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Chapter 4 Rocks.  Why should I care? You’ve just been abducted by aliens!!!

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Presentation on theme: "Chapter 4 Rocks.  Why should I care? You’ve just been abducted by aliens!!!"— Presentation transcript:

1 Chapter 4 Rocks

2  Why should I care?

3 You’ve just been abducted by aliens!!!

4 What do I use to chop down trees with to build my new fortress? They’ve abandoned you on another planet. NOW WHAT?!?!?!

5  What kinds of rock will work?  What can I do to make the axe?  What else can I use rocks for?!?!?!  But first……..

6  It is a hard substance that is made of one or more minerals

7  Rocks are classified according to how they are formed. 1. Igneous Rocks – “fire formed” 2. Sedimentary Rocks - “sediment rocks” 3. Metamorphic Rocks - “changed rock”

8  The natural process of one rock type changing into another rock type.

9 Magma Igneous Rock Sediment Sedimentary Rock Metamorphic Rock Heat, Pressure, & Chemical Reactions Melting Cooling & Crystallizing Erosion & Weathering Cementing & Compacting

10  Rocks that are formed from magma (below) or lava (above)  Make up a large portion of the crust.

11  Based on composition and texture.

12  the size, shape, & relationships of the mineral crystals in a rock a.Coarse Grain - large crystals Granite Diorite

13 b.Fine Grain - small crystals c.Vesicular - full of holes because of gas bubbles PumiceBasalt Rhyolite Basalt

14 d.Glassy - cools too fast to form crystals e.Pyroclastic – cemented volcanic ash, cinders, & bombs Obsidian Scoria Pumice

15  Magma will cool and form mineral crystals at different temperatures.  Geologists can identify igneous rocks based on the specific minerals in the rock.

16 Ж Igneous rocks with fine grain texture are made from lava (Extrusive). ж Igneous rocks with coarse grain texture are made from magma (Intrusive).

17  Rocks formed by the cementing & compacting of small rock particles.

18 1. As rocks are broken down by water & wind (weathering/erosion,) the rock particles (sediment) will sink to the bottom of a water source.

19 2.Over a long period of time the sediment will build up in layers. The upper layers cause pressure on the lower layers (compacting.) ------physical process Pressure = compacting

20 3.In other cases, chemicals within the sediment will “glue” the sediment together forming a rock (cementing.) -----chemical process

21  Grouped based on how the rock was formed & where the sediment came from.

22  Sedimentary rocks that are made of previously existing rock fragments.  These rocks are named based on the size & shape of the rock fragments within the main rock.

23 EX: Sandstone & Shale Conglomerate Breccia Sandstones Shales

24  Includes rocks that were formed as a result of mineral crystallization when water evaporated. Ex:rock salt

25  Includes organic rocks such as coal & fossils  Includes cavernous rocks such as stalactites & stalagmites.  Includes microcrystaline quartz rocks

26 EX: Limestone & Flint Flint/Chert Limestones

27  A rock that has changed in form because of heat, pressure, and/or chemical reactions.

28  When a rock goes through a change it is called metamorphism.  Metamorphism can affect igneous and/or sedimentary rocks that are deep within the crust.

29  Heat will cause the minerals within the rock to break down to form more heat resistant minerals.  Pressure will force the minerals to rearrange themselves.

30  Chemicals within the rocks can alter or change the chemical make-up of the rock. Shale----------Slate Granite----------Gneiss Limestone--------Marble

31  Based on the arrangement of the grains within the rock.

32  Metamorphic rocks that have mineral crystals arranged in parallel layers or bands.  The rock tends to break along the bands.

33 EX: Schist, Gneiss, & Slate

34  Metamorphic rocks that are NOT banded and do NOT break into layers.

35 EX: Marble & Quartzite Marble Quartzite

36 How are rocks my friend in this situation?

37 To Do list: 1. Things I need to live: 1.


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