Geology 101 - Introduction to Physical Geology
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Sedimentary Rock Classification Table
Clastic Sedimentary Rocks
Grain Size Rounding Sorting Rock Name
gravel
coarse
(> 2 mm)
angular poorly breccia
rounded poorly conglomerate
sand
medium
(0.0625 - 2 mm)
variable variable sandstone
rounded to subangular well to moderately quartz arenite - >90% quartz
subrounded to angular well to moderately arkose - >25% feldspar
subangular to angular moderately to poorly graywacke - high % lithics, clay matrix
silt
fine
(0.004 - 0.0625 mm)
variable well siltstone
clay
extra fine
(< 0.004 mm)
not visible well shale - breaks along bedding planes
mudstone - lacks bedding planes
claystone - pure mineral clay, very soft
Chemical Sedimentary Rocks
Mineral Distinguishing Characteristics Rock Name Common Depositional Environment
calcite softer than glass, reacts to HCl limestone warm shallow ocean
calcite visible fossils, softer than glass, reacts to HCl fossiliferous limestone warm shallow ocean
dolomite white to pink, softer than glass, reacts to HCl only when powdered dolostone saline lagoon
calcite gray or brown, porous, reacts to HCl travertine evaporated spring or cave water
calcite white, powdery, reacts to HCl chalk warm shallow ocean
microscopic quartz conchoidal fracture chert deep ocean floor
microscopic quartz red, conchoidal fracture jasper deep ocean floor
microscopic quartz black, conchoidal fracture flint nodules in limestone
microscopic quartz translucent, layered, conchoidal fracture agate nodules in volcanic rocks
microscopic quartz white, powdery diatomite lakes in volcanic environments
carbon black, soft, low density coal heavily vegetated swamp
halite tastes like salt, cubic crystals and cleavage rock salt evaporating water body
gypsum softer than fingernail gypsum rockevaporating water body

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Geology 101 - Introduction to Physical Geology
Basics Table--Sedimentary Rock Classification
Created by Ralph L. Dawes, Ph.D. and Cheryl D. Dawes, including figures unless otherwise noted
updated: 9/16/13

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