No oolitic limestone is mostly calcium carbonate with some spar cement,but sandstone is mostly quartz but with all sorts of weathered products of other preexisting rocks with size within the range of 1/16mm to 4mm
Limestone is porous and can absorb water, while sandstone is also porous but less absorbent than limestone. Granite is a denser and less porous rock, so it does not absorb water as readily as limestone or sandstone.
Grain size is more important for determining the classification of clastic sedimentary rocks, such as sandstone or shale. Composition is more important for determining the classification of chemical sedimentary rocks, such as limestone or rock salt. Layering is more important for identifying the structure of sedimentary rocks, such as bedding in sandstone or shale.
Yes, crushing limestone is a physical change. This is because the chemical composition of limestone remains unchanged during the process of crushing. The size and shape of the limestone particles may change, but the chemical makeup remains the same.
Granite particles are interlocked as the minerals formed from the slow cooling of molten material. Sandstone does not have the same interlocking crystal system, and voids between particles are generally larger.
== == The "coarseness" of a sedimentary rock refers to the rock's textural character, and more particularly, the size of grains contained within it. Thus, a conglomerate containing pebble or cobble clasts is coarser than a sandstone containing sand grains. In the same way, a conglomerate containing boulders is coarser than a conglomerate containing pebbles. Clastic sedimentary rocks are classified using the Wentworth Scale. The coarsest elements of this scale are the Rudites. Boulder rudites are conglomeratic rocks with grains of diameter greater than 256mm. They are the coarsest element described on the Wentworth Scale. There is no upper limit to the scale of sedimentary coarseness, since the size of clast which can be preserved in a sedimentary rocks is potentially very large. 'Olistolith' is a term which describes very large clasts often derived from the sub-sea collapse of oversteepened slopes such as are found at continental margins. Sediments containing olistoliths may reasonably be described as the coarsest sedimentary rocks.
Limestone is porous and can absorb water, while sandstone is also porous but less absorbent than limestone. Granite is a denser and less porous rock, so it does not absorb water as readily as limestone or sandstone.
No, sandstone can vary in size depending on the specific composition of minerals and grain size. Sandstones can have a range of grain sizes from very fine to coarse. The size of the sand grains in the sandstone will impact its appearance and texture.
Sandstone is a sedimentary rock made up of sand-sized mineral particles, mainly quartz and feldspar, cemented together by a matrix of silica, calcite, or iron oxide. Limestone, on the other hand, is a sedimentary rock primarily composed of calcium carbonate minerals. In the laboratory, you can differentiate between the two rocks by performing acid tests - limestone will fizz and dissolve in acid due to its calcium carbonate content, while sandstone will not react in the same way.
Limestone and sandstone are both sedimentary rocks. Therefore, they are rocks that were once other rocks, then they were eroded and weathered, so small sediments were broken off, and then they were deposited and compacted or cemented, and turned into a new rock! That is the case for sandstone (sandstone is just sand very finely compacted and cemented by minerals to form the rock. It is formed in slowish moving waters like oceans). However, limestone is one of the exceptions. Limestone instead of being sediments that were eroded, it is made up of dead marine life and shells. It turns into the metamorphic rock marble when it is metamorphosed. To answer your question simply, what they both have in common is they are sedimentary rocks.
The great pyramid was the color of Oolitic limestone- a kind of honey color. When it was built, the outside was covered in a layer of polished white fine grained limestone, but had been removed later to build Cairo
The chemical composition of the limestone cobble remains the same when subjected to abrasion, as the mineral content does not change. However, the physical appearance and shape of the cobble will be altered due to the abrasion, resulting in smoother surfaces and potential changes in size and shape.
Grain size is more important for determining the classification of clastic sedimentary rocks, such as sandstone or shale. Composition is more important for determining the classification of chemical sedimentary rocks, such as limestone or rock salt. Layering is more important for identifying the structure of sedimentary rocks, such as bedding in sandstone or shale.
Yes, crushing limestone is a physical change. This is because the chemical composition of limestone remains unchanged during the process of crushing. The size and shape of the limestone particles may change, but the chemical makeup remains the same.
The erosion of sandstone is considered a physical change because it involves the breaking down of the solid sandstone through processes like wind, water, and temperature fluctuations, without altering its chemical composition. The particles of sandstone are physically worn away but remain the same in terms of their chemical structure.
It is made of limestone and wood. Wait is wood a rock, is that your question. Oh yeah and t is also made of Portland rock. Which is very similar to limestone.....it may even be the same thing but who knows?? :\ :]
Marble is made from limestone.
No, not all stones are the same. Stones can vary in composition, hardness, color, and origin. Different types of stones, such as granite, marble, quartz, and sandstone, have unique characteristics that make them suitable for different uses and applications.