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Rock formed underground under high heat and pressure is
Sedimentary
Paper read-out from an Earthquake Reading Machine
The point where you are standing directly above where the Earthquake happens
Metamorphic
Igneous Rock
Igneous
Metamorphic Rock
Rocks are constantly changing
Basalt and Obsidian are examples of
Sedimentary
Paper read-out from an Earthquake Reading Machine
The point where you are standing directly above where the Earthquake happens
Metamorphic
Igneous Rock
Igneous
Metamorphic Rock
Rocks are constantly changing
Lapilli is an example of what kind of rock?
Sedimentary
Paper read-out from an Earthquake Reading Machine
The point where you are standing directly above where the Earthquake happens
Metamorphic
Igneous Rock
Igneous
Metamorphic Rock
Rocks are constantly changing
The epicenter of an earthquake is the
Sedimentary
Paper read-out from an Earthquake Reading Machine
The point where you are standing directly above where the Earthquake happens
Metamorphic
Igneous Rock
Igneous
Metamorphic Rock
Rocks are constantly changing
The rock cycle says that
Sedimentary
Paper read-out from an Earthquake Reading Machine
The point where you are standing directly above where the Earthquake happens
Metamorphic
Igneous Rock
Igneous
Metamorphic Rock
Rocks are constantly changing
Marble and Slate are
Sedimentary
Paper read-out from an Earthquake Reading Machine
The point where you are standing directly above where the Earthquake happens
Metamorphic
Igneous Rock
Igneous
Metamorphic Rock
Rocks are constantly changing
Seismograms are
Sedimentary
Paper read-out from an Earthquake Reading Machine
The point where you are standing directly above where the Earthquake happens
Metamorphic
Igneous Rock
Igneous
Metamorphic Rock
Rocks are constantly changing
Squeezing sand, dirt, igneous, and metamorphic rock pieces together over time makes
Sedimentary
Paper read-out from an Earthquake Reading Machine
The point where you are standing directly above where the Earthquake happens
Metamorphic
Igneous Rock
Igneous
Metamorphic Rock
Rocks are constantly changing
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