a coarse-grained sedimentary rock made of rounded pebbles cemented together
Gritty can see grains, IMMATURE has many sizes, rounded lots of different minerals, stay where it started, greywacke, like conglomerate rocks MATURE has all the same size, angular, just quartz, traveled a lot, quartz sandstone, like breccia rocks
rock made of compressed clay
sedimentary rock made of organic materials
Made of calcite. You can often find fossils in them, fizzes with hydrochloric acid
fragments of rock that have settled and cemented
the process of things being made into rock, cemented the fragments or compressed under their own way
the consolidation of sediments resulting from the overlying deposits.
detrital clastic sedimentary rocks
rock in small particles or other material worn or broken away from a mass, as by the action of water or glacial ice. Rocks fragmented together
dirty sandstone (immature sandstone)
intermediate sandstone. Sandstone with feldspar
a pure quartz sandstone
sedimentary rock made of silt
larger particles than clay but smaller than sand
very soft limestone
porus limestone made of crushed shells (petrified granola)
is a very fine grained limestone that is used in lithography
layered limestone with holes in it
a very common mineral, calcium magnesium carbonate, CaMg(CO 3 ) 2 , occurring in crystals and in masses.
can hold grains together, quartz, 7 in hardness, lower class gemstones are made of this
is a fine grained chemical sedimentary rock made of silica; it is often associated with limestone. This material usually has a dull surface in contrast to the waxy appearance of flint.
is a chemical sedimentary rock of cryptocrystalline quartz; similar to chert but with a waxy surface. This material chips with a conchoidal fracture, making it an ideal material for creating arrowheads, spear points, and scrapers.
is a form of chert or flint that is strongly colored by iron oxides.
can be polished
Calcite, dolomite, gypsum, iron oxides, salt. When water evaporates, it creates these
is is the mineral halite, sodium chloride
calcium sulfate minerals, makes plaster o paris, and sheet rock, number 2 on hardness.
are a group of borate minerals formed as evaporites. Death Valley, California is a famous borax deposit.
organic material that has become rock
is dark brown to black organic debris left from plants that grow in swampy areas. It is the parent material for coal.
is soft, brown coal.
is soft coal.
is hard coal.
Primary Sedimentary structures
-are structural features found in sedimentary rocks that were created while the sediments were still unconsolidated. Examples include mud cracks, cross bedding, graded bedding, layering, ripple marks, etc.
...As mud dries out, some of the water between clay particles evaporates, causing the surface of the layer of mud to shrink and crack
...are layers of sedimentary rock
...is a primary sedimentary structure in which one set of inclined sedimentary layers is beveled off by an erosional process and a new set of sedimentary layers is deposited on top of the truncated original layers; this type of primary sedimentary structure is common in stream sediments and sand dunes.
...is a layer of sediment in which the largest particles occur at the bottom of the layer and grade upwards into finer materials
...are small parallel ridges of sand formed by flowing water or wind