Deep ocean deposition is the norm for the bulk of limestone formation, although seepage in caves also creates limestone structures, as well as shallow water coral reefs, and hydrothermal surface structures.
shallow, clear, marine waters with vigorous current activity
This is because in the wet climates the limestone will break apart due to the rain. And in dry climates it does nothing to the limestone. Therefore, this is why limestone can form cliffs in dry climates than wet climates.
Marble is one form of metamorphosed limestone.
marble
marble
shallow, clear, marine waters with vigorous current activity
Limestone caves are formed through a process called karstification, where rainwater picks up carbon dioxide from the air and soil, creating a weak carbonic acid. This acidic water dissolves the limestone rock over time, creating underground cavities and passages. As the water drains away, it leaves behind caves and unique formations such as stalactites and stalagmites.
Chemical limestone can form when calcite is dissolved.
it rains and sinks into limestone and over to starts to corrode at the vulnerable limestone
This is because in the wet climates the limestone will break apart due to the rain. And in dry climates it does nothing to the limestone. Therefore, this is why limestone can form cliffs in dry climates than wet climates.
Marble is one form of metamorphosed limestone.
limestone forms from skeletons and shells
Limestone can be formed partly or mostly by visible shell fragments. .
Although limestone can form into other types of metamorphic rock, the most common form is marble.
Limestone - sedimentary deposition of calcarious marine organisms. Marble - compressed (metamorphosed) limestone.
marble
Grikes form when limestone is dissolved by water.