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Pangaea
Single
landmass
or
supercontinent
Panthalassa
Vast
sea
or super
ocean
Tectonic
Term derived from a Greek word tekton which means "carpenter" or "builder"
Lithosphere
Massive,
irregular
slab of solid rocks that envelope the surface of
Earth
Contraction
theory
As the
Earth
cooled after its formation, its surface contracted and wrinkled, with these wrinkles being the
mountain ranges
on Earth's surface
Continental Drift Theory
Proposed by Alfred Wegener in 1915, explained that about 1, 100 million years ago, there was a super continent named
Rodinia
, which predated
Pangaea
Seafloor Spreading Theory
Proposed by Harry Hess in 1960s, says that the seafloors or ocean floors, not the
continents
move and carry the
continents
along
Mantle Convection Theory
Warm less dense material rises
,
cooler more dense material sinks
, creating a cycle
Slab Pull Theory
Gravity
and the plates themselves are responsible for the
plate tectonics
through SUBDUCTION process
Divergent Plate Boundary
Two plates move
away
from each other, creating a gap or
rift
between them
Convergent Plate Boundary
Two plates slide toward each other and form either a
subduction zone
or an
orogenic belt
Transform Plate Boundary
The
plates
slide against one another in opposite directions, resulting in
earthquakes
Wegener's
continental drift
theory was regarded as improbable and ridiculous until the discovery of
magnetic reversals
in the 1950s
Paleontological Evidence
Fossils of
Lystrosaurus
and
Cynognathus
Identical
plant
fossils found in
coal beds
of Europe and US
Evidence from
Glaciation
Till
deposits
indicating
erratic
glacier motion
Glaciation
in the
southern
hemisphere
Evidence from structure and rock type
Coastlines
of
continents
fitting together
Rift Valleys
of
Africa
Evidence from
Paleoclimates
Distribution
of specific rock types indicating past
climatic
zones
Lithosphere
Outer solid part of the planet includes
Earth's crust
and the underlying cool, dense and rigid upper part of the
upper mantle
Asthenosphere
High viscous, hotter, and ductile region of the upper
mantle
involved in
plate
tectonic movement and isostatic adjustment
Layers of the Earth
Crust
Mantle
Core
Layers of the Atmosphere
Troposphere
Stratosphere
Mesosphere
Thermosphere
Exosphere
Biosphere
Sphere that encompasses all
life forms
on earth
Aeolian Landforms
Formed by the chemical and mechanical action of the
wind
Aeolian Landforms: Erosional
Mesas
Buttes
Canyons
Gorge
Mountainous and
Glacial
Landforms
Exhibit
slopes
,
summit
area, and local relief, rise higher than the rest of their surroundings
Volcano
Cone-shaped hill or mountain formed by the
extrusion
of lave or ejection of rock fragments from a
vent
Theories of Volcanism
1.
Plate tectonics
2.
Natural radioactivity in rocks
3.
Convection currents
Features of a Volcano
Cone
Vertical and horizontal movement of the crust
Typically produces the
mountains
Erosion
Physical removal of rock or wearing down of
landmasses
Volcanism
Phenomenon related to the various processes associated with the surface discharge of
magma
or hot water and
steams
Volcano
Cone-shaped
hill or mountain formed by the
extrusion
of lava or ejection of rock fragments from a vent
Vulcano
An island off Sicily named after the Roman god of
fire
,
VULCAN
There are 859 active volcanoes in the world, more than
75
% of them are located in the
Circle of Fire
Plate tectonics
Scientific study of the origin and arrangement of the broad structural features of the Earth's surface known as the
LITHOSPHERE
Convection currents
are formed and caused the plates in the
crust
to move
Volcanoes
are formed when hot materials such as
magma
from the below rises and leaks into the crust
Features of a Volcano
Cone
Fissure
Conduit
Vent
Crater
Flank
Summit
Magma chamber
or
reservoir
Inactive or dormant volcano
The volcano is declared inactive or dormant if the last traces of volcanic heat
disappear
and if it has not erupted in
2000
years
Some extinct volcanoes in the Philippines
Mt. Butay
Mount
Guinsiliban
on
Camiguin
Island
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