How good your physical geology is? Do you know an overview of sedimentary rock? If all your answer is yes, then take up the quiz below and check how sharp your memory is. Sedimentary rocks are formed by the deposition of the mineral particles at Erath's surface. The most common form of these rocks is chalk, limestone, clay, and shale. The following quiz consists of some basic questions related to sedimentary rocks. If you know enough about these rocks, try the quiz and see for yourself.
Uplift, folding, and subsidence
Molten rock material gluing particles together
Deposition, cross-cutting, inclusion, and continuity
Weathering, transport, deposition, and lithification
Feldspar resists transport
There is more quartz produced in the mountains
Feldspar breaks down chemically more easily than quartz
Feldspar is pink and white, quartz is clear
Oxidation in cold climates forces cracks to widen
Water expands 9% when it freezes and widens cracks in rocks
Rocks fall into gaps and wedge apart talus
Minerals expand at different rates when heated
Tends to reduce the rate of chemical weathering
Does not affect the rate of chemical weathering
Chemical weathering and mechanical weathering are independent of each other
Tends to increase the rate of chemical weathering
They expand when frozen
They combine to form carbonic acid which dissolves rocks
They reduce the space needed for limestone crystals causing the rock to fall apart
They convert the limestone to marble
Pyroxene
Quartz
Olivine
Potassium feldspar
Rhyolite
Basalt
Andesite
Granite
Feldspar, biotite and ions
Quartz, clay and ions
Pedalfers, pedocals and laterites
Calcite, halite and iron
A horizon
B horizon
O horizon
C horizon
A horizon
C horizon
O horizon
B horizon
A rock made of coal
A rock that forms from a melt
A rock made of particles cemented together
A rock that is made of elements precipitated in the ocean
Particles rolling, sliding, and bouncing on the bottom
Dissolved material
Particles suspended in the water column
Ions suspended in the water column
1/16 – 2 mm
64 – 256 mm
2 – 64 mm
1/256 – 1/16 mm
Flow in which streamlines do not cross
Flow with extensive mixing of fluid
Flow in which streamlines cross
Flow that is chaotic
Sand and silt
Large particles and cohesive clays
Sand
Silt
Ions in solution
Large particles that are rolling on the bottom
Larger particles that bounce along the bottom
Fine particles that are dispersed in the flow
The degree to which sediment grains resemble spheres
A measure of the sharpness of a particle's edges and corners
The largest grain size in a sample
The range in grain sizes
Contains abundant olivine
Has little or no quartz
Probably had not been transported far
Contains mostly quartz grains
Chemically immature
Angular
A type of bedding
A siliciclastic rock that only contains silt
Sand
Pebbles
Clay
Gravel
Wavy ridges in sediments
Flat layers in sedimentary rocks
Units that are coarser at the top and finer at bottom
Layers tilted with respect to the main layer
There was a water current
Deposition was very fast
It periodically dried out
It was at the bottom of a lake
A rock made of particles, mostly quartz and clay
A rock made from ions that were concentrated and precipitated
A type of quartz
A rock made of clay
Limestone
Chert
Rock salt
Coal
In warm water far from a clastic source
Near mountains that provide food
In cold shallow water with a strong undertow
Near the mouths of major rivers
Wait!
Here's an interesting quiz for you.