- Jurassic Age Belemnite
- Miocene Age Meteorite Impact
- Ries Meteor Crater
- Western Bavaria, Germany
- The specimen measures approx. 1 1/16″ long and will come in the 3.25″ x 4.25″ Riker Mount with Label as Shown
14.5 Million Years Ago a Meteorite crashed into Western Bavaria, Germany causing the Ries Crater that has a rim 24 km in diameter. Today the floor of the crater sits approx. 150 Meters below the level of the rim. The tremendous shockwaves from the impact caused these belemnites that were buried in Jurassic Claystone to fracture into sections. Over the next 14.5 Million Years they re-fossilized in this fractured state. This is a calcite belemnite rostra – already a fossil over 100 million years old at the time of the impact – which was shattered below ground in the claystone and marlstone rock where it was deposited under the impact site. Over the ensuing million years silicates leached into the cavities to re-fuse a structure now looking like a rattle snake tail.
The depression is interpreted as a meteorite impact crater formed about 14.3 million–14.5 million years ago in the Miocene. The crater is most commonly referred to simply as the Ries or Ries crater. The original crater rim had an estimated diameter of 24 kilometers (15 mi). The present floor of the depression is about 100 to 150 m (330 to 490 ft) below the eroded remains of the rim.
It was originally assumed that the Ries was of volcanic origin. In 1960 Eugene Shoemaker and Edward C. T. Chao showed that the depression was caused by meteorite impact. The key evidence was the presence of coesite, which, in unmetamorphosed rocks, can only be formed by the shock pressures associated with meteorite impact. The coesite was found in the locally derived suevite building stone of the Nördlingen town church. The suevite was formed from mesozoic sediments shocked by the bolide impact.
Another impact crater, the much smaller (3.8 km diameter) Steinheim crater, is located about 42 km (26 mi) west-southwest from the centre of Ries. The two craters are believed to have formed nearly simultaneously by the impact of a binary asteroid.
Recent computer modeling of the impact event indicates that the impactors probably had diameters of about 1.5 kilometers (4,900 ft) (Ries) and 150 meters (490 ft) (Steinheim), had a pre-impact separation of some tens of kilometers, and impacted the target area at an angle around 30 to 50 degrees from the surface in a west-southwest to east-northeast direction. The impact velocity is thought to have been about 20 km/s (45,000 mph). The resulting explosion had the power of 1.8 million Hiroshima bombs, an energy of roughly 2.4×1021 joules.
The Ries crater impact event is believed to be the source of Moldavite tektites found in Bohemia and Moravia (Czech Republic). The tektite melt originated from a sand-rich surface layer that was ejected to distances up to 450 km (280 mi) downrange of the crater.
Stone buildings in Nördlingen contain millions of tiny diamonds, all less than 0.2 mm (0.0079 in) across. The impact that caused the Nördlinger Ries crater created an estimated 72,000 tonnes (79,000 short tons) of them when it impacted a local graphite deposit. Stone from this area was quarried and used to build the local buildings.