Exogenic & Endogenic ( galing sa rev ni ms )
Exogenic & Endogenic Quiz
Test your knowledge on exogenic and endogenic processes with our engaging quiz! This interactive experience will challenge your understanding of geological concepts, from the angle of repose to volcanic activities.
Prepare to explore:
- Earthquake causes
- Volcanic eruptions
- Chemical weathering
The steepest angle at which material remains stable
Angle of repose
Floodplain
Hydration
Hydrolysis
Oxbow Lake
Erosion
MASS WASTING
Flat, wide expanse of alluvium that covers flat areas which are prone to flooding
Angle of repose
Floodplain
Hydration
Hydrolysis
Oxbow Lake
Erosion
MASS WASTING
Chemical weathering occurs when water is absorbed into the crystal structure of the mineral, causing it to expand
Angle of repose
Floodplain
Hydration
Hydrolysis
Oxbow Lake
Erosion
MASS WASTING
Chemical weathering occurs when water reacts with minerals and breaks them down
Angle of repose
Floodplain
Hydration
Hydrolysis
Oxbow Lake
Erosion
MASS WASTING
A horse-shoe lake that forms as a river finds a different, shorter course
Angle of repose
Floodplain
Hydration
Hydrolysis
Oxbow Lake
Erosion
MASS WASTING
The separation and removal of weathered and unweathered rocks and soil from its substrate due to gravity of transporting agents.
Angle of repose
Floodplain
Hydration
Hydrolysis
Oxbow Lake
Erosion
MASS WASTING
The downslope movement of rock, regolith, and soil under the direct influence of gravity. It does not require a transporting medium.
Angle of repose
Floodplain
Hydration
Hydrolysis
Oxbow Lake
Erosion
MASS WASTING
Conical hill or mountain that has a crater or vent through which the lava and other fragments are being erupted from the Earth’s crust
Volcano
Dormant Volcano
Orogenic Process
Thermal energy and Gravitational Energy
Sudden movements
Diastrophism
Mount Pinatubo
Potentially Active Volcanoes
Volcano
Dormant Volcano
Orogenic Process
Thermal energy and Gravitational Energy
Sudden movements
Diastrophism
Mount Pinatubo
Tectonic and Volcanic Activities
A large circular depression formed by the collapse or explosion of the volcano
Volcano
Dormant Volcano
Orogenic Process
Thermal energy and Gravitational Energy
Sudden movements
Diastrophism
Mount Pinatubo
Caldera
Tectonic and Volcanic Activities
Cause of Earthquakes
Volcano
Dormant Volcano
Orogenic Process
Thermal energy and Gravitational Energy
Sudden movements
Diastrophism
Mount Pinatubo
Caldera
Tectonic and Volcanic Activities
Also known as Mountain building.
Volcano
Dormant Volcano
Orogenic Process
Thermal energy and Gravitational Energy
Sudden movements
Diastrophism
Mount Pinatubo
Caldera
Tectonic and Volcanic Activities
forces behind endogenic movements
Volcano
Dormant Volcano
Orogenic Process
Thermal energy and Gravitational Energy
Sudden movements
Diastrophism
Mount Pinatubo
Caldera
Tectonic and Volcanic Activities
Movements that occur in a very short period of time
Volcano
Dormant Volcano
Orogenic Process
Thermal energy and Gravitational Energy
Sudden movements
Diastrophism
Mount Pinatubo
Caldera
Tectonic and Volcanic Activities
Iit is the direct opposite of sudden movements
Volcano
Dormant Volcano
Orogenic Process
Thermal energy and Gravitational Energy
Sudden movements
Diastrophism
Mount Pinatubo
Caldera
Tectonic and Volcanic Activities
June 15, 1991 - 800 people were killed and 100,000 became homeless. The global temperature also decreased by 0.5C
Volcano
Dormant Volcano
Orogenic Process
Thermal energy and Gravitational Energy
Sudden movements
Diastrophism
Mount Pinatubo
Caldera
Tectonic and Volcanic Activities
Bulkan Taal
Volcanoes doesn't erupt when the magma rises to the surface
True
False
Magma contains volatiles such as water and air
True
False
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