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Why Do Some Tektites Have a Teardrop Shape?

Published in Tektite Morphology 2 mins read

Teardrop-shaped tektites primarily form due to the intense spinning forces experienced by molten terrestrial ejecta as they rapidly re-enter Earth's atmosphere after a meteorite impact.

The Dynamic Formation of Tektite Shapes

Tektites are unique natural glass objects created when a large meteorite strikes Earth, melting and ejecting terrestrial material into the atmosphere or even briefly into space. As this molten material falls back to Earth, it undergoes significant aerodynamic shaping while still in a molten state, before solidifying into distinct forms.

Among the various shapes of tektites – including spheres, dumbbells, and buttons – the teardrop or spindle shape is a specific outcome of the extreme rotational forces during their atmospheric journey.

How Teardrop Shapes Emerge:

The formation of a teardrop-shaped tektite involves a fascinating sequence driven by rotational dynamics:

  • Initial Elongation: As the molten tektite material descends through the atmosphere, it often elongates due to aerodynamic drag and initial spin, forming a prolate (elongated spheroidal) shape.
  • Dumbbell Precursor: With increasing and rapid rotation, this elongated mass can become constricted in the middle, evolving into a "dumbbell" shape, characterized by two rounded ends connected by a narrower central bridge.
  • Splitting Due to Excessive Spin: If the spinning force becomes too great for the structural integrity of the central mass of the dumbbell-shaped tektite, the narrow bridge connecting the two ends ruptures. This powerful split causes the two resulting pieces to separate. Each piece continues its trajectory toward Earth, solidifying into the characteristic spindle or teardrop form as it cools rapidly.

This process illustrates the volatile conditions under which tektites are created, where a combination of high-speed re-entry, aerodynamic forces, and intense spinning sculpts them into their final, often intricate, shapes.