BR 1150 ATLANTIC 61+14
Yellow Dahlia
Pretty Rouge Dahlia
Kleiber Günther (5)
A Tornado in the backyard
After the bath
Notlandung
Schloss Pillnitz
Liebe Erinnerungen
Kleiber Günther (42)
Happy New Year!
Let’s start the new year a little more relaxed
Kleiber Günther (34) and the big nut
Greetings by a bunch of flowers
Kleiber Günther (40)
Wrinkled hornbill
A Sunbather
VW Phaeton Tower
Azalee
Gymnasts on Tour
Kleiber Günther (41)
Leaf in fence
Wasaplatz Grafitti
Schmuck- und Dekorativ-Dahlie "Dynastie" (2)
La France renaissante
Le Jongleur
Aster novi-belgii
Just Pink Autumn
VFW 614 Jetliner
Im Schatten der Engelstrompeten
Das Städtchen Kufstein im schönen Tirol
Pink Littles
Dresden - Großer Garten - Postkarte
Palais im Großen Garten
Die Atlantis
Mil Mi-8 PS11 94+01
Beim Kaffeetrinken
Red Autumn Propeller
Alpenstrasse
Herbst in Rot-Grün
Feuerschiff - ELBE 1
Vermessungsschiff Grimmershörn
Korsar GRE 11
Stier
Breguet Atlantic 61+06
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Alfred Wegener Institut
Alfred Wegener Institute for Polar and Marine Research in Bremerhaven
en.wikipedia.org/wiki/Alfred_Wegener_Institute_for_Polar_and_Marine_Research
www.awi.de
Alfred Lothar Wegener (November 1, 1880 – November 1930) was a German polar researcher, geophysicist and meteorologist.
During his lifetime he was primarily known for his achievements in meteorology and as a pioneer of polar research, but today he is most remembered as the originator of the theory of continental drift by hypothesizing in 1912 that the continents are slowly drifting around the Earth (Kontinentalverschiebung).
His hypothesis was controversial and not widely accepted until the 1950s, when numerous discoveries such as palaeomagnetism provided strong support for continental drift, and thereby a substantial basis for today’s model of plate tectonics
en.wikipedia.org/wiki/Alfred_Wegener
en.wikipedia.org/wiki/Alfred_Wegener_Institute_for_Polar_and_Marine_Research
www.awi.de
Alfred Lothar Wegener (November 1, 1880 – November 1930) was a German polar researcher, geophysicist and meteorologist.
During his lifetime he was primarily known for his achievements in meteorology and as a pioneer of polar research, but today he is most remembered as the originator of the theory of continental drift by hypothesizing in 1912 that the continents are slowly drifting around the Earth (Kontinentalverschiebung).
His hypothesis was controversial and not widely accepted until the 1950s, when numerous discoveries such as palaeomagnetism provided strong support for continental drift, and thereby a substantial basis for today’s model of plate tectonics
en.wikipedia.org/wiki/Alfred_Wegener
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