Geology 1 Review

The chemical and mechanical breakdown of rocks at the surface.

This is not just academic trivia. The principles of are used daily to:

The mantle is not liquid magma. It is a hot, ductile solid that flows like very thick pitch. geology 1

Leo stopped fidgeting. "Fire?"

: Elements like quartz or precious gems like diamonds. The chemical and mechanical breakdown of rocks at

Everything starts with , which are the naturally occurring inorganic compounds that build every rock on the planet.

![Rock Cycle Concept] (Imagine arrows looping between the three rock types) It is a hot, ductile solid that flows like very thick pitch

"Lesson one, Leo," she said, tapping a fingernail on a sparkly cluster of crystals. "This is the beginning."

She looked from the fossil to the distant peak where the granite began. "So you see, Leo, this mountain isn't one thing. It's a library. The bottom floors are fire and strength. The middle floors are mud and time and ghosts of the deep. And the top…" She looked up at the jagged peak. "The top is the latest chapter, still being written."

Formed by the cooling and solidification of magma (underground) or lava (above ground).

Classify samples into major categories: Igneous, Sedimentary, or Metamorphic. Geological Processes: Explain the forces that shaped the area, such as volcanism, earthquakes, or weathering 4. Conclusion: