description Dyalpur Overview
Dyalpur is a ureilite meteorite that fell in the state of Uttar Pradesh, India, in 1872. As an achondritic meteorite, it belongs to a rare group known for its carbon-rich composition. Dyalpur specifically contains both graphite and microscopic trace diamond inclusions formed under high pressure within its parent asteroid. This carbon-bearing mineralogy makes it a valued subject for researchers investigating the early solar system and the dynamic processes of planetary bodies.
help Dyalpur FAQ
What makes Dyalpur unusual among ureilite meteorites?
Dyalpur is a carbon-rich ureilite containing graphite and microscopic trace diamond inclusions. Those inclusions record high-pressure processes that affected material in its parent body.
When and where did Dyalpur fall?
Dyalpur fell in Uttar Pradesh, India, in 1872. It is therefore an observed historical fall rather than a meteorite found only after long exposure on the ground.
How do the graphite and diamond inclusions form in Dyalpur?
The graphite and microscopic diamonds formed during intense pressure and shock-related processes in the meteorite's parent body. They are mineral inclusions inside the ureilitic rock, not manufactured gems suitable for ordinary jewelry use.
How does Dyalpur compare with the ureilite Almahata Sitta?
Both Dyalpur and Almahata Sitta belong to the carbon-rich ureilite group. Almahata Sitta fell in Sudan in 2008 and is known as a polymict ureilite, while Dyalpur is the older Indian fall described here.
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