Types Of Rocks Flashcards
What do we use sedimentary rocks for?
Studies in Earth’s geological history.
Use of flint and chert as tools in the Neolithic Age.
Building materials – cathedrals and public buildings.
Fuel from oil, coal and natural gas in sedimentary strata.
Sand gravel and limestone in cement production.
Important store of groundwater.
Deposits of metallic (Copper, Uranium, Lead, Zinc, Gold) minerals and diamonds.
What are sedimentary rocks composed of?
Fragments of other rocks.
Chemical precipitates such as salt and gypsum.
Organic materials such as vegetation, coral and shells.
Define the terms strata, bedding planes and formations. As a part of your definition, link these terms together.
Strata (single layer) defines each layer of a sedimentary rock. These are separated by bedding planes indicating when deposition ceased temporarily. A formation is a combination of strata and covers a large area.
What is a fossil?
Evidence of former life (plant and animal).
Why are fossils more common in sedimentary rocks and not in the other two rock types?
Usually deposited by water as layers near the surface.
Less stress which might destroy the fossil.
Heat and pressure of igneous and metamorphic rocks might destroy the fossil and these usually occur at depth
Briefly describe the world distribution of sedimentary rocks.
Sedimentary rocks cover 75% of the continents and 100% of the ocean floor.
What are the two types of sedimentary rocks?
Clastic
Biochemical
Describe clastic sedimentary rocks.
Made from gravel, sand silt or clay.
Particles were carried to a site and deposited.
They are classified by grain size.
Describe biochemical sedimentary rocks.
Chemical processes move ions dissolved in water to make solid particles.
What are some different types of clastic sedimentary rocks?
Conglomerate
Sandstone
Mudrocks
Describe conglomerate.
Smooth and round.
Particle size >2mm.
Cemented by sand and mud.
Describe sandstone.
Sand grains of 0.6-2mm.
Mostly quartz grains.
Particles cemented by calcite, quartz and iron oxide.
Describe mudrocks.
Particle size
What are some different types of biochemical sedimentary rocks?
Limestones
Dolostones
Chert
Evaporites
Describe limestones.
CaCO3
Great variety of textures including skeletal.
Build up as a deposit when calcite precipitates through the grains, eg: chalk, oolitic and microcrystalline.
Inorganic limestones precipitated by springs, eg: travertine.
Describe dolostones.
Carbonate rock formed of dolomite.
Describe chert.
Composed of microcrystalline quartz occurring as irregular nodules in
limestone or as thin layers in marine sedimentary rocks.
Describe evaporites.
Formed when basins are subject to prolonged evaporation, e.g., halite and gypsum.
Explain the origin of sedimentary strata.
Sedimentary strata are deposited in layers or beds by water, wind or ice. Layers form in response to changes in deposition (changes in weather, seasons of climate).
Define and identify the causes of cross-bedding.
Cross-bedding occur when layers are angled to the upper and lower surfaces of the bed.
They are typically asymmetrical.
Dunes, deposited by wind, are the usual reason for cross-bedding.
Describe sediments which are graded.
Beds which are graded start as large particles and particle size decreases upwards through the bed.
What is turbidity and how does it affect sediments?
Turbidity is produced by the variation in density between a current and the surrounding water.
The faster flowing turbid current loses velocity and grades its deposition from coarse to fine particles.
Distinguish between fossils and trace fossils.
A fossil is the biological remains of a pre-historic creature or plant.
Trace fossils are is a preserved remnant of a track, burrow or cocoon made by an extinct animal.