1.
Endogenic Proccess

2.
• Endogenic processes are geological processes that occur
beneath the surface of the earth.
• It is associated with energy originating in the interior of the
solid earth.
• The ground we live on is moving all the time, the forces
within the earth that cause the ground to move are called
Endogenic process.

3.
Endogenic Processes
• Folding & Faulting
• Heat in the Earth’s Interior
• Magmatism
• Metamorphism
• Volcanism & Plutonism

4.
Folding & Faulting
• Folding- when two forces push towards each other from
opposite sides, the rock layers will bend into folds.
• Faulting- faulting is the fracturing and displacement of
more brittle rock strata along a fault plane either caused
by tension or compression.

5.
Interior Heat
• Primordial Heat- Heat generated during earth’s formation.
Sources:
Accretion Energy- Heat released from collision of planetary
objects during the early formation of planets.
Core Formation Energy- Heat from earth’s core.
Radioactive Heat- Heat generated by long term radioactive
decay.

6.
Magmatism
• It happens when magma generated and develops into
ingneous rocks.

7.
Mid-Oceanic Ridges
• The rising of magma in mantle convection cell brings heat
to the suface, transferring heat to the overlying rocks.

8.
Mid Oceanic Ridges
• The transfer of heat due to the convection is accompanied
by a decrease in pressure or decompression associated
with the spreadibg of the tectonic plates.

9.
Mantle Plumes
• The transfer of heat and the compression result to magma
generation.

10.
Subduction Zone
• Oceanic crustal rocks ate formed along spreading
centers, typically beneath several kilometers of sea water.

11.
Metamorphism
• It is the process of changing materials that make up the
rock, the chemical components and gealogic
characteristics of the rocks change because of exposure
to heat & pressure.

12.
Compression
• Rocks push or squeeze against on another where the
stress produced is directed towards the center.

13.
Tension
• Pulled apart rocks may separate in opposite direction.

14.
Shearing
• Some of the portion of a plate at the edge may break
away in different directions. Eventually makit the plate
smaller inside.

15.
Confining
• The crust become compact. Thus making it look smaller.

16.
Volcanism
Plutonism- is the formation of intrusive igneous rock by
solidification of magma beneath the earth’s surface.
Volcanism- is the phenomenon of eruption of molten rocks
( magma) onto the surface of the earth or a solid suface
planet.
Volcano- a volcano is a vent or opening on planet’s surface
which allows molten rocks called magma, volcanic ash and
gas to escape out onto its surface.
Tectonic Plates- most volcanoes are formed by the
movement of tectonic plates on the suface of the earth.

17.
• The edge of the tectonic plates are the areas where
most volcanoes form.
• Crater- funnel shaped pit at the top of a volcano, it is
formed when materials are blown out of the volcano by
explosion.
• Caldera- whem the volcano collapses due to an empty
magma chamber.

18.
Types of volcano
• Composite volcano
• Cinder cone volcano
• Shield Volcanoes

19.
Composite Volcanoes
• Composite volcanoes often form the largest and tallest
volcanoes, they are the most explosive and dangerous of
the types of volcanoes.

20.
Cinder Cone Volcano
• It is usually smaller than composite volcano amd the
eruptions are smaller also, they form into steep cone
shaped hills.

21.
Gas and Pyroclastic
• Most of the gas released during eruption is water vapor
carbon dioxied, sulfur dioxide, hydrogen sulfide, and
hydrochloric acid, are given off in lesser amount of
surface water introduced into a volcanic system can
greatly increase the explosivity of an eruption.

22.
Types of Volcanic Eruptions.
• Hawaiian Eruption
• Strombolian Eruption
• Volcanian Eruption
• Pinian Eruption

23.
Types of Lava flow
• Pahoehoe
• AA
• Pillow Lava
• Blocky