Aristotle observed Earth’s land composition changes at a slow rate
Earth Systems Science (ESS) studies Earth as an integrated system, seeking to understand the past, current, and future state of our planet
Sustainability refers to the capacity of Earth to support human life without depleting natural resources
Notable scientists in Earth Science include Vladimir Vernadsky, Alexander von Humboldt, James Hutton, James Lovelock, and Lynn Margulis
Earth Science includes four subsystems: Atmosphere, Biosphere, Lithosphere, and Hydrosphere
The Atmosphere is composed of gases like Nitrogen, Oxygen, and Carbon dioxide
The Atmosphere is divided into layers including the Troposphere, Stratosphere, Mesosphere, Thermosphere, and Exosphere
The Geosphere (Lithosphere) is divided into three layers: crust, mantle, and core
The Crust is the thinnest and outermost layer of the Geosphere, made of solid rocks and minerals like Fe, Na, Ca, Ti, Si, O, Al, K, H
The Mantle is mostly made up of silicate rocks rich in magnesium and iron, contributing to plate tectonics, volcanoes, earthquakes, and mountain building
The Core is the innermost layer of Earth, made up of iron and nickel, with two layers: the outercore (liquid state) and the inner core (solid state)
Earth is a complex system consisting of living and nonliving components
Earth Science is the branch dealing with the physical components of Earth, including Geology, Physics, and Atmospheric Science
Earth System Science (ESS) studies Earth as an integrated system, aiming to understand the past, current, and future state of the planet
Sustainability refers to Earth's capacity to support human life without depleting natural resources
Noosphere is the sphere of human consciousness and reason
Uniformitarianism states that geological forces in the past are the same as those in the present
Gaia hypothesis proposes that Earth works as a self-regulating system
Atmosphere consists of all the gases on Earth, derived from the Greek word atmos meaning gas
Geosphere, from the Greek geo meaning ground, is divided into crust, mantle, and core
Hydrosphere is the total water on a planet, including surface, underground, and the cryosphere, which is frozen water
Biosphere is the zone where life exists, encompassing all living organisms and ecosystems
Troposphere is where most of Earth's weather occurs and where clouds are generated
Stratosphere houses Earth's ozone layer, protecting from UV rays
Mesosphere is the coldest layer of Earth where most meteors burn up
Thermosphere, where auroras are seen
Exosphere is the uppermost layer of the atmosphere with gases like hydrogen and helium
Crust is the thinnest, outermost layer of Earth made of solid rocks and minerals
Mantle, the largest layer, is mostly silicate rocks rich in magnesium and iron
Core, the innermost layer, is made of iron and nickel, with the inner core solid and the outer core liquid
Asthenosphere is a ductile part of the upper mantle
Oceanic crust is thinner and denser, making up the seafloor, while continental crust is thicker and less dense, forming continents
Trenches are long depressions on the seafloor formed at tectonic plate boundaries where one plate subducts beneath another
Volcanic arcs are chains of volcanoes above subduction zones
Karman line separates the atmosphere and outer space
Mohorovicic discontinuity is the boundary between the crust and mantle
Bullen discontinuity separates the upper and inner core
S-waves and P-waves help identify the liquid state of the outer core
Saltwater makes up 97.5% of Earth's water
Ocean currents describe how water moves in the oceans