Sedimentary Rocks Flashcards
explain the rock cycle
ge tama yan
pre existing rocks that are formed by water as sediments
Sedimentary Rocks
How are sedimentary rocks formed
Compression and Compaction
Types of Sedimentary Rocks and give examples for each
clastic - baka di m pa masagot 2
chemical - limestone, dolomite
organic rocks - coal, plant fossils
Explain diagenesis
go beh kaya mo yan
Classification of Sedimentary Rocks (3) give examples
Rudaceous Rocks - Conglomerate, breccia
Arenaceous Rocks - Sandstone
Argillaceous Rocks - Shale
particle size of sediments from least to greatest
clay
silt
sand
gravel
pebble
Coarse grain size
Medium grain size
Fine grain size
5 mm
1 - 5 mm
1 mm
The deposition of the sediments in to layer or beds are called?
Stratification
The thin bedding less than 1 cm in thickness are called? Found in very fine grained rocks.
Lamination
Each bed shows a gradation in grain size from coarse below to fine above.
Graded bedding
In this structure minor beds or laminations lie at an angle to the planes of the general stratification
Cross bedding or current bedding
Are produced by the action of waves and current in shallow water
Ripple Marks
What causes the landscape to be different?
Weathering
Erosion
Deposition
The chemical and physical processes that change the characteristics of rocks on the Earth’s surface.
Weathering
Occurs when rocks are broken in to smaller pieces without changing the chemical composition of the rock.
Physical Weathering
Examples of physical weathering (4)
Frost Wedging
Exfoliation
Abrasion
Biological Activity
The breakup of rock caused by the freezing and thawing of water.
Frost Wedging (action)
is the peeling away of large sheets of loosened materials at the surface of a rock.
Exfoliation
The physical wearing down of rocks as they rub or bounce against each other.
Abrasion
Is where the rock material is changed into another substance by reacting with a chemical.
Chemical Weathering
Types of Chemical Weathering (3)
Oxidation
Hydration
Carbonation
When water interacts chemically with minerals
Hydration
When oxygen interacts chemically with minerals
Oxidation
When carbon dioxide interacts chemically with minerals
Carbonation