Any process that includes geological phenomena and processes originating within the Earth's surface
Endogenic Processes
Responsible for any tectonic changes on the surface by releasing energy from within
Attributed to the leftover heat (measure to be at least 5000°–7000°C) within the planet's crust during its accretion 4.54 billion years ago
Gravitational energy
Built up over the years during the accretion period up to the point that the theoretical planet "Theia" crashed onto the juvenile Earth, creating the Moon
Radioactive elements
Disintegration of uranium-238, thorium-232, and potassium-40 buried deep within the Earth
Magma
Rocks in liquid to semi-liquid form, less dense than actual stones, found in specific locations on Earth
Magma
Primarily composed of silicon dioxide, aluminum oxide, calcium oxide, magnesium oxide, iron oxide, and H2O, along with dissolved gases such as water vapor and carbon dioxide
Temperature ranges from 800°–1400°C
Lava
Flowing magma seen on the Earth's surface
Viscosity of magma
Generally depends on its silica content, gas content and temperature
Decompression Melting
A method of melting where the temperature is constant throughout while the pressure decreases
Flux Melting
A form of melting where volatiles (i.e. gaseous substances) are added into the magma
Heat Transfer Melting
A method of melting rocks with the introduction of pre-existing magma
Partial Melting
A method of melting rocks where certain minerals are dissolved once its eutectic temperatures are met
Crystallization of Magma
Rocks that have been extruded to the surface solidifies, recrystallizing to a solid form and forming grains
Common Minerals
Quartz
Orthoclase
Plagioclase
Muscovite
Biotite
Amphibole
Pyroxene
Olivine
Feldspar
Includes plagioclase and orthoclase
Mica
Includes biotite and muscovite
Igneous rocks
Classified based on the distribution of silica, magnesia, and wustite, and grain size that dictates the rocks' textures
Igneous intrusions
Magma that never reaches the surface, including dikes, sills, and plutons
Bowen's reaction series
Crystallization sequence of minerals formed as magma cools
Felsic rocks
Rocks with higher silica content, as compared to its magnesia and wustite contents
Mafic rocks
Rocks with substantially higher magnesia and wustite contents than silica
Ultramafic rocks
Rocks made with different kinds of mafic rocks, ensuring that the silica content is very low compared to the two
Intermediate rocks
Combinations of felsic, mafic, and ultramafic rocks
Volcanism
Geological activity involving volcanoes, which are visible vents—manifestations of rock formation
Volcanoes
Serve as the conduit for lava or molten rock within the Earth's surface
Lava exits through a funnel-shaped opening known as a crater
Effusive eruptions
Eruptions with dominant lava flow and formation of fountains and lakes
Explosive eruptions
Eruptions that eject other materials aside from lava, which can range from ash to large pyroclastics
Shield volcanoes
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
Cinder cones
Consist of small cones formed by lava spattering, usually made of cinders with mafic compositions
Pahoehoe
Lava with smooth surfaces, often forming tubes
'A'ā
Lava with very coarse surfaces, appearing rubbly or broken rocks
Obsidian
A glassy material formed by rapidly cooling high-silica lava flow
Pumice
A high-silica lava material that has solidified into a rock, frothy and contains many air spaces inside it created by trapped gas bubbles
Pyroclastics
Fragmented materials (of varying grain sizes) released from a volcano
Lapilli
Pea- to marble-sized fragments of lava known to be a size classification of tephra
Volcanic ashes
Very fine particles consisting of glass shards, crystals, and fragments of existing rocks
Pyroclastic flow deposits
Aggregates of pyroclastic debris that flow on the slopes of volcanoes