sedimentary rocks

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Page 1: Sedimentary rocks
Page 2: Sedimentary rocks

Weathering Erosion Deposition Compaction Cementation

*LITHIFICATION*

Page 3: Sedimentary rocks

Weathering – the breakdown of material at the Earth’s surface.g

The weathered material is calledSEDIMENT.

Page 4: Sedimentary rocks

Sediment size varies – mud, sand, gravel

Page 5: Sedimentary rocks

Erosion – movement of sediment from on place to another by WIND, WATER, or ICE.

Page 6: Sedimentary rocks

Deposition – dropping off the sediment in a new location.

Page 7: Sedimentary rocks

Sediment gets put together into sedimentary rock through

Compaction (Squeezing)

Cementation (Gluing)

Page 8: Sedimentary rocks

Sand becomes sandstone

Page 9: Sedimentary rocks

Clay and mud become shale

Page 10: Sedimentary rocks

Gravel becomes conglomerate.

Page 11: Sedimentary rocks
Page 12: Sedimentary rocks

Organic sedimentary rock is formed from previously living things.

Limestone – ocean life

Coal – plant life on land

Page 13: Sedimentary rocks

Chemical sedimentary rock is formed from water evaporating and leaving rocks behind.

Page 14: Sedimentary rocks

Mineral crystals left behind in Death Valley after the water evaporates

Playa Lake in California – in the process of evaporating and leaving chemical rock behind

Page 15: Sedimentary rocks

Sedimentary rocks are used in many ways – •Buildings•Making cement•Burning for fuel