Any process that includes geological phenomena and processes originating externally to the Earth's surface, driven by solar energy and other external influences
Weathering
The gradual on-site breakdown of rocks into sediments caused by many factors
Mechanical weathering
The physical breakdown of rock into unconnected grains and/or chunks without any chemical alteration
Mechanicalweathering processes
Exfoliation
Thermal expansion
Wedging
Erosion
The separation of weathered and unweathered materials from its substrate due to gravity or agents of transportation
Winderosion
Erosion where sediments and loose soil are carried by the wind to new locations, resulting in soil loss, soil dryness, soil structure deterioration, soil nutrient and productivity losses, and air pollution
Glacial erosion
Erosion caused by glacier movement, where rocks and ice being carried by glaciers weather against other stones on the Earth's surface
Ways water/tidal erosion moves sediments
Traction
Saltation
Suspension
Solution
Mass wasting
The downslope movement of rocks, soil, and ice due to the pull of gravity
Factors contributing to mass wasting
Relief
Fragmentation and weathering
Unbalanced forces that disrupt the equilibrium between downslope and resistance forces in masswasting
Tectonic vibrations/earthquakes
Changes in the structure of the slope
Material composition
General motion types in mass wasting
Fall
Topple
Slide
Spread
Flow
Complex
Deposition
The process where sediments settle out of the transporting medium, usually associated with water
Types of deposition areas
Glacial
Mountainous
Desert
Lacustrine
Fluvial
Deposition
The process where sediments settle out of the transporting medium, usually associated with water [Lat. de- ("away") + ponere ("to put, place"), "place elsewhere"]
Bed
The layer formed when sediments settle in a new area
Sorting
The distribution of grains in a bed
Lacustrine
Adjective used to associate something with lakes
Lakes are still water forms due to a lack of underwater currents
Coarse sediments carried by connected tributaries are deposited on a lake's margin
Silt and clay are deposited from suspension in the deeper parts
Fluvial
In areas of low elevations where rivers are present
The velocity of water is slow and commonly carries an assortment of sediments
Coarser sediments tumble along the river bed
Finer sediments flow in suspension with the water
Delta
Areas where accumulated sediments that have been compacted and lithified at the river's end is connected to a stagnant body of water
When rivers enter the stagnant water form, it empties its sediment load into a delta
Beach
Areas containing fine sand and coarse sediments and rocks
Ocean waves and tidal currents transport sand into the coastlines, filtering and sorting out the sand to form ripples at the coastlines
Marine
Areas where saltwater is dominant and activity is observed on both surface and deep levels
Includes shallow marine, shallow water (carbonate), and deep
Endogenic processes
Any process that includes geological phenomena and processes originating within the Earth's surface
Responsible for tectonic changes on the surface by releasing energy from within
Attributed to the leftover heat within the planet's crust during its accretion 4.54 billion years ago
Heat comes from gravitational energy and disintegration of radioactive elements buried deep within the Earth
Magma
Rocks in liquid to semi-liquid form, less dense than actual stones, found in specific locations on Earth
Generation of Magma
1. Decompression Melting
2. Flux Melting
3. Heat Transfer Melting
4. Partial Melting
Crystallization of Magma
Rocks that have been extruded to the surface solidify, recrystallizing to a solid form and forming grains
Crystallization can also occur underground if the temperature permits it, creating igneous rocks
Common Minerals
Quartz
Orthoclase
Plagioclase
Muscovite
Biotite
Amphibole
Pyroxene
Olivine
Dikes
Intrusions that form wall-like sheets
Sills
Intrusions that form tabularlayers in between pre-existing rock layers
Plutons
Intrusions with the blob-like appearance and form many configurations
Amalgamations of plutons are known as batholiths
Felsicrocks
Rocks with higher silica content, as compared to its magnesia and wustite contents
Maficrocks
Rocks with substantially higher magnesia and wustite contents than silica
Ultramaficrocks
Rocks made with different kinds of mafic rocks, ensuring that the silica content is low
Intermediate rocks
Combinations of felsic, mafic, and ultramafic rocks
Volcanism
Geological activity involving volcanoes, which are visible vents—manifestations of rock formation
Types of Eruption
Effusive eruptions (dominant lava flow and formation of fountains and lakes)
Explosive eruptions (eject other materials aside from lava, ranging from ash to large pyroclastics)
Shieldvolcanoes
Form very broad domes with gentle slopes that cover a wide area, mostly made of alternating layers of basaltic lava and cinder accumulation
Stratovolcanoes or composite volcanoes
Made of alternating layers of lava and pyroclastics, generally made of felsic to intermediate rocks, building tall edifices
Cindercones
Consist of small cones formed by lava spattering, usually made of cinders with mafic compositions
Metamorphism
The process where the original rocks (called protoliths) undergo both mineralogical and textural changes due to modifications in its physical and/or chemical environments, altering it without changing its composition through melting or disintegration