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Endogenic processes
Processes that occur beneath the surface of the Earth.
Magma
A mixture of molten rock, minerals, and gases that is formed beneath the Earth's surface.
Asthenosphere
The layer below the lithosphere where rocks can flow like a liquid due to high pressure and heat.
Lithosphere
The outermost layer of the Earth, consisting of the continental crust and oceanic crust.
Formation of Magma
The process by which magma is formed, which can occur through temperature increase, pressure decrease, or the addition of fluids.
Gases in Magma
Dissolved gases in magma that form separate vapor phases as pressure decreases.
Volcano
A vent in the Earth's crust through which magma, gases, and other materials are ejected.
Viscosity of Magmas
The resistance to flow of magma, which depends on its composition and temperature.
Magma escape routes
The ways in which magma can leave the asthenosphere and crust, either through intrusion or extrusion.
Lava
Magma that has extruded onto the Earth's surface.
Tephra
Solidified magma in the air, also known as volcanic ash.
Pyroclastic rock
Rock formed from the accumulation of tephra on the Earth's surface.
Crust
The outermost layer of the Earth's surface.
Magma chamber
A reservoir of molten rock beneath the Earth's surface.
Decompression melting
The process of melting rock due to a decrease in pressure.
Ridge
A long, narrow elevated landform formed by tectonic activity.
Upwelling
The upward movement of hot material in the Earth's mantle.
Lithosphere
The rigid outer layer of the Earth, including the crust and upper mantle.
Asthenosphere
The partially molten layer of the Earth's mantle beneath the lithosphere.
Flux melting
Melting of rocks due to the addition of water or carbon dioxide.
Felsic magma
Magma with high silica content, high gas content, and high viscosity.
Intermediate magma
Magma with higher silica content than mafic magma, resulting in higher gas content and viscosity.
Mafic magma
Magma with low silica content, high iron and magnesium content, low gas content, and low viscosity.
Ultramafic magma
Magma with very low silica content, high iron and magnesium content, and high temperature.
Stress
The force that can cause deformation in rocks.
Lithostatic stress
Equal pressure exerted on rocks from all directions due to the weight of overlying rocks.
Differential stress
Unequal stress experienced by rocks due to tectonic forces.
Tension stress
Stress that stretches or pulls rocks apart.
Compressional stress
Stress that presses, squeezes, or pushes rocks together.
Shear stress
Stress that results in slippage and translation of rocks.
Strain
The change in shape or deformation of rocks in response to stress.
Elastic deformation
Reversible deformation of rocks in response to small differential stresses.
Brittle deformation
Irreversible deformation of rocks resulting in fracture.
Faults
Large cracks or breaks in rocks caused by tectonic forces.
Dip-Slip (Normal Fault)
A type of fault where brittle rocks are stretched and tectonic tensional forces are involved, causing the movement of blocks of rock mainly in the vertical direction.
Hanging Wall
The block lying on the top of a dip-slip fault surface.
Footwall
The block lying below the dip-slip fault surface.
Strike-Slip Fault
A type of fault where brittle rocks are sheared and the movement of blocks of rock is chiefly in the horizontal direction.
Ductile Deformation
The behavior of rocks buried deep within the Earth's crust when subjected to differential stress, causing them to become thicker under compressional stress and thinner under tensional stress.
Folds
Structures formed when rocks deform in a ductile manner, bending or folding instead of fracturing to form faults or joints.
Monoclines
The simplest type of folds where horizontal layers are bent upwards, resulting in two horizontal limbs of the fold.
Synclines
Fold structures where the original rock layers have been folded downward and the two limbs of the fold dip inward toward the hinge of the fold.
Anticlines
Fold structures formed when the originally rock layers have been folded upward and the two limbs of the fold dip away from the hinge of the fold.
Endogenic Processes
Internal processes that occur beneath the surface of the Earth.
Magma
A mixture of molten rock, minerals, and gases.
Felsic Magma
Magma with a high silica content.
Intermediate Magma
Magma with a moderate silica content.
Mafic Magma
Magma with a low silica content.
Ultramafic Magma
Magma with a very low silica content.
Viscosity
The resistance to flow of a substance, in this case, magma.
Universe
All existing matter and space considered as a whole.
Big Bang Model of Universe
Proposed by Georges Henri Joseph Edouard Lemaitre, it describes the universe as originating from an infinitely tiny, dense point or singularity.
Inflationary Epoch
The period of rapid expansion of the universe, occurring between 10^-35 seconds and 10^-33 seconds after the Big Bang.
Formation of Universe
The process in which gravity and strong nuclear force led to the formation of fundamental particles and energy, such as quarks, electrons, protons, and neutrinos.
Formation of Basic Elements
The process of nucleosynthesis, where protons and neutrons combine to form hydrogen nuclei, which then combine to form helium nuclei.
Radiation Era
A period of 10,000 years after the Big Bang when most of the energy in the universe was in the form of radiation, including light, x-rays, radio waves, and UV rays.
Matter Domination
The period of 300,000 years after the Big Bang when matter began to dominate, leading to the formation of neutral atoms and the birth of stars and galaxies.
Solar System Model
A representation used to describe and explain the phenomena of the solar system, including the understanding of its origin and structure.
Geocentric Model
A model of the solar system proposed by Claudius Ptolemy, where the Earth is believed to be the center.
Heliocentric Model
A model of the solar system proposed by Nicholas Copernicus, where the Sun is believed to be the center.
Angular Momentum
The quantity of rotation of a body, determined by its moment of inertia and angular velocity.
Nebular Hypothesis
A theory proposed by Immanuel Kant and Pierre-Simon Laplace, suggesting that the solar system originated from a cloud of interstellar gas called a nebula.
Terrestrial Planets
The rocky planets in the solar system, including Mercury, Venus, Earth, and Mars.
Jovian Planets
The gaseous planets in the solar system, including Jupiter, Saturn, Uranus, and Neptune.
Protoplanet
A whirlpool of gas within a rotating mass of a nebula, believed to be the precursor to the formation of planets.
Gravity
The force that describes how planets move as they orbit the Sun.
Composition Layer
The layers of the Earth based on their composition, including the crust, mantle, and core.
Mechanical Layer
The layers of the Earth based on their mechanical properties, including the lithosphere, asthenosphere, mesosphere, and inner/outer core.
Lithosphere
The outermost layer of the Earth's composition layer, consisting of large rocks and divided into oceanic and continental crust.
Mantle
The solid rocks and minerals layer of the Earth's composition layer, making up 85% of the planet's mass.
Core
The metal alloy layer of the Earth's composition layer, consisting of the inner and outer core and responsible for the planet's magnetic fields.
Seismic Waves
Waves caused by the breaking down of rocks or explosions, used to study the Earth's interior structure.
Earth's Subsystems
The four subsystems of the Earth, including the lithosphere, hydrosphere, atmosphere, and biosphere.
Pangea
The supercontinent proposed by Alfred Wegener, suggesting that all continents were once connected.
Hydrospere
The water near the Earth's surface, including liquid, vapor, and ice.
Atmosphere
The layer of air or gas surrounding the Earth.
Biosphere
The zone of life on Earth, where living organisms exist.
Ocean Zones
The different layers or zones in the Earth's oceans, including coastal, pelagic, neritic, and oceanic zones.
Vertical Zone
The zone that begins at sea level and ends at the deepest point in the ocean, consisting of 5 different zones with varying sunlight.
Atmosphere
The thin layer of gas surrounding the Earth.
Green House Gases
Gases that help maintain the Earth's temperature at a level conducive to life.
Troposphere
The lowest layer of the atmosphere that is visible to us.
Stratosphere
The layer of the atmosphere that contains the ozone layer.
Mesosphere
The coldest region of the atmosphere, including the upper mesosphere where meteors are found.
Thermosphere
The hottest region of the atmosphere.
Epipelagic
Also known as the "Sunlight zone," this zone extends from 0-200m in the ocean and receives a lot of sunlight. It is inhabited by sharks.
Mesopelagic
Also known as the "Twilight zone," this zone extends from 200-1000m in the ocean and has limited sunlight. It is inhabited by octopuses.
Bathypelagic
Also known as the "Midnight zone," this zone extends from 1000-4000m in the ocean and has no sunlight. It is inhabited by animals that lack eyes, such as the stripe eel.
Abyssopelagic
Also known as the "abyss" or "Deep sea," this zone extends from 4000-6000m in the ocean and is characterized by blind shrimps and other invertebrates.
Hadalpelagic
Also known as the "Trenches," this zone extends from 6000m to the bottom of the ocean and is the deepest part. It is characterized by trenches, canyons, and sea cucumbers.
Exosphere
The upper limit of the atmosphere.
Biosphere
The "zone of life" on Earth, encompassing all living things.
Biomes
The world's major communities, divided into different types such as aquatic, forests, desert, and tundra.
Transpiration
The process of releasing water in plants.
Tropical Rainforests
A type of forest biome with four different layers:emergent, canopy, middle (understory), and bottom (forest floor).
Temperature Deciduous Forest
A type of forest biome that experiences changing seasons.
Taiga Forest
Also known as the "boreal forest," it is the largest and thickest biome, characterized by cone-bearing evergreen trees.
Desert
A biome with low rainfall and high temperatures.
Universe
All existing matter and space considered as a whole.
Big Bang Model of Universe
Proposed by Georges Henri Joseph Edouard Lemaitre, it describes the universe as originating from an infinitely tiny, dense point or singularity.