Classifying Sedimentary Rocks

HOW ARE THEY FORMED

WEATHERING

Igneous rock is broken down to form new minerals

DEPOSITION

Sediment accumulates in a deposit area from a source area

COMPACTION

The new minerals are overlayed, forcing
forcing grains together

CEMENTATION

Precipitation of mineral matter in the space of the grains
, holding the grains together

TYPES OF SEDIMENTARY ROCKS

CLASTIC

Form from weathering products that
don't dissolve in water

CLASTS

Large pieces of sand or gravel

MATRIX

Mud/ grained sediment surrounding
clasts

CHEMICAL SEDIMENTARIES

Form when mineral constituents in solution
become supersaturated and inorganically precipitate.

ORGANIC SEDIMENTARIES

Form from accumulation of organic debris (carbon containing)
Contain Calcite

PRODUCTS OF WEATHERING

CALCIUM CARBONATE/CaCO3

CLAY

QUARTZ

"Glue" holding the Clastic rocks together is either Calcite, iron oxide, or silica

CLASTIC ROCKS

CONGLOMERATES

SANDSTONES

SHALES

Stratification is a visible feature of
sedimentary rocks. They are the layers you can see as the different types of sediment

DOLOMITE
GYPSUM
LIMESTONE

COAL

SEBASTIEN SETO