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New mineral „Riesite” discovered in the crater of the Ries of Nördlingen

Nördlinger Ries in wintertime, view of the southern crater rim near the village of Mönchsdeggingen. Photo: Bernhard Hampp / Wikimedia Commons
It was found in melt veins of a gneiss-like rock that was exposed to extreme pressure and high temperature during the impact

A new, so far unknown mineral has been discovered in the Ries of Nördlingen, one of the best-preserved impact craters on Earth formed some 15 million years ago by the impact of an asteroid. Its discovery is the result of an international cooperation between scientists from the USA and Germany who are working in Las Vegas, Heidelberg, and in the Natural History Museum at Berlin.

For the new high-pressure mineral discovered in the Ries crater, the discoverer Prof. Oliver Tschauner (Las Vegas) and Prof. Chi Ma (Pasadena) proposed the name „Riesite”. The International Mineralogical Association (IMA) confirmed this name officially in 2017.

The discovery of this mineral is the result of a new analytical technique in which synchrotron radiation is applied instead of the more conventional techniques such as optical microscopy or electron microscopy. PD Dr. Volker Stähle (Heidelberg), and Prof. Dieter Stöffler (Berlin) provided suitable samples from the Ries to the US colleagues.

Riesite occurs in the form of extremely small grains. It was found in melt veins of a gneiss-like rock that was exposed to extremely high pressure and to temperatures of more than 1500 °C during the Ries impact.

Riesite is chemically a special high-pressure form of titanium dioxide (TiO2). Titanium dioxide occurs in small amounts as the mineral rutile in many crustal rocks of the Earth and therefore also in the crystalline basement rocks of the Ries.

They were originally present in a depth of more than 600 m. But the impact exposed them to extremely high pressure and temperature and ejected the shock-metamorphosed rocks out of the crater to the surface where they were deposited as the so-called suevite breccia.

The transition from rutile to Riesite is rather complicated because rutile is first transformed to another high-pressure mineral called akaogiite. Subsequently akaogiite transforms in part to the mineral Riesite during pressure-temperature release.

Nördlinger Ries, schematic drawing of the cratering event. Source: User Vesta / Wikimedia Commons

The suevite layer, in which Riesite was detected, forms the uppermost layer of the ejecta blanket of the Ries crater. Suevite is a typical rock that occurs in a large number of impact craters on Earth. Already the Romans used it as a building stone in the Ries. During the Middle Age, it was frequently used in Nördlingen and other towns of the Ries and in the 19th century even in cities like Leipzig and Berlin.

On the walls of buildings made from suevite stones, such as the St. George cathedral in Nördlingen, one can see inclusions of rocks, which contain Riesite and many other high-pressure minerals, altogether 10 minerals including diamond. This is the highest number of high-pressure minerals among all known 190 impact craters on Earth.

The Nördlinger Ries in Southern Germany ist the result of a meteorite impact about 14,5 million years ago. Normaly, wind an weather wish the crater structures away – yet in the Ries, the large hole in the ground has been well preserved.

Source: Naturkundemuseum Berlin

(07.06.2018, USA: 06.07.2018)