Geology Reference
In-Depth Information
Sediment
Process
Rock
Gravel > 2 mm
Compaction/cementation
Conglomerate
Rounded clasts
Sedimentary
breccia
Angular clasts
Sand 2 mm- 16 mm
Compaction/cementation
Quartz sandstone
(mostly quartz)
Sandstone
Arkose
(> 25% feldspars)
1
1
Silt
16 mm -
256 mm
Compaction/cementation
Siltstone
Mostly silt
1
Mudstone
Silt and clay
Clay <
256 mm
Compaction
Shale if
fissile*
Claystone
Mostly clay
*Fissile refers to rocks capable of splitting along closely spaced planes.
Figure 6.18 Lithifi cation and Classifi cation of Detrital Sedimentary Rocks Notice that little
compaction takes place in gravel and sand.
TABLE 6.2
Classifi cation of Chemical and Biochemical Sedimentary Rocks
Chemical Sedimentary Rocks
Texture
Composition
Rock Name
Varies
Calcite (CaCO 3 )
Limestone
Carbonate rocks
Varies
Dolomite [CaMg(CO 3 ) 2 ]
Dolostone
Crystalline
Gypsum (CaSO 4 ·2H 2 O)
Rock gypsum
Evaporites
Crystalline
Halite (NaCl)
Rock salt
Biochemical Sedimentary Rocks
Clastic
Calcite (CaCO 3 ) shells
Limestone (various types, such as chalk and coquina)
Usually crystalline
Altered microscopic shells of SiO 2
Chert (various color varieties)
Carbon from altered land plants
Coal (lignite, bituminous, anthracite)
gravel has experienced little transport, probably less than
a kilometer. Considerable energy is needed to transport
gravel, so conglomerate is usually found in environments
such as stream channels and beaches.
Sand is a size designation for particles between 1/16
and 2 mm, so any mineral or rock fragment can be in
sandstone. Geologists recognize varieties of sandstone
based on mineral content (Figure 6.18). Quartz sandstone
is the most common and, as the name implies, is made up
mostly of quartz sand. Another variety of sandstone called
arkose contains at least 25% feldspar minerals. Sandstone
is found in many depositional environments, including
stream channels, sand dunes, beaches, barrier islands,
deltas, and the continental shelf.
Mudrock is a general term that encompasses all detrital
sedimentary rocks composed of silt- and clay-sized particles
 
 
 
 
 
 
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