There are three main types of rocks: sedimentary rock, which forms from the deposits of other rocks over time; igneous rock, which forms when lava or magma cools on the surface of the Earth; and metamorphic rock, which forms underground through heat and pressure acting on sedimentary or igneous rocks. The document provides details on the formation and characteristics of each rock type.
Rocks on Earth can be classified into three categories based.pdfadaacollections
Rocks on Earth can be classified into three categories based on the way they were formed.
Igneous rocks are formed through volcanic action. Sedimentary recks are formed by deposition.
Metamorphic rocks are formed when existing rocks undergo a change due to extreme heat and
pressure. Rocks that have a volcanic origin are classifed as igneous and form when magma or lwa
cook and hardens. As the magma or lava cook; crystals begin to form. The size of the crystals
depends upon how fast the magma or lawa cools. If magma cools quickly, small crystals form and
can be observed on the rock surface, such as in basalt, for example. Lava can cool so quickly that
crystals do nothave time to form at all, such as with obsidian. If mogma cools slowly. larger
crystals form and can easily be seen on the surface of rock specimens. A common example of
igneous rock that exhibits large erystal formation is granite. When Earth's materials are deposited
in layers and pressed together over time, sedimentary rocks form. The formation of sedimentary
rock begins with the deposition of sediments. As layers are added, the oldest or lower layers that
were deposited first experience increased pressure. The sediments and the spaces between then
are crushed together in a process cal ied conpaction. During the cementation process, the
sediments are bound together when a solution fills in around the particles like glue. If the
rediments deposited are sand particles, such as in a beach environment, sandstone forms. If the
sediments are fine sit or clay-sited particles, commonly cal ed'mud;' such as those found in basins
worldwide, shaie forms, thestone typically forms from shells and other sediments deposited in
ocean environments. A quiet and undistubed ewironnent will sometimes lead to fossit formation
vithin the Layers of sedimentary deposition. Metamorphic rock forms when one type of rock
changes into another due to exposure to heat and pressure ofter cansed by morement of material
deep beneath Carthis surface. This change to rock appearance and cemposition takes an
entrenelylong tine. Metamorphle rocks are often characterized by wavy layers of mineral orytals or
by the presence of unusual mincrals. Any rock can become a metamorphic rock. For example, the
sedimentary rock ahule forms from layers of deposited sitt. When exposed to high pressure due to
scologic processes. the metamorphic rock slate forms. The sedimentary rock sandstone changes
to cuataite when exposed to extreme heat and pressure beneath Eath's surface. Another example
of a metamorphic rock is mable. which forms when limestone is exposed to extreme temperatures
or prescure. Igneous basalt changes to schikt in the metanorphic process. The interesting. thing
about the motamorplic nrocess is that any rock-igneous, metamorphic, or seclinentary-will change
and form now metamorphic rock given enough time, heat, andor pressure. The rock cycle
llustrates how rocks move on and under Earth's crust and change from one typ.
List each category of rock and describe how it formsExpl.pdfadityacomputers001
List each category of rock and describe how it forms.Explore Student Journal: The Rock Cycle aks
on Earth can be classified into three categories based on the way they were formed. Igneous
rocks are formed through volcanic action. Sedimentary ks are formed by deposition. Metamorphic
rocks are formed when existing rocks undergo a change due to extreme heat and pressure. cks
that have a volcanic origin are classified as igneous and form when magma or lava cools and
hardens. As the magma or lava cools, crystals begin to im. The size of the crystals depends upon
how fast the magma or lava cools. If magma cools quickly, small crystals form and can be
observed on the rock iface, such as in basalt, for example. Lava can cool so quickly that crystals
do not have time to form at all, such as with obsidian. If magma cools slowly. ger crystals form and
can easily be seen on the surface of rock specimens. A commen cxample of igneous rock that
exhibits large crystal formation is anite. Then Earth's materials are deposited in layers and
pressed together over time, sedimentary rocks form. The formation of sedimentary rock begins
with the eposition of sediments. As layers are added, the oldest or lower layers that were
deposited first experience increased pressure. The sediments and the paces between them are
crushed together in a process called compaction. During the cementation process, the sediments
are bound together when a olution fills in around the particles like glue. If the sediments deposited
are sand particles, such as in a beach environment, sandstone forms. If the ediments are fine silt
or clay-sized particles, commonly called "mud." such as those found in basins worldwide, shale
forms. Limestone typically forms from thells and other sediments deposited in ocean
environments. A quiet and undisturbed environment will sometimes lead to fossil formation within
the layers of sedimentary deposition. Metamorphic rock forms when one type of rock changes into
another due to exposure to heat and pressure often coused by movement of material deep
beneath Earthis surface. This change to rock appearance and composition takes an extremely
long time. Metamorphic rocks are often characterized by wavy layers of mineral crystals or by the
presence of unusual minerals. Any rock can become a metamorphic rock. For example, the
sedimentary rock shale forms from layers of deposited silt. When exposed to high pressure due to
geologic processes, the metamorphic rock slate forms. The sedimentary rock sandstone changes
to quartzite when exposed to extreme heat and pressure beneath Earth's surface. Another
example of a metamorahic rock is marble. which forms when limestone is exposed to extreme
temperatures or pressure. Igneous basalt changes to schist in the metamorphic process. The
interesting thing about the metamorphic process is that any rock-igneous, metamorphic, or
sedimentary-will change and form new metamorphic rock given enough. time, heat, and/or
pressure. The .
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Session Overview
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2. THE_THREE_TYPES_OF_ROCKS_
1. Sedimentary Rock: over time the deposit of other
rocks form together to form a sedimentary rock.
2. Igneous Rock: igneous rock is formed when lava
or magma cool into a rock on the surface.
3. Metamorphic rock: metamorphic rock forms
under earths surface when heat and pressure
cause igneous or sedimentary to change into
metamorphic rock
4. IGNEOUSE_ROCK_
1. Igneous rock is usually the top layer of the earths
surface
2. Igneous usually takes several years to form
3. It forms when lava or magma cool an harden
5. METAMORPHIC_ROCK_
1. Metamorphic rocks are usually found under igneous
or sedimentary rocks
2. Metamorphic rocks are formed by heat and pressure
on other rocks
6. QUESTIONS!
1. How are metamorphic rocks formed?_________
2. What are Sedimentary rocks?________
3. The three main rocks are metamorphic,
sedimentary and _________ rock.
7. I'M DONE
• Thanks for watching this amazing
video!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!
