- In March 2025, a rare and well-preserved petrified fossil was discovered at Rajmahal Hills in Pakur district, Jharkhand. The fossil, identified as petrified teak wood, is significant for understanding ancient plant life.
What is Petrification?
- Petrification is a type of fossilization where minerals replace the original organic material, creating a stone-like fossil while maintaining the structural details of the original organism.
- Example: Petrified wood, also known as fossil wood, forms when plant material is buried under sediment and preserved due to a lack of oxygen, which prevents decay.
- Over time, minerals like silica (SiO₂) or calcite (CaCO₃) replace the organic material, crystallizing and turning it into stone while retaining the original structure of the wood.
- This process can occur in both hard and soft tissues.

How Does Petrification Occur?
Petrification requires specific geological conditions, including:
- Burial under sediment – Organic material must be quickly covered to prevent decay.
- Exposure to mineral-rich water – Groundwater or lake water rich in minerals seeps into the buried material.
- Slow replacement of organic matter – Over thousands to millions of years, minerals fill the pores of tissues, dissolve the organic matter, and take its place.
- Formation of a fossil – The mineralized structure remains, preserving details of the original material.
What are the Types of Petrified Fossils?
- Petrified Wood – Trees or forests fossilized over time, retaining bark, rings, and cell structure.
- Amber-Preserved Fossils – Insects or small organisms trapped in tree resin, which hardens over time.
- Coprolites – Fossilized animal feces that help scientists study ancient diets.
Importance of Petrification
- Preserves ancient life forms – Helps in understanding extinct species.
- Gives insights into past environments – Shows climate, vegetation, and geological changes.
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Scientific value – Used in paleontology to reconstruct prehistoric ecosystems.
- Paleontology is the study of the history of life on Earth as based on fossils.
Global Example of Petrification
- Petrified Forest National Park (Arizona, USA): Home to vast silicified wood deposits.
- Chalcedony (a quartz form) replaces tree tissues while preserving cellular structures.
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- Fossils are the remains of plants, animals, fungi, bacteria, and single-celled living things that have been replaced by rock material or impressions of organisms preserved in rock.
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About Rajmahal Hills
- Located in the Santhal Pargana division of Jharkhand.
- Formed by volcanic activity during the Jurassic period, leading to Rajmahal Traps (ancient volcanic rock formations).
- Known for rich plant fossil deposits, some dating back millions of years.
- Inhabited by indigenous Sauria Paharia (higher elevations) and Santhal (valleys) tribes.
Significance of the Discovery
- The 1st recorded petrified fossil from Rajmahal Hills.
- The fossilized teak wood provides insights into the ancient flora of the region.
- Strengthens Rajmahal Hills’ status as a paleontological and geological site.
