Review the key concepts, formulae, and examples before starting your quiz.
🔑Concepts
Rocks are naturally occurring solids made up of one or more minerals, such as Quartz ().
Igneous Rocks: Formed from the cooling and solidification of molten rock. When it is underground, it is called magma; when it reaches the surface, it is called lava.
Sedimentary Rocks: Formed from the accumulation of dust, sand, and organic matter. Over millions of years, these layers are pressed together through a process called and .
Metamorphic Rocks: Formed when existing igneous or sedimentary rocks are subjected to extreme heat () and pressure (), changing their physical and chemical structure.
The Rock Cycle: A continuous process by which rocks change from one type to another over geological time due to forces like weathering, erosion, and plate tectonics.
Weathering and Erosion: The breaking down of rocks into smaller pieces () by wind, water (), and ice.
Fossils: Primarily found in sedimentary rocks because the low-pressure formation process preserves the remains of ancient organisms.
📐Formulae
💡Examples
Problem 1:
A scientist finds a rock near a volcano that has large crystals and a grainy texture. What type of rock is it, and how did it form?
Solution:
It is an Intrusive Igneous Rock (e.g., Granite).
Explanation:
Because the rock was near a volcano and has large crystals, it cooled slowly underground from magma. Slow cooling allows larger mineral crystals like Quartz () and Feldspar to grow.
Problem 2:
If a piece of Limestone () is pushed deep into the Earth's crust where it gets very hot but does not melt, what happens to it?
Solution:
It turns into Marble.
Explanation:
The application of extreme heat () and pressure () triggers a metamorphic change, recrystallizing the into a harder, denser rock called Marble.
Problem 3:
Why are fossils rarely found in Igneous rocks?
Solution:
Because of the extreme heat of magma/lava.
Explanation:
Igneous rocks form from molten rock. The temperature () of lava is usually between and , which would melt or destroy any organic remains before they could become fossils.