description B.P. Structure Overview
The B.P. Structure is an eroded meteorite impact structure in Libya, with a reported diameter of about 2.8 kilometres. It was discovered during petroleum exploration, so its identification is linked to subsurface geological investigation rather than to a clearly preserved surface crater. The structure is relevant to the study of small impact features, erosion in desert geology, and the search for impact evidence in regions explored for oil.
It is of interest to geologists and planetary-impact researchers.
help B.P. Structure FAQ
Where is the B.P. Structure located?
The B.P. Structure is an eroded meteorite impact structure in Libya. Its identification is linked to subsurface geological investigation.
How wide is the B.P. Structure?
Its reported diameter is about 2.8 kilometres. Because the structure is eroded, its original surface form is not clearly preserved.
How was the B.P. Structure discovered?
It was discovered during petroleum exploration. Subsurface geological evidence helped identify it as an impact structure.
Is the B.P. Structure a clearly visible crater?
No. It is eroded and does not have a clearly preserved surface crater, so geological investigation rather than a simple surface view is important.
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