Structure of the Earth – Quick-Review Notes
Branches of Earth Science
Geology – Earth’s structure, formation, forces; founded by James Hutton
Geography – spatial relationships between people & environment; Eratosthenes
Physiography – physical surface features & natural processes; Alexander von Humboldt
Geophysics – Earth’s shape & physical reactions to forces; Alfred Wegener
Soil Science – outermost layer & soils; Vasily Dokuchaev
Hydrology – water distribution & movement; Robert E. Horton
Oceanography – all ocean aspects; Matthew F. Maury
Glaciology – cryosphere & environmental impact; Louis Agassiz
Atmospheric Science – entire atmosphere; Wladimir Köppen
Meteorology – troposphere & lower stratosphere phenomena; Luke Howard
Biology – living organisms; Aristotle
• Zoology – animals
• Botany – plants (Theophrastus)
Earth’s History
Age
Formation: planetary disc → proto-planets (ice & rock, no atm/water)
Core differentiation: solid inner core, liquid outer core
Theia impact → Moon; early land masses form
Atmosphere from volcanic outgassing; gravity retains gases
Oceans from cometary ice / moisture
Principle of Uniformitarianism – present processes
past processesSupercontinents timeline:
Vaalbara (3.6 billion years ago)
Ur (3.1 billion years ago)
Kenorland (2.6 billion years ago)
Columbia/Luna (1.8 Billion years ago)
Rodinia (1.1 years ago)
Pannotia (600-540 million years ago)
Pangaea (300 years ago)
Ancient ocean:
Earth’s Subsystems
Atmosphere (altitude & typical temperature ranges)
Troposphere
:Stratosphere
(Ozone layer) :Mesosphere
:Thermosphere
:Exosphere
800-10,000km
:
200Celius
Geosphere
Crust : solid silicate rocks (basalt, granite); thickness
5-50km• Boundary: Mohorovičić (Moho) discontinuity
Mantle :
2900km
thick; Fe, Mg, Al, O• Asthenosphere (flowing); convection currents
• Mantle Transition Zone
• Gutenberg discontinuity (mantle–outer core)
Core :
• Outer core
2100km
approx2100\,\text{km
, liquid Fe–Ni (creates magnetic field)
• Inner core
1200km
, solid Fe–Ni;• Lehmann discontinuity (outer–inner core)
Hydrosphere
Global water:
97.5$
saline2.5$
fresh• Glaciers
1.7%
(of total), consumable fresh water0.77
Water cycle: evaporation, condensation, precipitation, runoff, infiltration, transpiration, subduction release (volcanic steam)
Biosphere (Cycles)
Oxygen cycle: produced mainly by photosynthesis (land plants & phytoplankton); consumed by respiration, decomposition, oxidation
Carbon cycle: photosynthesis
respiration, decomposition; fossil fuel storage & human extraction; ocean–atmosphere diffusion; sedimentationNitrogen cycle:
• Nitrogen fixation (
by bacteria/lightning• Ammonification, nitrification (
returns gas to atmosphere
Geomorphic Processes
Endogenic forces (internal): driven by isostasy & mantle convection
• Diastrophism – slow bending, folding, faulting
• Fast movements – earthquakes, volcanic eruptions
Exogenic forces (external): weathering, erosion, mass movement; lower & fill Earth’s surface
Crustal Deformation
Epeirogenic (continent-scale)
Uplift → raised beaches, elevated terraces & sea caves
Subsidence → sinking crust, subduction zones
Plutonism – intrusive magma forms plutons
Volcanism – extrusive magma builds volcanic rocks
Orogenic (mountain-building)
Folding (compression)
Monocline – single gentle bend
Anticline – convex-up arch
Syncline – concave-up trough
Overturned – limbs tilt past vertical
Recumbent – fold on its side
Faulting (fracturing & displacement)
Normal – hanging wall down (tension)
Reverse – hanging wall up (compression)
Thrust – low-angle reverse
Strike-slip (lateral)
Oblique-slip – combined dip & strike movement
Horst – uplifted block between faults
Graben – down-dropped block between faults