click below
click below
Normal Size Small Size show me how
Rocks and Minerals
| Question | Answer |
|---|---|
| Are remains or evidence of ancient plant and animal life on Earth. | Fossils |
| This period of time was about 544 million years ago. Fossils of fish, simple plants, insects, and the first animals to live on land are in rocks. | Paleozoic era |
| Shows how rocks change from one type of rock to another. | Rock Cycle |
| When the weight of the layers and sticky clay minerals in the sediment hold particles together. | Sedimentary rocks |
| The way a minerals surface reflects light. | Luster |
| The most common igneous rock. The ocean floor is made up of this rock. | Basalt |
| Looks like glass, forms when lava cools very rapidly. | Obsidian |
| This mineral makes up more than half the minerals in Earth’s crust. | Feldspar |
| In this era some flowering plans and bees began to appear. | Cenozoic era |
| The color of the powder that a mineral leaves when it is scratched on a special plate. | Streak |
| Rocks from this era have fossils of jellyfish in them. | Precambrian era |
| This era was about 248 million years ago. Fossil evidence shows dinosaurs appeared and then became extinct during this period. | Mesozoic era |
| Is formed from lava that has lots of gas bubbles. This floats on water. | Pumice |
| Made up of quartz, feldspar and mica. It is a slowly cooled igneous rock. | Granite |
| Testing for this is seeing how easily a mineral can be scratched. | Hardness |
| Rocks that have changed as a result of heat and pressure are known as these types of rocks. | Metamorphic rocks |
| Color, luster, hardness, streak, and cleavage are examples of these. | Physical Properties |
| The movement of bits of rock, soil, shells, and dead plant and animal matter from one place to another. | Erosion |
| Natural, nonliving solid crystals that make up rocks. | Minerals |
| Eroded material that settles on land or on the bottoms of lakes, rivers, and oceans. | Sediment |
| This is molten rock. | Magma |
| These rocks are formed when molten rock cools and hardens. | Igneous rocks |