Georges Lemaître, a Belgian Catholic priest and physicist, developed the Big Bang theory, suggesting the universe began from a single primordial atom
The Big Bang Theory explains the universe starting with a small singularity, then inflating over 13.8 billion years to the cosmos we know today
The Steady State Theory claims the universe is always expanding with a constant average density and has no beginning or end, but it's now rejected by most cosmologists
The Cosmic Inflation Theory supports the Big Bang Theory, proposing that the early universe was a rapidly expanding bubble of pure energy
The Nebular Hypothesis explains that the solar system formed from the collapse of a giant cloud of gas and dust, with the hot central region becoming the sun and the surrounding materials forming planets
The Planetesimal Theory suggests that about 5 billion years ago, a great cloud of gas and dust rotated slowly in space, eventually forming solid bodies called planetesimals
Earth's atmosphere contains 78% nitrogen, 21% oxygen, and 1% argon, with atmospheric layers including the troposphere, stratosphere, mesosphere, thermosphere, and exosphere
The Nebular Hypothesis explains how stars and planets form from the collapse of a giant cloud of gas and dust, with the material in the center forming a star and the outer part forming planets
The Earth's internal structure includes the crust, mantle, outer core, and inner core, as well as the lithosphere, asthenosphere, and mesosphere
Factors for life to thrive on Earth and other worlds:
Water is a crucial solvent
Energy sources are essential, like sunlight for photosynthesis
Time for evolution, with stars living long enough for life to evolve
Recycling processes like plate tectonics are vital
Bonus features like stable radiation from the sun and a protective magnetic field
The Earth's atmosphere is composed of 78% nitrogen, 21% oxygen, 0.9% argon, 0.03% carbon dioxide, and trace amounts of other gases
The biosphere includes all parts of Earth where life exists, from root systems to ocean trenches and mountaintops
The lithosphere is the solid, outer part of the Earth, including the crust and the top part of the mantle
The hydrosphere comprises the Earth's liquid water, covering about 70% of the Earth's surface and divided into freshwater and saltwater
Rocks are made up of minerals, which are naturally occurring solid substances with a definite chemical composition
Physical properties used to identify minerals include color, streak, hardness, cleavage, crystalline structure, transparency, magnetism, tenacity, luster, odor, and specific gravity
The Mohs scale is used to measure the hardness of minerals, graded from 1 to 10, with 10 being the hardest and 1 the softest
Georges Lemaître, a Belgian Catholic priest and physicist, developed the Big Bang theory
The Nebular Hypothesis explains how stars and planets form: a giant cloud of gas and dust collapses, rotates, flattens into a disk, with the densest and hottest material forming a star and the outer part forming planets
A cutaway view of the earth reveals its internal structure, including the crust, mantle, outer core, inner core, lithosphere, asthenosphere, and mesosphere
Fluorite is a calcium fluoride mineral found in various colors, used in applications like steel production and hydrofluoric acid manufacturing
Crystalline solids have atoms, molecules, or ions arranged in a regular, repeating pattern, giving them characteristic properties like shape, hardness, and melting point
Mineral properties:
Cleavage and fracture describe how minerals break into pieces, with cleavage being a smooth break along the crystalline structure and fracture occurring where there is no cleavage
Crystalline structure indicates how a mineral's crystals are arranged, with silicate minerals being the largest and most abundant group containing silicon, oxygen, and other elements
Mineral identification:
Transparency or diaphaneity indicates the extent of light passing through a mineral
Magnetism shows a mineral's ability to attract or repel other minerals
Tenacity reveals a mineral's resistance to stress like crushing or bending
Luster refers to a mineral's reaction to light, determining its brilliance
Odor is the distinct smell released by a mineral when subjected to water, heat, air, or friction
Specific gravity measures a mineral's density and weight compared to water
Chemical properties of minerals:
Minerals are classified based on their chemical composition, with eight basic classes like silicate, carbonate, sulfate, and oxide
Rock classifications:
Rocks are categorized into igneous, sedimentary, and metamorphic types based on their formation process
Igneous rocks form from the solidification of molten rock material, either below the Earth's surface (plutonic) or at the surface (volcanic)
The Nebular Hypothesis explains how stars and planets form from the collapse of a giant cloud of gas and dust, which flattens into a disk where the densest and hottest material forms a star, while the outer part forms planets
Igneous rocks form from the solidification of molten rock material (magma or lava) either below the Earth's surface (plutonic igneous rocks) or at the surface (volcanic igneous rocks)
Minerals are formed during the crystallization of magma, with the rate of cooling being a crucial factor that controls crystal size and the texture of the rock
Sedimentary rocks form through the accumulation, compaction, and cementation of sediments, with common features including strata (bedding and lamination) and fossils
Metamorphic rocks form from the transformation of pre-existing rocks through metamorphism, involving changes in physical and chemical properties in response to heat, pressure, and chemically active fluids
The lithosphere is the solid, outer part of the Earth, including the brittle upper portion of the mantle and the crust, the outermost layers of Earth's structure
The hydrosphere covers about 70% of the Earth's surface and is the home for many plants and animals, divided into freshwater and saltwater
The atmosphere is composed of 78% nitrogen, 21% oxygen, 0.9% argon, 0.03% carbon dioxide, and trace amounts of other gases
Silicate minerals are the largest and most abundant group containing silicon and oxygen with some aluminum, magnesium, iron, and calcium
The Big Bang theory explains the universe starting with a small singularity and inflating over 13.8 billion years to the cosmos we know today
The Cosmic Inflation theory supports the Big Bang Theory, stating that the early universe is a rapidly expanding bubble of pure energy
The Nebular Hypothesis is a scientific theory explaining how stars and planets form from the collapse of a giant cloud of gas and dust
The Steady State theory claims the universe is always expanding with no beginning or end, and its appearance remains the same over time
The Biosphere is the part of Earth where life exists, extending from the deepest root systems of trees to high mountaintops