Fossils can form in sedimentary rocks. Here's the step-by-step process:

1. An organism dies: The process of fossilization begins when an organism dies. It's important that the organism quickly gets covered by sediment. This sediment can be sand, silt, or clay.

2. Sedimentation: Over time, more and more sediment layers build up on top of the organism. The weight of the upper layers compresses the lower layers into rock.

3. Decay: Most of the organism decays or is eaten away. However, the hard parts like bones and shells are left behind.

4. Mineralization: Over thousands of years, water seeping through the rock can deposit minerals in the bones and shells, turning them into stone.

5. Erosion: Eventually, erosion or people digging can reveal the fossil.

It's important to note that not all organisms become fossils. The conditions have to be just right. That's why fossils provide only a fragmentary record of life on Earth.

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Fossils can form in sedimentary rocks. Here's the step-by-step process:

1. An organism dies: The process of fossilization begins when an organism dies. It's important that the organism quickly gets covered by sediment. This sediment can be sand, silt, or clay.

2. Sedimentation: Over time, more and more sediment layers build up on top of the organism. The weight of the upper layers compresses the lower layers into rock.

3. Decay: Most of the organism decays or is eaten away. However, the hard parts like bones and shells are left behind.

4. Mineralization: Over thousands of years, water seeping through the rock can deposit minerals in the bones and shells, turning them into stone.

5. Erosion: Eventually, erosion or people digging can reveal the fossil.

It's important to note that not all organisms become fossils. The conditions have to be just right. That's why fossils provide only a fragmentary record of life on Earth.

Knowee AI · Accepted Answer

Fossils can form in sedimentary rocks. Here's the step-by-step process:

1. An organism dies: The process of fossilization begins when an organism dies. It's important that the organism quickly gets covered by sediment. This sediment can be sand, silt, or clay.

2. Sedimentation: Over time, more and more sediment layers build up on top of the organism. The weight of the upper layers compresses the lower layers into rock.

3. Decay: Most of the organism decays or is eaten away. However, the hard parts like bones and shells are left behind.

4. Mineralization: Over thousands of years, water seeping through the rock can deposit minerals in the bones and shells, turning them into stone.

5. Erosion: Eventually, erosion or people digging can reveal the fossil.

It's important to note that not all organisms become fossils. The conditions have to be just right. That's why fossils provide only a fragmentary record of life on Earth.

In what kind of rock CAN fossils form?

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