in low areas. In the relief action, it becomes destructive. Great Plains act on the land filled with the inner forces. Volcanic Activity: SLG materials inside the Earth are forced to come to the surface or cracks. This occurs through an increase in the cap of the lithosphere, causing the melting of rocks. Subduction Zone: Friction between tectonic plates produces heat, causing lithospheric material to melt and produce magma. Abduction: Heat tries to push magma to the surface. Therefore, volcanoes like those on Easter Island are formed. Hot Spots: The material comes from deep layers of the mantle, causing fast drilling in the lithosphere. Volcanoes: Mountains produced by the accumulation of material from the land into the magma chamber, where there is an accumulation of melt. The crater is located in the upper part of the volcano. Hawaiian Volcanoes: They are rounded at the tip; tranquil lava eruptions occur when the lava is very liquid. Volcanic Cones: These are conical, explosive, and have viscous lava eruptions, often accompanied by enclosed gases. Volcanic Fights: Dense material rises slowly and solidifies as it ascends.

Lava: Rock of volcanic origin produced by large accumulations of lava that solidify, obstructing the circulation of surface water. Lava Tables: Plains generated by rocky lava flows; if the material is resistant, rocks give rise to a flat area. Boilers: Large cavities caused by the explosion of a volcano. Hot Springs: They form the relief, carrying minerals from the land within, deposited on the surface. Tectonic Plates: The movement can cause two types of faults and folds transformations. Faults: Fractures in the crust accompanied by a shift from the position of faults and the displacement of: Normal or Locked-Direct: is inclined in the direction Straddling: sunk. Locked: one is mounted on another. Reverse: is inclined towards high. Tearing: Locked: horizontal scroll or deviation. Folds: Caused by surface undulations from lateral compression forces. The concave part is called the syncline, and the convex part is called the anticline. Inclined: Sides = inclined axial plane, and the sides are different. Lying or Lying: Horizontal or near axial plane.
Formation of the Andes: Palca Asian / plate indicates / subduction / sediments. - Folding of the sediments accumulated in the formation of the basin. - Elevation of the Himalayan mountain.