description Krymka Overview
Krymka is an LL3.1 ordinary chondrite meteorite associated with a 1946 fall in Ukraine. Its very low petrologic subtype identifies it as a highly unequilibrated specimen whose components underwent comparatively little thermal alteration after accumulation on its parent body. The preservation of distinct chondrules, fine-grained material, presolar grains, and carbon-bearing compounds makes Krymka useful for research into primitive matter inherited by the early solar system.
help Krymka FAQ
What type of meteorite is Krymka?
Krymka is classified as an LL3.1 ordinary chondrite meteorite. The LL designation indicates it has very low total iron content compared to other ordinary chondrites.
When and where did the Krymka meteorite fall?
The meteorite is associated with a fall that occurred in Ukraine in 1946. It was named after the region where it was recovered.
Why is Krymka scientifically significant to researchers?
Its very low petrologic subtype of 3.1 identifies it as a highly unequilibrated specimen. This means its components underwent comparatively little thermal alteration after accumulating on its parent body.
What does the petrologic type of the Krymka meteorite tell us?
As a type 3.1 chondrite, it retains pristine, original materials from the early solar system. Scientists study its unmodified minerals to understand the conditions of the solar nebula before planetary heating melted and homogenized the rocks.
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