Coal and coral reef limestone are organic sediments
salt is an evaporite
Sandstone and conglomerate are sedimentary deposit rocks the latter from a high energy environment.
They are ALL sedimentary deposits.
Some examples of lithified sediment are sandstone, shale, and limestone. Sandstone forms from grains of sand compacted together over time, while shale is formed from compacted clay and silt particles. Limestone is made predominantly of calcite that has accumulated and solidified in marine environments.
a sandstone would break more easily because a quartzite is harder. a quartzite is made of sandstone melted together by magma
To find an aquifer, you would typically need to look for rocks that are porous and permeable, such as sandstone, limestone, or fractured volcanic rock. These types of rocks allow for the movement and storage of water within their spaces, forming potential underground reservoirs from which water can be extracted.
As the water froze and expanded, it would exert pressure on the surrounding sandstone. This pressure could cause the sandstone to crack or fracture, as the ice expands and pushes against the rock material. Over time, repeated freezing and thawing cycles can lead to weathering and erosion of the sandstone.
No, Mount Rushmore is carved in granite, which is a harder and more durable type of rock than sandstone. Sandstone is much softer and would erode more quickly, making it a less suitable material for such a carving.
both would be a good building material because conglomerate is mixed with water and moisture mixed which makes it easier to stick and sandstone because its above conglomerate. :]
The rock type finer than conglomerate but coarser than siltstone is sandstone. Sandstone is a sedimentary rock composed mainly of sand-sized grains, which are larger than the particles found in siltstone but smaller than the pebbles and cobbles in conglomerate.
botany because it is a type of plant
Conglomerates.
In that scenario, you would most likely find the three basic types of clastic sedimentary rocks (conglomerate, sandstone, and shale) in the following order: conglomerate near the creek where larger sediment particles accumulate, sandstone in the transition zone between the creek and lake where medium-sized particles settle, and shale in the deeper parts of the lake where fine sediment particles settle.
Compaction would likely be more significant as a lithification process for shale and sandstone due to their fine-grained composition, which is conducive to compaction. Conglomerate and breccia are coarser and have less room for compaction due to their larger grain sizes and irregular packing.
Some examples of lithified sediment are sandstone, shale, and limestone. Sandstone forms from grains of sand compacted together over time, while shale is formed from compacted clay and silt particles. Limestone is made predominantly of calcite that has accumulated and solidified in marine environments.
A clump. Unless they have undergone compaction and cementation in a process known as lithification. Then they would be classified as a sedimentary rock, maybe conglomerate, breccia, or sandstone.
Conglomerate is a sedimentary rock that is composed of sever host rocks. These host rocks could be from very different environments, and from very far away. That is how you get two very different rocks within one conglomerate. the heat smelts them together
Sandstone
Conglomerate rock would be formed by the compaction and cementation of rounded pebbles.
WHich group would you classify -3