description Lowicz Overview
Lowicz is a rare mesosiderite meteorite that fell in Łowicz County, Poland, in 1935, producing several fragments with a combined mass of roughly 56 kilograms. Mesosiderites are a class of stony-iron meteorites formed from the mixing of iron and silicate materials during asteroid collisions. The Lowicz meteorite features a complex brecciated structure, making it an important subject for planetary geologists. It provides physical evidence for understanding the differentiation and impact processes that occurred in the early solar system.
help Lowicz FAQ
Why are mesosiderites such as Lowicz called stony-iron meteorites?
Lowicz combines metallic iron-nickel material with silicate rock, giving it both stone and metal components. This unusual mixture is the defining feature of the mesosiderite class.
When and where did the Lowicz meteorite fall?
Lowicz fell in Łowicz County, Poland, in 1935. The fall produced several recovered fragments with a combined mass of roughly 56 kilograms.
Why is the Lowicz fall especially useful to meteorite researchers?
A witnessed fall provides a reliable terrestrial date and location for a meteorite that formed in an asteroid. Lowicz also preserves evidence of mixing between metallic and rocky materials inside its parent asteroid.
How can I tell whether a Lowicz fragment is genuine?
A genuine specimen should be identified as a mesosiderite and linked to the 1935 Polish fall through dealer or laboratory documentation. Its appearance may include contrasting metallic and silicate areas, but appearance alone is not proof of authenticity.
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