The awnser is limestone. If you want to look it up look for the peirson succeess science book it's either grade3 or four
Basalt does not belong because it is an igneous rock formed from volcanic activity, while shale, sandstone, and limestone are sedimentary rocks formed from different processes such as compression of sediment or accumulation of organic materials.
Sandstone can metamorphose into quartzite.
Sedimentary Rocks. Sedimentary rocks are created from stratification by the layering of materials on one another which then get compacted and cemented by sedimentation process over long period of time. The whole process of formation of sedimentary rocks from sediment is called Diagnesis. Examples of sedimentary rocks are limestone, chalk, and sandstone.
Limestone or Sandstone are two examples of sedimentary rocks. Two examples of sedimentary rocks are slate (fine silt) and chalk (shell remains of sea creatures).
Limestone is a sedimentary rock.
Basalt does not belong because it is an igneous rock formed from volcanic activity, while shale, sandstone, and limestone are sedimentary rocks formed from different processes such as compression of sediment or accumulation of organic materials.
Limestone is not classed as either a granitoid or a sandstone rock. Limestone is a sedimentary rock, either chemically precipitated or bioclastic in origin. Granite is a plutonic igneous rock, and sandstone, although sedimentary, is formed from the cementation of sand-sized particles of eroded rock.
Limestone, shale, and sandstone are all sedimentary rocks formed through the accumulation and compression of sediments. They are all composed of mineral particles such as quartz, calcite, and clay minerals. Additionally, these rocks are commonly used in construction and as building materials due to their durability and strength.
Sedimentary rocks. Example, sandstone.
Sandstone can metamorphose into quartzite.
Sedimentary rock is the rock formed as a result of deposits from weathering and erosion. Sedimentary rock can be millions of years old.
Sedimentary Rocks. Sedimentary rocks are created from stratification by the layering of materials on one another which then get compacted and cemented by sedimentation process over long period of time. The whole process of formation of sedimentary rocks from sediment is called Diagnesis. Examples of sedimentary rocks are limestone, chalk, and sandstone.
Limestone or Sandstone are two examples of sedimentary rocks. Two examples of sedimentary rocks are slate (fine silt) and chalk (shell remains of sea creatures).
Sedimentary rocks are formed when sediments are compressed, compacted, and cemented together. Examples include sandstone, shale, and limestone.
There are many different kinds of sedimentary rock. Four examples of this type of rock are shale, sandstone, limestone and coquina.
Rocks formed from sediment deposits are called sedimentary rocks. They are formed from the accumulation and lithification of sediment, which can include fragments of pre-existing rocks, minerals, and organic material. Examples include sandstone, shale, and limestone.
Shale, sandstone, and limestone belong to the sedimentary rock group. Sedimentary rocks are formed by the accumulation and compression of sediment over time. Shale is a fine-grained rock formed from clay and silt; sandstone is made up of sand-sized grains cemented together; and limestone is primarily composed of calcite from marine organisms.