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the peninsula is primarily made of limestone, a type of rock that easily dissolves in water. Over time, rainwater seeped through the limestone, creating underground channels and caverns through a process called karstification. This geological process is responsible for the formation of the caverns in the Yucatán Peninsula.
Tikal is made out of limestone, which is a sedimentary rock that can be easily carved and shaped. The limestone used in Tikal was sourced locally from quarries near the site.
Limestone is a rock that is easily dissolved by water, forming cavities and underground features like caves, sinkholes, and underground rivers. Over time, the natural processes of erosion and chemical weathering create these unique geological formations in limestone terrain.
Some sedimentary rock, like limestone, is susceptible to chemical attack from acidic rainfall due to its carbonate chemistry. Other sedimentary rock, like shale, is prone to freeze/thaw cycles due to the easily penetrated fractured layering. Sedimentary rocks like sandstone can be poorly cemented or porous, allowing for attack and disintegration by freezing or moving water, or dissolution of the cementing minerals.
Limestone would be potentially harder until the clay is fired. The problem we have here is that "clay" is an ambiguous term. There is no homogenous or standard formula for clay. However, clays can generally be formed and baked to become set and hard. This is called firing. Fired clay tends to be quite hard, and depending on the formula, might be harder than limestone.
It is called brittle.
A material that crumbles or breaks easily is often referred to as brittle. This means that it is prone to breaking, shattering, or crumbling under stress or pressure. Examples of brittle materials include glass and some types of ceramics.
Because limestone is a very intimmadate stone that you can break up easily.
Limestone is a rock that is about 10 percent of the total amount of all the rock formations. Limestone can be very soluble and tends to erode easily. When erosion starts the limestone can be crumbly.
Bedrocks such as limestone, dolomite, and gypsum are easily dissolved by running water due to their solubility in water. These rocks contain minerals that are easily weathered and dissolved, resulting in the formation of features like caves, sinkholes, and underground rivers.
Shale & Limestone !
Shale usually crumbles easily because it is composed of fine-grained clay minerals that lack cohesion. The rock's sedimentary nature means it has undergone compaction and cementation relatively less than harder rocks like sandstone or limestone. This makes shale prone to breaking into small pieces when stressed.
It has been, but limestone is prone to weathering, and is easily damaged by air pollution.
Limestone and chalk get easily weathered by acid.
Shale & Limestone !
Shale & Limestone !
Coal is easily seen as black. Limestone is usually gray. Coal has no real features to it. Limestone has shells, and other things.