Core, Mantle, and Crust are divisions based on composition
Core
Mostly iron metal
Mantle
Hot and represents about 68 percent of Earth's mass
Crust
Makes up less than 1 percent of Earth, consisting of oceanic crust and continental crust, continental crust is often more Felsic rock
INGE LEHMANN discovered the Earth's Composition
Layers of the Earth
Crust
Mantle
Outer core
Inner core
Crust
Thin outer layer
Mantle
Thickest layer, made up of Magma
Magma
Semi-molten outer core layer which surrounds the inner core
The Earth is composed of several distinct layers, each with its own unique properties and composition
Percentage composition of the Earth
Iron (35 percent)
Oxygen (30 percent)
Silicon (15 percent)
Magnesium (13 percent)
Earth has existed for 4.543 billion years
Temperature
Influences how quickly atoms, molecules, or organisms move
Low temperature slows down chemical reactions, produces ice
High temperature breaks down important biological molecules
Radiogenic heat is heat emitted by the planet
Goldilocks zone is Earth's location where the temperature is just right
Water
Most important ingredient in biological processes
Absence of water will interfere with reactions necessary for life
Solid form (ice) hinders living organisms to use it
Solid (ice) in the 2 poles and liquid along the equator (can be consumed)
Atmosphere
Provides chemicals needed for life: carbon dioxide, nitrogen
Provides insulation/shielding from the sun and impact of small to medium size meteorites
Greenhouse gases like carbon dioxide (CO2) and methane (CH4) trap heat and avoid our planet from freezing
Ozone (O3) layer shields the Earth's surface from harmful UV radiation
Size and distance from the sun affects the ability of the Earth to hold a significant amount of atmosphere
Presence of gravity also sustains the atmosphere
Energy
Earth has rich sunlight to support life
Living organisms like plants and photosynthetic bacteria use light as a source of energy
Chemosynthetic organisms rely on chemical energy to support biological processes
Earth's position from the sun is just right to enable it to harness enough amount of sunlight
Nutrients
Essential factor used to build and maintain organism's body structure
Insufficient amount can impede synthesis of biological molecules
Volcanism helps in cycling nutrients
Water, carbon, and oxygen are some examples of nutrients
Spheres of the Earth
Atmosphere
Geosphere
Hydrosphere
Biosphere
Crust
The outermost layer and is composed of solid rock
Divided into continental crust, which is thicker and makes up the continents, and oceanic crust, which is thinner and covers the ocean basins
Mantle
The layer beneath the crust and makes up the majority of the Earth's volume
Composed of solid, but flowing, rock called mantle rock
The uppermost part of the mantle is partially molten and is known as the asthenosphere
Inner Core
The innermost layer of the Earth and is solid due to the extreme pressure
Primarily composed of iron and nickel and is the hottest part of the Earth
Outer Core
A liquid layer made up mostly of iron and nickel
Surrounds the inner core and is responsible for generating Earth's magnetic field
Asthenosphere
The layer that lies after the lithosphere (100-250km) beneath the Earth's surface
The balance between temperature and pressure is such that the rocks have little strength (weak) and easily deformed
Plays a critical role in the movement of plates on the surface of the Earth according to plate tectonic theory
Lower Mantle
Hot and exhibits "Plasticity"
In between the upper mantle and outer core of the earth
Gutenberg discontinuity is detected between Earth's lower mantle and the outer core as observed by changes in the seismic waves
Thickness: 2,240 km
Oceanic Crust
Dark shaped color
Rock Sample: basalt
More dense
Thin layer, 50 km
Continental Crust
Light-Colored
Rock Sample: Granite
Less Dense
Coarse-Textured
Thick Layer, 40-70 km
The Earth's molten metallic core gave rise to magnetic field. The magnetic field is attributed to dynamo effect of circulating current. The nature of the dynamo are not known in detail, however, it is always linked to the rotation of the earth.
Layers of the Atmosphere
Stratosphere
Troposphere
The biosphere contains the entirety of Earth's living things. It is sometimes referred to as the "zone of life." The biosphere is divided into biomes namely aquatic, forest, desert, and tundra.
Lithosphere
The solid outer section of Earth
Includes the entire Earth's crust and the rigid upper mantle
Where we can find the lithospheric plates also called the tectonic plates
The two plates are the continental and oceanic plate
Hydrosphere
The combined mass of water found on, under, and above the surface of a planet, minor planet, or natural satellite
Oceans are then divided into layers known as zones namely horizontal zones (coastal zone and pelagic zone) and vertical zone (epipelagic zone, mesopelagic zone, bathypelagic zone, abyssopelagic zone, and hadalpelagic)
Alfred Wegener proposed the "Continental Drift" theory, which is the foundation of plate tectonics
Earth's subsystems
Lithosphere
Hydrosphere
Biosphere
Lithosphere
The solid outer section of Earth, including the entire Earth's crust and the rigid upper mantle, where the lithospheric/tectonic plates are found
Hydrosphere
The combined mass of water found on, under, and above the surface of a planet, minor planet, or natural satellite, divided into horizontal and vertical zones
Silicon makes up 15 percent of the Earth's crust
Tectonic plate theory
The Earth's outer shell (lithosphere) is divided into several plates that glide over the Earth's rocky inner layer (mantle)
Tectonic plates
Act like a hard and rigid shell compared to the Earth's mobile mantle
Alfred Wegener
The father of plate tectonics, proposed the "Continental Drift" theory in 1912 which was initially ridiculed