the rock cycle
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NASA video. The Rock Cycle. The three types of rocks Igneous sedimentary Metamorphic A ll types of rock are subject to processes that change one rock type into another. Igneous Rocks. Formed from cooled and solidified magma Intrustive - PowerPoint PPT PresentationTRANSCRIPT
The three types of rocks– Igneous– sedimentary– Metamorphic
All types of rock are subject to processes that change one rock type into another.
Igneous RocksFormed from cooled and solidified magma– Intrustive• formed from the cooling of magma within the earth’s
crust• Cools and hardens slowly • Coarse grained- forms large, well-developed crystals
– Extrusive• melted rock that hardens on the earth’s surface• Lava cools rapidly• fine grained rocks
Composition of Igneous Rocks• Felsic- Rocks in the granite family – Light colored– High silica content– Low magnesium and iron content
•
• Mafic- Rocks in the basalt family – dark colored– lower silica content– high mg and fe content
•
• Andesitic - Medium Silica– Green, grey, or brown
Sedimentary Rocks• rock formed from the debris of both other rocks and
living matter.• 90% of the earth’s crust is made from igneous rock,
but 75% of the world’s land surface is covered with thin layers of debris or sediments.
• These sediments settle on the beds of oceans, lakes, and rivers, and recompacted over millions of years to form sedimentary rock.
How are Sedimentary Rocks Formed?• DIAGENESIS-
– the process that turns loose sediments into rock – COMPACTION- • the slow squeezing of sediment to form hard rock
– CEMENTATION- • The binding together of compacted sediments by
chemicals like calcite, silica, and iron
3 types of Sedimentary Rock:– CLASTIC- form from rock fragments weathered
and eroded by glaciers, wind, rivers, and waves.– ORGANIC- rock made from the remains of plants
and animals– CHEMICAL- rock made from chemicals dissolved in
water
BEDDING PLANE- a boundary between one layer of sedimentary rock and another
Metamorphic Rocks• formed from other rocks as a result of intense
heat, pressure, and chemical processes– most form deep beneath the surface of the earth– formed from existing igneous, sedimentary, or
metamorphic rock
Types of metamorphic formation:• Contact metamorphism: – when hot magma pushes through
existing rock, changing the structure and composition of the rock. Only rocks near the magma are changed.
• Regional metamorphism: – movement of one tectonic plate
against another causes heat and pressure, affecting rocks over an area of many thousands of kilometers
Types of metamorphic rocks:• Foliated: – show visible parallel bands of minerals ex: slate,
schist• Unfoliated: – no bands of crystals ex: quartzite, marble