Last weekend, Red Baron attended a 90th birthday party in Postbauer-Heng near
Nuremberg.
A son of the jubilee,
Gernot Arp, professor of geology and paleontology at Göttingen University, offered to
take those interested on a geological excursion to the former university town
of Altdorf. Nearby, there is a unique geological formation.
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Altdorf in the Topographia Frankoniae 1648. The university
buildings are on the upper left.
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When I hear the word Altdorf, I automatically think of
William Tell, but Old Village is a common name in "German" lands.
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Students at Altdorf University listen to their lecturer
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Hadn't Wallenstein once studied in Altdorf, not far from the site of one
of his greatest triumphs?
In August 1632, Gustaf Adolf had made himself at home in
Nuremberg. Wallenstein had fortifications built on the hills on the north
bank of the Rednitz near the Alte Veste in Zirndorf and waited until the
Swedish king was forced to leave Nuremberg due to a lack of provisions.
Finally,
on September 3, Gustaf Adolf sought a military decision. Again and again,
he sent his troops to attack the well-entrenched imperial forces, but in
vain.
Wallenstein wrote to his emperor,
Ferdinand II, "The king has suffered a tremendous blow in this enterprise ... and
although Your Majesty had valor and courage to spare before, this occasion
has confirmed them even more, seeing how the king, having brought all his
power to bear, has been repulsed, and the title of
invictissimi belongs not to him but to Your Majesty." Well,
Wallenstein kisses the but of his commander.
Gustav Adolf not
only lost his aura of invincibility but also a third of his troops. Many
of his mercenaries deserted and seamlessly joined Wallenstein's forces.
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The university building in Altdorf
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Gustaf Adolf fell in the Battle of Lützen in November 1632, and the
University of Altdorf
closed its doors in 1809
during the Napoleonic era.
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The campus in 2026. Note: the fountain is still in place.
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The main building of Altdorf’s former university is now a social-diaconal
facility focused on people with disabilities, named after
Johann Heinrich Wichern.
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If you want something, you have to want it completely;
half-heartedness is the same as nothing.
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Wichern is widely known as the inventor of the Advent wreath.
But I digress.
Before we visited the geological site, we went to the Museum in Atdorf,
which houses impressive fossils found during the excavation of the
Ludwigskanal.
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The Ludwigskanal at the Dörlbach incision near Altdorf
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At the beginning of the 19th century, Bavarian King Ludwig I ordered the
construction of an artificial waterway to be built between Kelheim on the
Danube and Bamberg on the Main. The project started in 1836 and took 10
years to complete.
The idea of building a navigable connection between the Rhine and Main
rivers and the Danube was not new. Common theories assume that Charlemagne,
then still King of the Franks, had the so-called
Fossa Carolina (also
known as Karl's Ditch) built in 793.
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The Dörlbach incision for the Ludwigskanal in 1845, with the old
road bridge
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The
Ludwigskanal was 173 km long and had 100 locks. However, the
ships were too small for mass transport, and soon the powerful railroad
entered the market.
In 1950, the canal was abandoned after many sections had already been
destroyed during World War II. In 1992, a modern Main-Danube Canal was
inaugurated, but it proved uneconomical too and is now used only for
tourist boat trips and water sports.
At the museum, Prof. Arp gave an introduction to Earth's history before
our group admired the exhibit.
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Timeline of Earth's history
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A map in the museum shows the geological formation through which the
Ludwigskanal was built.
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Pachycormus, the thick-bodied fish, lived in the
time period of 189-60 million years ago
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Ammonites
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Ichtyosaur (Stenoteropterygius quadriscissus)
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Ichthyosaurs are land animals that returned to the sea and
transformed their limbs back into flippers. The number of finger
joints and finger rays increased, especially between 182 and 174
million years ago.
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Altdorf black marble
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Black marble from Altdorf with its fossil inclusions was à la mode and
correspondingly expensive.
According to the museum director, this tobacco box made from black
marble is the “most expensive” item of the exhibition.
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Geological cross-section through the terraced slope of the
Dörlbach incision for the Ludwigkanal.
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Using a display board, Prof. Arp explained the geological situation
of the Dörlbach incision.
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Climate change, ocean currents, and mass extinction
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The rock sequence cut into Dörbach reflects a striking shift
from a cold, glaciated period to a warm period. The cause is
believed to be the simultaneous strong volcanic activity in the
southern hemisphere of the Earth and the resulting increase in
atmospheric carbon dioxide. As temperatures rose, sea levels
rose sharply, and ocean circulation decreased. This led to salt
stratification in the water and ultimately to a lack of aeration
of the sea floor. This was followed by species extinction and
the formation of facies sludge in the Posidonia shale.
Only the slow degradation of carbon dioxide over 2-3 million
years and the further opening of the epicontinental sea to the
Arctic led to gradual re-aeration and mixing with
bottom-contacting ocean currents. Evidence of this can be found
in so-called belemnite battlefields and a more species-rich
bottom fauna in the Jurassic marl.
(Gernot Arp, University of Göttingen).
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(©James Albright)
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The most impressive find during construction of the Ludwig Canal was
a 1.5-meter-long ichthyosaur skull.
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Tunnelling of the Ludwigskanal at Schwarzenbach
(©Brunzerus/Wikipedia)
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On our way back to Postbauer-Heng, we passed the tunnel at
Schwarzenbach. What a technical achievement in the middle of the
19th century.
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Interesting article. On the way back from MA after Thanksgiving we were driving back thru upstate NY and stopped at the Erie Canal Museum in Syracuse. We didn't realize the manpower needed to construct such a long project. I have visited the lift near Eberswalde and rode up in the lodge lift while the new was being built. Quite an accomplishment.
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