Download presentation
Presentation is loading. Please wait.
Published byQuentin Williamson Modified over 9 years ago
1
Place your paper on your desk landscape style.
2
Do a burrito fold (dividing the paper into thirds).
3
Do another burrito fold (dividing the paper into thirds again).
4
When you unfold, it should look like this.
5
Turn your paper to the side as shown and cut on the folds.
6
Cut both folds.
7
Cut through the folds on second flap also.
8
Now divide the top inside flap in half by cutting down the middle.
9
Cut the middle inside flap into THIRDS by making 2 cuts- dividing the flap into 3 equal spaces.
10
Cut the bottom inside flap in half by cutting a line down the middle.
11
Close it all up- turn it to where it opens like a book. Label as shown- Igneous, Sedimentary, Metamorphic
12
Open small flaps 1 at a time & draw lines to separate areas
13
Should look like this when you are done drawing lines to separate areas.
14
Form when molten rock (magma or lava) cools & hardens intrusive extrusive
15
Magma cools and hardens below Earth’s surface Coarse grained Large crystals Ex: Granite
16
Magma reaches the surface as lava, then cools and hardens quickly Fine grained Small crystals Ex: Pumice, Obsidian
17
Existing rock weathers, sediment erodes. Deposition in layers. Then compaction & cementation form rock clastic chemical Non-clastic/organic
18
Made up of smaller pieces of rock Sandstone- used in buildings Shale- used in ceramic tile
19
Coal- used for energy Limestone- fossiliferous Organic- made from remains of living organisms
20
Calcite Limestone walls- building material, glass & paint Dissolved minerals are deposited as water evaporates
21
When mineral crystals in existing rocks are changed by heat & pressure Non-foliated Foliated
22
Gneiss Slate Have visible layers or bands
23
Quartzite Marble Uniform throughout (no layers)
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.