“An eternal reminder” echoed in my mind as I approached this stone. This is the Wetterstein. It commemorates a severe storm from August 11, 1837.
Now, let’s delve into the story of the Wetterstein. The Wetterstein Formation is a regional geologic formation. It stretches across the Northern Limestone Alps and Western Carpathians. This area extends from southern Bavaria in Germany. It continues through northern Austria to northern Hungary and western Slovakia.
The formation dates back to the Late Triassic period. Specifically, the Ladinian to Carnian stages. The Wetterstein is named after the Wetterstein Mountains. These mountains are in southern Germany and northwestern Austria. The Karwendel Mountains are at the center of its distribution. It occurs in the Northern and Southern Limestone Alps. Also, it is found in the Western Carpathians.
The Wetterstein Formation consists mainly of reefal limestones and dolomites. Dolomitization is a widespread process that alters the limestone. It leads to the formation of dolomite. In many areas, limestone and dolomite frequently alternate. Local names for the Wetterstein Formation include Wettersteinkalk and Wettersteindolomit.
The Wetterstein Formation can reach a thickness of up to 1,000 meters. This formation belongs to the tectonostratigraphical unit Austroalpine nappes. The carbonate rock is from the Middle Triassic epoch. It is comparable to the Muschelkalk rock strata.
Numerous fossils have been found within the Wetterstein Formation. These fossils include corals, sponges, bivalves, and gastropods. These marine groups indicate a shallow marine carbonate platform environment. This environment existed at the northern end of the Tethys Ocean.
Alternative names exist for the Wetterstein Formation. These names are used in a stratigraphical sense. Examples include Wetterstein Limestone and Wettersteinkalk Formation. Others are Wettersteindolomit and Wetterstein Limestone Formation.
Subunits of the Wetterstein Formation include Messerstich Limestone. Others are Schlern Dolomite, Marmolata Limestone, and Steinalm Formation. Also included is the Ramsau Dolomite Formation.
The Wetterstein Mountains are an ideal region for mountaineers and climbers. The Zugspitze is the highest peak. It is also the highest mountain in Germany. The proximity to southern German population centers make it a tourist destination. Despite this, some places in the Wetterstein are rarely visited.
The Wetterstein borders several other mountain ranges. These include the Ammergau Alps to the west and north. The Bavarian Prealps are to the northeast. The Karwendel is to the east. The Mieming Chain is to the south.
The Wetterstein mountains offer habitats for several animal species. These include chamois, Alpine marmots, and Alpine choughs. Also found are Alpine salamanders, adders, and golden eagles.
The Wetterstein Tunnel project was discussed for many years. It aimed to build a railway tunnel between Telfs and Garmisch-Partenkirchen. The tunnel would have been 22 kilometers long. It would have cut travel time between Munich and Innsbruck. The project was estimated to cost 2.2 billion euros.
So, as you stand before the Wetterstein, remember its geological history. Consider its impact on the landscape. Appreciate its role as a boundary. A home for diverse species. Finally, remember the storm it commemorates.