From Fiery Origins to Earthly Layers: The Transformation of Igneous Rock into Sedimentary

How does an igneous rock become sedimentary?

1. An Introduction

Igneous rocks are formed from solidified magma or lava that cools and crystallizes. They are typically found deep within the Earth’s crust or on the surface as volcanic extrusions. Over time, however, igneous rocks can undergo various processes that transform them into sedimentary rocks. This transformation occurs through a series of geologic processes such as weathering, erosion, transport, deposition, and lithification. In this article, we will explore these processes and understand how igneous rocks can become sedimentary rocks.

Sedimentary rocks, unlike igneous rocks, are formed by the accumulation and cementation of sedimentary particles derived from pre-existing rocks or organic materials. The transformation of igneous rocks to sedimentary rocks involves the breakdown of the original rock, transport of the resulting sediment, and subsequent deposition and lithification processes. Let’s take a closer look at each of these processes to better understand how igneous rocks become sedimentary rocks.

2. Weathering

Weathering is the first step in the transformation of igneous rocks into sedimentary rocks. It refers to the physical and chemical processes that break the rock into smaller fragments or particles. There are two main types of weathering: mechanical weathering and chemical weathering.

Mechanical weathering involves the physical breakdown of rocks into smaller pieces without changing their chemical composition. It occurs due to various factors such as temperature changes, freeze-thaw cycles, wind abrasion, and the action of plant roots. When igneous rocks are exposed to these forces, they gradually disintegrate into smaller fragments.

Chemical weathering, on the other hand, involves the alteration of the chemical composition of the rock through chemical reactions. Water, atmospheric gases, and organic acids can react with the minerals present in the igneous rock, causing them to break down and form new minerals. Over time, these chemical reactions weaken the structure of the rock, making it more susceptible to erosion.

3. Erosion and Transportation

Once the igneous rock is weathered into smaller particles, the next step is erosion and transport. Erosion is the process by which weathered rock fragments are loosened and removed from their original location. This can occur through the action of water, wind, ice, or gravity.

Water is an important agent of erosion and plays a critical role in transporting sediment. Rivers, streams, and ocean currents can carry the weathered rock particles away from their source areas. This transport process causes the sediments to be sorted and separated based on their size, shape, and density. Heavier particles settle out more quickly, while finer particles can be carried over long distances.

As the sediment is transported, it undergoes further physical and chemical changes. Particles may collide with each other, become rounded or smoother, and even undergo additional weathering processes. These changes contribute to the eventual formation of sedimentary rocks.

4. Deposition

Deposition is the process by which transported sediment settles and accumulates in a new location. When the transport agents, such as rivers, wind, or glaciers, lose their energy, they can no longer carry the sediment particles, causing them to settle and come to rest. The sediment is then deposited in different environments such as riverbeds, lakes, deltas, or ocean basins.

During deposition, different sediment particles are sorted according to their size and density. Coarser and denser materials tend to settle first, while finer particles may be carried further before finally coming to rest. This sorting process leads to the formation of distinct layers or beds of sediment called strata.

5. Lithification

Lithification is the final step in the transformation of sediment into sedimentary rock. It involves the compaction and cementation of the deposited sediment to form a solid rock mass. Compaction occurs as the weight of the overlying sediment compresses the lower layers, reducing the pore space between the particles. This pressure causes the sediment to become more densely packed and reduces the amount of water between the grains.
Cementation is the process by which minerals precipitate from the groundwater and fill the remaining pore spaces between the sediment particles. These cementing minerals, such as silica, calcium carbonate, and iron oxides, act as a binder, holding the sediment particles together and transforming them into a cohesive rock mass.

Over time, with increasing pressure and growth of cementing minerals, the sediment is lithified and becomes sedimentary rock. The type of sedimentary rock formed depends on factors such as the composition of the original igneous rock, the nature of the sediment particles, and the environmental conditions during deposition and lithification.


The transformation of igneous rocks into sedimentary rocks involves a complex series of geological processes. Weathering breaks the original rock into smaller particles, which are then eroded and transported by natural forces. Deposition occurs when the sediment settles and accumulates in a new location, forming distinct layers. Finally, lithification compacts and cements the sediment, transforming it into a solid sedimentary rock.
Understanding the processes involved in the formation of sedimentary rocks from igneous rocks is critical to unraveling Earth’s geologic history and reconstructing past environments. By studying sedimentary rocks, scientists can gain valuable insights into Earth’s past climate, the evolution of life, and even the presence of natural resources.


How does an igneous rock become sedimentary?

An igneous rock can become sedimentary through a process called weathering and erosion. Over time, exposure to the elements, such as wind, water, and temperature changes, breaks down the igneous rock into smaller fragments or sediments.

What happens during weathering?

Weathering is the process by which rocks are broken down into smaller pieces through physical or chemical means. In the case of igneous rocks, weathering can occur due to the expansion and contraction caused by temperature changes, or through the action of water and ice.

How are sediments formed?

Sediments are formed when weathering and erosion break down rocks into smaller fragments. These fragments can range in size from tiny particles to larger boulders. The type of sediment formed depends on the composition of the original rock and the intensity of the weathering and erosion processes.

What happens after sediments are formed?

After sediments are formed, they can undergo transportation by agents like water, wind, or ice. These agents carry the sediments away from their original location and deposit them in new areas.

How do sediments become sedimentary rocks?

Sediments become sedimentary rocks through a process called lithification. Lithification involves the compaction and cementation of the sediments over time. The weight of the overlying sediments and the minerals present in the groundwater act as cementing agents, binding the sediments together to form a solid rock.

What are some examples of sedimentary rocks?

Some examples of sedimentary rocks include sandstone, limestone, shale, and conglomerate. Sandstone is composed of sand-sized grains that have been compacted and cemented together. Limestone is made up of the remains of marine organisms, such as shells and coral. Shale is formed from compacted clay and silt particles, and conglomerate consists of rounded pebbles embedded in a matrix of sand or clay.