Regmaglypts

Regmaglypts are shallow, thumbprint-like impressions on the surface of larger meteorites that are formed by preferential local ablation of material from the surface as a meteor passes through the Earth’s atmosphere. They are probably formed by vortices of hot gas. Any meteorite with regmaglypts will have a fusion crust. Many meteorites with fusion crusts do not have regmaglypts, however.

Here are photographs of a few examples.  (I collect meteorite photos an do not remember where I obtained some of these photos.)

Lunar meteorite Northwest Africa 482. Regmaglypts are present on the left but not the right. Image credit: Jim Strope

MacAlpine Hills 88108, a 15.4-lb H5 chondrite from Antarctica. Image credit: Randy Korotev

This large meteorite, Lewis Cliff 85320 (H5 chondrite, (244 lbs) has lots of regmaglypts.

Even this small meteorite (on the ice in Antarctica) has regmaglypts.

One of the Camel Donga stones from Australia. (Photo credit: Jim Strope)

Unidentified meteorite found in Nevada with regmaglypts and a grasshopper. Image credit: I’ve forgotten. Let me know if this great photo is yours. photo.

This is a pretty one. Image credit: ?

Unidentified meteorite with regmaglypts: Image credit: ?

Regmaglypts on iron meteorites can be spectacular. Here are small fragments of Sikhote-Alin, an iron meteorite. All of the biggest have regmaglypts. Image credit: Randy Korotev

NOT Regmaglypts

All the photos below were sent to me buy people who thought the rocks had regmaglypts. None of these rocks are meteorites – none has a fusion crust. Most of these features are the result of sculpting by wind or water on Earth. Some of the depressions are incipient vesicles.