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Marine Sediment Rocks: Definition, Types, and Examples

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There are various types of rocks that make up the skin layer of the Earth. Some are called igneous rocks, some are called sedimentary rocks. Sedimentary rocks are rocks that we can easily find on the surface of the Earth. Weathering of rocks, both chemical weathering and mechanical weathering contribute to the formation of sedimentary rocks.


Rocks that have undergone weathering will usually be carried away by water or other transport media so that they settle somewhere. According to where it settles, sedimentary rocks can be divided into several types. One of them is marine sedimentary rocks. What are marine sedimentary rocks? The following are the definition, types, and also examples of marine sedimentary rocks.

Definition of Marine Sedimentary Rocks

Marine sedimentary rocks are one of the types of sedimentary rocks formed in the ocean or ocean environment. In addition, marine sedimentary rocks can also be defined as rocks which sedimentation processes are caused by the presence of energy or waves of sea water. Weak or strong sea waves will form different marine sedimentary rocks which will then be explained in marine sedimentary rock types.

Types of Marine Sedimentary Rocks

Based on the ocean where rocks are formed, marine sedimentary rocks can be classified into two types, namely rocks formed in shallow seas and sedimentary rocks formed in the deep sea. Here are the explanations.

Shallow Sedimentary Rocks

Shallow sea is an area of ​​marine waters that is no more than 200 meters below sea level. Shallow seas have currents that are stronger than the deep sea’s. This is influenced by its location close to the surface. There are many things that cause the magnitude of the current, including sea breeze and large waves that hit the coast.

The amount of energy in the shallow sea results in sedimentary rocks formed in the environment having a rough structure. The shallow sea also allows sunlight to penetrate the sea floor. It is used by marine biota to form a shell frame. Shells of marine animals are rich in carbonate minerals. When the marine animals die, the shells will accumulate and settle in a place so that rocks are formed.

Deep Sea Sedimentary Rocks

Contrary to the shallow sea, the deep sea is an area of ​​water that is more than 200 meters deep. Weak deep ocean currents only allow to transport fine particles. This results in rocks that settle on the deep sea floor having a smooth structure. In the ocean zone called isocline, the presence of carbonate is as much as it is.

The carbonate is then dissolved so that it cannot form reef rocks in the deep sea. However, the shell of marine biota containing silica will not dissolve and form radio lite rocks. The sudden disturbance in the deep sea zone results in sudden amounts of sedimentation. The type of rock that undergoes deposition is of course a fine structure, such as silt and sand.

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Examples of Marine Sedimentary Rocks

Some examples of marine sedimentary rocks that form in deep seas and shallow seas are:

  • Coral reef

As explained earlier that precipitation that occurs in shallow seas will form rocks. Coral is better known as coral reefs. This stone is composed of calcium carbonate minerals or lime minerals.

Limestone is a place where the coral attaches, which in biology there are live corals and dead corals. What is meant by live coral is a group of animals that can produce lime as the main ingredient in the formation of reefs. Its habitat is in a shallow sea that can be penetrated by sunlight. While a collection of dead corals is called a rock.

(Also read: 17 Importance of Marine Microbiology)

  • Sandstone

Sandstone is an example of sedimentary rock that is found in many coastal ecosystems which are still included in shallow marine environments. Sandstone on the beach is generally gray, white and light brown. This sandstone transport media is usually a wave of sea water and sea breeze. Sandstone has a small grain size, which only ranges from 0.1 – 2 mm only. The minerals that make up the sandstone are quartz, feldspar, basalt, rhyolite, chlorite, and iron ore.

  • Salt Stone

Salt stone is one example of sedimentary rocks formed in the ocean. The deposition area usually occurs around lagoons and bays. This stone is composed of mineral halite (NaCl). The process of forming sedimentary rocks is caused by the evaporation of seawater which contains many positive ions of sodium and negative ions from chloride. Salt stone has a white and brownish white color. Some areas that are commonly found in salt rock are Michigan, Jordan, and Ethiopia.

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Natural Appearance due to Deposition of Marine Sedimentary Rocks

Sedimentation of marine sedimentary rocks, especially sandstone in a place will form certain natural features, including:

  • Tombolo

One of the natural features caused by sandstone sedimentation is tombolo. Tombolo can be defined as a levee formed from sandstone that occurs naturally and becomes a link between land and islands located close to the coast. In general, tombolo is formed in the sea of ​​money having a bay without interference with ocean currents.

Tombolo does occur naturally, although there is a tombolo that is intentionally made to bridge the two islands. The process of formation begins with the presence of large waves originating from the deep sea towards the shallow sea. Sea waves then experience refraction due to the sholing effect. These waves carry the sand to the same place continuously so that a tombolo is formed which adds to the length of the coastline.

(Also read: 17 Importance of Ocean Sediments)

  • Sandbar

Sandbar is a land in the form of sand that juts into the waters of the sea. From this definition it can be seen that charred formed from sandstone that is collected into one form the land. The occurrence of sandbar is caused by the flow of currents in the shallow sea. Sandbar has an elongated shape with a length of hundreds of kilometers, while its thickness can reach six spears. If the tide is high, then the sand can be sunk by sea water. One of the seas in Indonesia that has many sandbanks is the Java Sea in the north of Java.

Those are the beauties of the life underwater. After reading this articles, you can know more about how marine sediment rocks formed and many types of it. Underwater is always success to impress us, isn’t it?

Post Date: Wednesday 13th, March 2019 / 09:12 Oleh :
Kategori : Environment