Across
- 2. ______ is an example of a hot spot.
- 3. the Black Forest in ______ is an example of a horst
- 7. A large expanse of nearly flat-lying lava flows.
- 8. is an example of a fault-block mountain.
- 10. The upwelling of high temperature material from deep within the mantle
- 12. When magma pushes up towards the surface of the Earth’s crust, the magma does not break through but instead raises a section of the crust up as it rises.
- 16. A mountain or range formed as a horst when it was elevated between parallel normal faults.
- 18. ________ Mountains form from an expulsion of materials from deep within the earth in the form of enormous amounts of lava or cinders which pile up on the earth's surface, forming a mountain.
- 20. _______ and water constantly wear a mountain, creating eroded Mountains
- 21. The Andes are an example of a mountain_____.
- 22. The group of natural processes, including weathering, dissolution, abrasion, corrosion, and transportation, by which material is worn away from the earth's surface.
Down
- 1. ________boundaries are areas where continental or oceanic plates are moving away from each other and creating new crust.
- 4. Hot molten or semifluid rock erupted from a volcano or fissure, or solid rock resulting from cooling of this
- 5. A mountain resulting chiefly from large-scale folding of the Earth's crust.
- 6. Stone Mountain is an example of a ____ mountain.
- 9. _______ ______are formed when two plates collide and buckle upwards.
- 11. A transverse boundary is when two _____ collide, causing great amounts of pressure.
- 13. The_____ are an example of fold mountains.
- 14. Hot fluid or semifluid material below or within the earth's crust from which lava and other igneous rock is formed by cooling
- 15. An example of an eroded mountain.
- 17. Dome Mountains form when magma is injected between two layers of sedimentary rock, causing the overlying strata to bulge _______ forming the dome shape
- 19. A _____is formed from extension of the Earth's crust. The raised block is a portion of the crust that generally remains stationary or is uplifted while the land has dropped on either side.
