1/77
Looks like no tags are added yet.
Name | Mastery | Learn | Test | Matching | Spaced | Call with Kai |
|---|
No study sessions yet.
Earth’s Structure – The internal organization of Earth into layers based on composition and physical properties
Core – Densest Earth layer made of iron, nickel, and radioactive elements that generate heat
Mantle – Thick layer of dense, mafic rock with high metal content and lower silica
Crust – Thin outermost Earth layer; oceanic crust is mafic and continental crust is felsic
Inner Core – Solid portion of Earth’s core composed mainly of iron and nickel
Outer Core – Liquid portion of the core that generates Earth’s magnetic field
Mesosphere – Solid lower mantle beneath the asthenosphere
Asthenosphere – Semi
molten, plastic
Lithosphere – Rigid outer Earth layer made of crust and upper mantle; divided into tectonic plates
Tectonic Plate – Large piece of lithosphere that moves over the asthenosphere
Plate Tectonics – Theory explaining movement of lithospheric plates and Earth’s surface changes
Pangaea – Ancient supercontinent where all continents were once joined
Alfred Wegener – Scientist who proposed continental drift in 1912
Seafloor Spreading – Creation of new oceanic crust at divergent boundaries
Convection Currents – Heat
driven circulation in the mantle that moves tectonic plates
Hotspot – Area where magma rises through the mantle independent of plate boundaries
Hotspot Island Chain – Line of volcanic islands formed as a plate moves over a hotspot
Divergent Plate Boundary – Plates move apart; magma rises and forms new crust
Mid Ocean Ridge – Underwater mountain chain formed at divergent boundaries
Rift Valley – Valley formed when continental crust pulls apart
Convergent Plate Boundary – Plates move toward each other, often causing subduction
Subduction – Process where a denser plate sinks beneath a less dense plate
Oceanic–Oceanic Convergence – One oceanic plate subducts forming island arcs and trenches
Island Arc – Curved chain of volcanic islands formed at oceanic–oceanic convergence
Oceanic–Continental Convergence – Oceanic plate subducts beneath continental plate forming volcanoes and mountains
Continental Continental Convergence – Collision of two continental plates forming large mountain ranges
Transform Fault Boundary – Plates slide past each other horizontally
Fault – Fracture in Earth’s crust where movement occurs
Earthquake – Sudden release of energy caused by movement along faults
Epicenter – Point on Earth’s surface directly above an earthquake focus
Richter Scale – Logarithmic scale measuring earthquake magnitude
Volcano – Opening in Earth’s crust that releases lava, ash, and gases
Tsunami – Series of large ocean waves caused by underwater earthquakes or volcanoes
Ring of Fire – Zone of intense volcanic and earthquake activity around the Pacific Ocean
Plate Movement Rate – Average movement of tectonic plates (~3–6 cm per year)
Allopatric Speciation – Formation of new species due to geographic isolation
Rock – Naturally occurring solid composed of minerals
Igneous Rock – Rock formed directly from cooled magma
Basaltic Rock – Dark, iron
rich igneous rock common in oceanic crust
Granitic Rock – Light
colored, silica
Sedimentary Rock – Rock formed from compressed and cemented sediments
Metamorphic Rock – Rock altered by heat and pressure without melting
Rock Cycle – Continuous process of rock formation, breakdown, and transformation
Weathering – Breakdown of rock into smaller pieces
Physical Weathering – Mechanical breakdown of rock without chemical change
Chemical Weathering – Chemical alteration of minerals releasing nutrients
Biological Weathering – Weathering caused by living organisms
Erosion – Transport of weathered material by wind, water, ice, or gravity
Deposition – Process where eroded material is dropped in a new location
Soil – Mixture of mineral particles, organic matter, water, air, and organisms
Parent Material – Original rock from which soil forms
Pioneer Species – First organisms to colonize bare rock and begin soil formation
Soil Formation – Process of soil developing from weathered rock and organic matter
Soil Horizons – Distinct layers of soil formed over time
O Horizon – Surface layer of organic matter and decomposing material
A Horizon – Topsoil rich in humus and biological activity
E Horizon – Zone of leaching where minerals are removed
B Horizon – Subsoil where minerals accumulate
C Horizon – Least
weathered layer closest to parent rock
Humus – Fully decomposed organic matter that improves soil fertility
Sand – Largest soil particle with high permeability
Silt – Medium
sized soil particle
Clay – Smallest soil particle with high water retention
Soil Texture – Percent of sand, silt, and clay in soil
Porosity – Amount of pore space in soil
Permeability – How easily water moves through soil
Water Holding Capacity – Ability of soil to retain water
Loam – Ideal soil texture with balanced sand, silt, and clay
Soil Fertility – Ability of soil to support plant growth
Nutrients – Essential elements for plant growth (N, P, K, Ca, Mg, Na)
Cation Exchange Capacity (CEC) – Soil’s ability to hold and exchange nutrient cations
Base Saturation – Proportion of nutrient bases relative to acids in soil
Soil Degradation – Decline in soil’s ability to support plants
Topsoil Erosion – Loss of nutrient
rich surface soil
Compaction – Compression of soil that reduces pore space
Nutrient Depletion – Loss of soil nutrients due to repeated cropping
Dust Bowl – Severe wind erosion event caused by poor farming practices
Biological Soil Activity – Actions of organisms that recycle nutrients and improve soil structure