the creek dried up and made shale, then what could of happened is it made a layer of shale and later limestone formed and made a layer of limestone on top of shale
Clints are the blocks of limestone that remain standing between the grykes, which are the fissures or cracks in the limestone pavement. This formation can be found in limestone areas, particularly in regions with karst topography like the Yorkshire Dales in England or the Burren in Ireland.
Sandstone is primarily composed of sand-sized grains of minerals and rock fragments, while limestone is mainly made up of calcium carbonate from marine organisms like shells and coral. Sandstone forms from the accumulation and cementation of sand grains, while limestone forms from the compression and cementation of calcium carbonate-rich sediments.
Stalactites hang from the ceiling of caves and are formed by mineral-rich water dripping down, while stalagmites grow up from the floor of caves from the mineral deposits left behind by dripping water. Stalactites have a tapering icicle-like shape, while stalagmites are more mound-like and grow upward.
good question NOthign happens rock just getts crushed^Do not listen to guest post =/The answer to your question would be that the rate of reaction would increase.Limestone is ther remains of sea creatures that sunk to the bottom of the sea. After millions of years, the bodies decompse and create limestone. Limestone turns into marble. PS, I am 12, you should know this stuff
Gypsum and limestone are both sedimentary rocks, but they have different compositions and uses. Gypsum is made of calcium sulfate dihydrate, while limestone is primarily composed of calcium carbonate. Gypsum is commonly used in construction for drywall and plaster, while limestone is used in construction for buildings and roads.
Nothing happened. Formation immediately just became present day in an instant.
Nothing. Absolutely nothing has happened!
The Burren in Ireland is primarily composed of karst landscape made up of limestone rock. This unique geological formation includes limestone pavements, caves, and grykes, which are deep fissures between the rocks.
Clints are the blocks of limestone that remain standing between the grykes, which are the fissures or cracks in the limestone pavement. This formation can be found in limestone areas, particularly in regions with karst topography like the Yorkshire Dales in England or the Burren in Ireland.
1986 - Expo '86 Every four years Vancouver BC { british columbia} holds the winter olympics.
Gypsum is formed underwater, usually between layers of shale and limestone. When the water evaporates and the area dries, the gypsum becomes solid "rock" gypsum.
The color differences in limestone can be attributed to factors such as mineral content, presence of impurities, and environmental conditions during its formation. Minerals like iron can give limestone a yellow or brown tint, while organic matter can lead to gray or black hues. Various geological processes and the presence of different minerals contribute to the wide range of colors found in limestone.
classic rocks are not minerals. limestone is
Limestone
Gypsum is formed underwater, usually between layers of shale and limestone. When the water evaporates and the area dries, the gypsum becomes solid "rock" gypsum.
It is questionable due to the fact that there is no official timeline of Fraser Island.
Chemical limestone is synthetic and manufactured through chemical processes, often for specific industrial applications. Organic limestone, on the other hand, forms naturally from biological sources like shells and coral reefs, and is often used as a building material or in agriculture for soil improvement. Organic limestone may contain impurities from its natural formation, while chemical limestone can be tailored for specific composition and properties.