METAMORPHISM.pdf Grade 11 earth and life science lesson

bucasascarlo 1,419 views 29 slides May 02, 2024
Slide 1
Slide 1 of 29
Slide 1
1
Slide 2
2
Slide 3
3
Slide 4
4
Slide 5
5
Slide 6
6
Slide 7
7
Slide 8
8
Slide 9
9
Slide 10
10
Slide 11
11
Slide 12
12
Slide 13
13
Slide 14
14
Slide 15
15
Slide 16
16
Slide 17
17
Slide 18
18
Slide 19
19
Slide 20
20
Slide 21
21
Slide 22
22
Slide 23
23
Slide 24
24
Slide 25
25
Slide 26
26
Slide 27
27
Slide 28
28
Slide 29
29

About This Presentation

Metamorphism


Slide Content

METAMORPHISM

OBJECTIVES
1. identify the factors involved in
metamorphism,
2. differentiate the types of metamorphism;
3. explain the effects of pressure and
temperature on the composition and texture of
the rocks undergoing metamorphism.

Metamorphism is one of the
geologic processes in which rocks
change in form, composition, and
structure due to intense heat and
pressure and sometimes with the
introduction of chemically active
fluids.

Metamorphism takes place tens of kilometers
below the surface where temperatures and
pressures are high enough to transform rock
without melting it. The increase in temperature
and pressure and change of the chemical
environment can change the mineral
composition and crystalline textures of the
rock while remaining solid all the while.

Factors Involved in Metamorphism
Temperature.
It plays a crucial role in metamorphism. The heat
affects the rock’s chemical composition, mineralogy,
and texture. For instance, during burial
metamorphism, at a depth of about 8 to 15 kilometers
from the surface of the crust, metamorphic reactions
begin

Factors Involved in Metamorphism
Pressure.
Like temperature, it changes the composition,
mineralogy, and texture of rocks. Pressure is
different in various tectonic settings, like
temperature. For instance, metamorphism in
the subduction zone is characterized by high-
pressure metamorphism.

Contact metamorphism is prominent in areas
where surrounding rocks are exposed to heat
coming from magma intrusion within the layers of
the rocks. Marble, quartzite, and other
granoblastic rocks with large visible crystals of
minerals may be formed through contact
metamorphism.

Regional Metamorphism forms foliated
metamorphic rocks such as Gneiss
and Schist due to high temperature
and pressure imposed on large parts
of the crust
Tags