how do sedimentary rocks form? by j. piccirillo. for thousands, even millions of years, little...
TRANSCRIPT
• For thousands, even millions of years, little pieces of our earth have been eroded--broken down and worn awayby wind and water (ice included).
• These little bits of our earth are washed downstream by
( E…. )where they settle to the bottom of the rivers, lakes, and oceans.
• These layers are pressed down ( ) more and more through time, until the bottom layers slowly turn into rock.
• While compacting, these sediments are also glued
( ) together by dissolved minerals oozing from the sediments
• Later on through many years of Earth moving upward or seas retreating or evaporating the compacted sediment turns into Hard Rock when exposed above the earth’s surface.
http://www.classzone.com/books/earth_science/terc/content/investigations/es0602/es0602page02.cfm?chapter_no=investigation
• Conglomerates• Breccia• Sandstones• Siltstones• Shale/mudstones
TYPES OF SEDIMENTARY ROCKS
Clastic rocks Chemical & Organic rocks
Evaporitic rocks
These rocks are formeddue to evaporation of saline water (sea water)eg. Gypsum, Halite (rock salt)
Carbonate rocks
Form basically from CaCO3 (Calcite) – both by chemical leaching and by organic source (biochemical) eg. Fossil Limestone; Dolostone (MgCO3)
Organic rocks
Form due to decomposition of organic remains under temperature and pressure eg. Coal/Lignite etc.
• Formed from broken rock fragments weathered and eroded by river, glacier, wind and sea waves. These clastic sediments are found deposited on floodplains, beaches, in desert and on the sea floors.
CLASTIC ROCKS
Clastic rockssolidify
• Clastic rocks are classified on the basis of the grain size: conglomerate, sandstone, shale etc.
GRAIN SIZE
Gravel< 256 - 2 mm
Sand2- 0.062 mm
Clay<0.0004 mm
Silt0.062 - 0.0004 mm
Boulder: >256mm
Cobble: 64-256 mm
Pebble: 4-64 mm
Granule: 2-4mmFine gravel
Non- Clastic or Chemical or Crystalline EVAPORITIC ROCKS
These rocks are formed within the depositional basin from chemical substances dissolved in the seawater or lake water.
GypsumHalite
(NaCl)CaSO4.2H20
Economic importance of Evaporites
• SALT: other then daily use of salt for cooking, it is used
• For production of Paper,• Soap• Detergents• Antiseptics• As chemical for dyeing etc.
• GYPSUM: is used for plaster and in manufacturing construction materials.
• Limestone: It is a non-clastic rock formed either chemically or due to precipitation of calcite (CaCO3) from organisms usually (shell). These
remains will result in formation of a limestone. • Limestones formed by chemical precipitation are
usually fine grained, whereas, in case of organic limestone the grain size vary depending upon the type of organism responsible for the formation
-Chalk: which is made up of foraminefera is very fine grained
-Fossiliferous Limestone: which medium to coarse
grained, as it is formed out of cementation of Shells.
Non- Clastic CARBONATE ROCKS
• used as a building stone and in the manufacture of lime, carbon dioxide, and cement.
• Massive and compact lst. Are competent to support CE-structure
• However, if it occur in huge thickness then it is not advisable, because of its typical CAVING character.
Chalk
Limestone - chemical variety..from precipitated calcite out of seawater.. deposited on the bottom beds of evaporated seas and lakes and from sea animal shells