1 / 41

The Rock Cycle

The Rock Cycle. One kind of rock turns into another which turns into another which turns into another which turns into another. Where it all begins. Igneous Rocks. Intrusive Extrusive. Intrusive Igneous. Extrusive Igneous. Basalt Low Silica – Shield Volcano.

oakes
Download Presentation

The Rock Cycle

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. TheRockCycle One kind of rock turns into another which turns into another which turns into another which turns into another

  2. Where it all begins

  3. Igneous Rocks Intrusive Extrusive

  4. Intrusive Igneous

  5. Extrusive Igneous

  6. Basalt • Low Silica – Shield Volcano

  7. Andesite – lava from the Andes • High Silica - Stratovolcano

  8. Pumice – floating rock!!! • High SilicaStratovolcano

  9. Rhyolite • High Silica – Stratovolcano

  10. Sedimentary Rocks Clastic – rock fragments - sediments Organic – shells – dinosaur bones Chemical – salt – Dead Sea Layers!!! Ripples in Stream bottoms!

  11. Sedimentary rocks cover about three-quarters of the earth's surface • Clastic sedimentary rocks are made up of rock fragments, called sediments, that have been eroded from one place and moved to another by water, ice, wind, or gravity. In time, the sediments are buried, compacted and cemented together to form sedimentary rocks. Examples include conglomerate, sandstone, and shale. • Other sedimentary rocks are “chemical” or “organic”. • Chemical sedimentary rocks are formed by the precipitation or evaporation of minerals from solution in an ancient seawater. Examples include limestone, gypsum, and halite (rock salt). • Organic sedimentary rocks are formed by the accumulation of dead plant and animal matter which is then compacted together. Examples include peat, coal and oil

  12. Strata • Layers! • Grand Canyon • Sedimentary & Metamorphic

  13. Jurassic Marl • Lyme Regis, UK

  14. Sedimentary cliff Cardiff, Cymru

  15. Ayers Rock / Uluru Sedimentary rock from rivers - exposed due to erosion Monolith!!!

  16. Metamorphic Rocks Contact or Thermal Metamorphism and Regional Metamorphism

  17. Thermal metamorphic rocks /Contact metamorphic rocks. • This type is often associated with igneous rocks. • Because of the high heat, the “regular” rock (known as country rock), near the hot rock is often altered. • The pressure involved is usually negligible. • Alteration of the rock is generally localized (close to the hot rock) in what is known as a metamorphic aureole or halo. x = Slight Metamorphism X = Intense Metamorphism ^ = Igneous rock

  18. Regional metamorphic rock is usually the result of extreme pressure. These are commonly associated with mountain building events and are often associated with plate boundaries at continental margins. • Pressure squeezes the mineral grains of sedimentary rock together. This eliminates the pore spaces, and fluids. • With more pressure, the mineral grains will form a tightly interlocking mosaic. • With even more pressure, the crystals may reform into fewer but larger grains. • This process is known as recrystallization. The recrystallized mineral may remain the same as it was, or it may be a new, more dense mineral.

  19. Classification of Metamorphic Rocks • Metamorphic rocks can be subdivided into foliated and nonfoliated types. • Foliated means there are mineral grains aligned parallel to each other. This results in a layered appearance. • A Nonfoliated metamorphic rock generally consists of equaldimensional grains. You can’t see layers • A rock can also be identified by its metamorphic grade. This is simply a description of the overall intensity of metamorphism the rock was subjected to. What this implies is that a low-grade metamorphic rock shows textural or mineralogic evidence of having been subjected to low pressures and/or temperatures.

  20. Gneiss • Foliated or Nonfoliated??

  21. Igneous /\ Melting\/ Heat&Pressure Melting /\Erosion \/ Sedimentary Metamorphic <-ErosionHeat & Pressure ->

  22. Word, Picture, Definition, Sentence • Mineral Silicate • Rock Luster • Crystal Streak • Gem Hardness • Ruby Moh’s Scale • Diamond Cleavage • Sapphire Fracture • Fossil Ore • Crystal System Texture • Specific Gravity Emerald

  23. END

  24. SEDIMENTARY TO METAMORPHIC • The following is a very general progression from sedimentary rock to metamorphic rock based primarily on pressure. • SURFACE MUD • 5 km DEEP SHALE (sedimentary) • 10 km DEEP SLATE (low grade metamorphic) • 15 km DEEP SCHIST (Garnet appears) • 20 km DEEP GNEISS (high grade metamorphic) • 25 km DEEP HORNFELS (Cordierite appears)

  25. Where is it all Found? • Hawai’i is easy enough, it’s all Volcanic! • What about the rest of North America?

  26. Shaded Relief

  27. Sedimentary

  28. Metamorphic

  29. Volcanic

  30. Plutonic

  31. All

  32. All • With some more detail

More Related