Limburg (Weilheim An Der Teck)
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Limburg (Weilheim an der Teck) is a mountain of
Baden-Württemberg Baden-Württemberg (; ), commonly shortened to BW or BaWü, is a German state () in Southwest Germany, east of the Rhine, which forms the southern part of Germany's western border with France. With more than 11.07 million inhabitants across a ...
,
Germany Germany,, officially the Federal Republic of Germany, is a country in Central Europe. It is the second most populous country in Europe after Russia, and the most populous member state of the European Union. Germany is situated betwe ...
. Striking is the breakdown of vegetation: the summit is covered with lean lawn and some solitary
Tilia ''Tilia'' is a genus of about 30 species of trees or bushes, native throughout most of the temperateness, temperate Northern Hemisphere. The tree is known as linden for the European species, and basswood for North American species. In Britain a ...
. Below this is a zone of scrub forest on the southern slope with vineyards, and on the lower slopes of extensive orchards.


Geology

The Limburg is a mountain of volcanic origin, more precisely a formerly active volcanic vent of the
Swabian Jura The Swabian Jura (german: Schwäbische Alb , more rarely ), sometimes also named Swabian Alps in English, is a mountain range in Baden-Württemberg, Germany, extending from southwest to northeast and in width. It is named after the region of ...
. However, it does not correspond, despite its striking cone shape the Ashes volcanoes on the type of Etna or
Vesuvius Mount Vesuvius ( ; it, Vesuvio ; nap, 'O Vesuvio , also or ; la, Vesuvius , also , or ) is a somma-stratovolcano located on the Gulf of Naples The Gulf of Naples (), also called the Bay of Naples, is a roughly 15-kilometer-wide (9 ...
. Before about 17 million years ago there came here to massive gas and dust explosions when percolating water met in the columns of the Jura on a magma bubble that had formed in the depths. The up broken rocks fell back into the crater and solidified over time to basaltic. Here no molten lava came to the surface. She remained rather stuck in the volcanic vent and froze there to Basalt. In the following year, millions the Jurassic layers were eroded more and more. The Basalttuffpfropf was more resistant than the surrounding limestone and remained as the northern slope of the
Swabian Alb The Swabian Jura (german: Schwäbische Alb , more rarely ), sometimes also named Swabian Alps in English, is a mountain range in Baden-Württemberg, Germany, extending from southwest to northeast and in width. It is named after the region of ...
mountain upstream cone stand and testified that this formerly extended further to the north. Mountains and hills of the Swabian Jura {{BadenWürttemberg-geo-stub