A solid collection of mineral grains held together in a solid mass, and they are majorly classified by how they are sourced and formed
Types of Rocks
Igneous Rocks
Sedimentary Rocks
Metamorphic Rocks
Rock Cycle
A web of processes that outlines how each of the three major rock types—igneous, metamorphic, and sedimentary—form and break down based on the different applications of heat and pressure over time
Mineral
Naturally occurring, solid at room temperature, inorganic, fixed chemical structure
A feature on Earth's surface that is part of the terrain, including mountains, hills, plateaus, plains, and minor landforms like buttes, canyons, valleys, and basins
Waterforms / Waterways
Ocean
Sea
Strait
Gulf
Bay
Lake
River
Tributary
Spring
Lagoon
Waterfall
Stratigraphy
The study of rock layers and layering (stratification)
Principles of Stratigraphy
Catastrophism
Uniformitarianism
Law of Superposition
Law of Lateral Continuity
Law of Original Horizontality
Law of Cross-Cutting Relations
Faunal Succession
Fossils
Preserved remains or traces of organisms from the past
Geologic Time
Formation of the Earth (4.6 BYA)
Cambrian explosion (530 MYA)
Holocene (11.8 KYA - Present)
Absolute Dating
Gives numerical age (e.g. 200 ± 3 million years)
Relative Dating
Arranges objects/organisms/events in time (which one is older/younger)
Plate Tectonics
Earth's crust and rigid upper mantle are broken into enormous slabs called tectonic plates that interact at their boundaries
Fueled by magma, which is a molten or semi-molten natural material formed by the heating of the Earth's crust and mantle
Convection currents
Cause plates to move
Divergent boundary
Plates move apart
Convergent boundary
Plates come together (oceanic-oceanic, oceanic-continental, continental-continental)
Transformboundary
Plates slide horizontally past each other
Magma
A slushy mixture of molten rock, mineral crystals, and gases
Lava
Magma that reaches the Earth's surface
Most of Earth's active volcanoes are located along plate boundaries
Shield volcanoes
Largest of the three types, long gentle slopes, composed of layers of solidified basaltic lava, quiet eruptions
Cinder cones
Smallest of the three types, steep-sloped cone-shaped, usually composed of basaltic lava, explosive eruptions, usually form at edges of larger volcanoes
Composite volcanoes
Considerably larger than cinder cones, tall majestic mountains, composed of layers of granitic rock and lava flows, cycle through periods of quiet and explosive eruptions
Types of magma
Basaltic
Andesitic
Rhyolitic
Stress
Total force acting on crustal rocks per unit area (compression, tension, shear)
Strain
Deformation of materials in response to stress
Faults
Any fracture or system of fractures along which Earth moves, they form when the forces acting on rock exceed the rock's strength
Types of faults
Reverse (compression), Normal (tension), Strike-slip (shear)