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Sedimentary Rock Classification. Rock cycle What are Sedimentary Rocks?  What are sediments?  How do sediments form sedimentary rocks?  Where do sedimentary.

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Presentation on theme: "Sedimentary Rock Classification. Rock cycle What are Sedimentary Rocks?  What are sediments?  How do sediments form sedimentary rocks?  Where do sedimentary."— Presentation transcript:

1 Sedimentary Rock Classification

2 Rock cycle

3 What are Sedimentary Rocks?  What are sediments?  How do sediments form sedimentary rocks?  Where do sedimentary rocks form?

4 General Features  sedimentary rocks usually come from SEDIMENTS (mud, sand, pebbles, etc.)  sediments are pressed into layers (strata)

5 Ernst Tinaja Big Bend National Park

6 Ernst Tinaja  Thin-bedded orangish rock = Del Rio Clay,  Stratigraphically just below the Buda Limestone  The massive white rock below the Del Rio is the Santa Elena Limestone  Time lapse between the deposition of the Santa Elena and the Del Rio = unconformity

7 Formation  sediment comes from the weathering and erosion of other rocks  wind and water move sediment

8 Formation ctd.  once sediments are settled, lithification (making a rock) begins  lithification can involve two main processes:  compaction: sediments are pressed together by weight, and water is forced out  cementation: minerals deposit out of water and “cement” together sediments

9 Rock Cycle

10 Types of Sedimentary Rocks: 1. Clastic  clastic rocks come from broken pieces of other rock (as was just described)  they are further classified according to their pieces

11 Clastic Rocks ctd.  conglomerates have large, round, pieces (see last slide)  breccias have large, angular pieces  clastic rocks from smaller pieces can be sandstones or mudrocks  Shale

12 2. Organic Rocks  form directly or indirectly from living material (despite our definition of minerals)  example: limestone is calcium carbonate from the shells of dead clams and oysters

13 3. Chemical Rocks  form by chemical processes (not regular compaction)  Limestone: a. grainstone b. boundstone  “evaporites” form when water evaporates, leaving just minerals  ex: gypsum, halite, and even some limestone are from evaporating water

14  Tools of a Geologist Grain size scale Roundness scale Hand lens  Field notebook Make good observations and notes FIELD GEOLOGY

15 Summary Questions  What might tip you off that you’re looking at a sedimentary rock?  What are two ways that limestone can form?  How are chemical rocks different from other sedimentary rocks?


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