Other parts of the Ischgl area, towards Höllboden and Paznauner Thaya, offer many red runs and some more challenging blacks.

A significant portion of the cases were further traced to the Kitzloch après-ski bar at the resort, where sharing of whistles were likely conduits of contagion.

Classified as an LL6 chondrite with excellent preservation, the meteorite's origin was traced back to a fireball event (EN241170) recorded in November 1970 over Germany.

[11] Advanced trajectory reconstruction techniques and radionuclide data confirmed the meteorite's link to this fireball, providing insights into its cosmic history and heliocentric orbit.

With a remaining main mass of 708.1 grams, the meteorite's exterior is fully crusted, showcasing regmaglypts, while its interior reveals a light-gray chondritic texture.

The identification of the meteorite's source fireball helps understand its journey through space and its relatively recent fall to Earth.