PRACTICAL TASK:
ROCKS
Igneous Rocks:
They are formed underground or above ground when magma
(if it is underground) or lava (when is above ground) cools.
Example:
Obsidian:
# Formed when lava cools above ground.
# Actually glass and not a mixture of minerals.
# It’s edges are sharp.
# It’s edges are sharp.
Metamorphic Rocks:
Were igneous or sedimentary rocks before, that with the pressure,
wich fosters hit build up, and this causes them to change.
Example:
Schist Rocks:
# Were igneous rocks before.
# Are formed from basalt.
# Were igneous rocks before.
# Are formed from basalt.
# Transform into metamorphic because of
heat and pressure.
heat and pressure.
Sedimentary Rocks:
Are formed million years ago, by little pieces of earth or rocks
that were erosion or weathering, this pieces get together
and formed the sedimentary rocks.
Example:
Conglomerate Rocks.
# Made up of large sediments.
# Made up of large sediments.
# It cemented together with dissolved
minerals.
minerals.
# Sediments are so large that pressure
can’t hold the rock.
What rocks are similar to the ones we saw in class?
The ones that are very similar to the ones we saw in class are the Obsidian
and Schist Rocks. But the Conglomerate Rock is not similar to any rock
that we saw in class.
PRECIOUS ROCKS | SEMIPRECIOUS ROCKS |
It’s less common to find them, that’ why they are more value. | It’s more common to find them, that’s why they are less value. |
By: Ganora, Florencia
&
Villar C. Camila
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