
STS106-711-49
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All of Ireland; Great Glen fault of Scotland in distance.
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STS106-718-28
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Straits of Dover, white cliffs, ships.
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STS106-714-79
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Netherlands looking north.
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STS106-718-30
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Antwerp, Belgium, on the Scheldt River.
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STS106-711-55
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Northern France looking north to Denmark.
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STS106-702-80
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France--panorama looking east.
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STS106-703-83
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City of Nantes, France.
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STS106-704-66
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The Pyrenees (highest point 3404 m), extending from the Bay of Biscay
to the Gulf of Lyon, began forming during Eurasian-African
interactions about 80 million years ago. The Cordillera Cantabrica,
along the north coast of Spain, is a more deeply eroded ancient
mountain chain that formed ~320 million years ago.
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STS106-702-84
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The Alps were uplifted later (~60 million years ago) than were the
Pyrenees, in the same Eurasian-African collision. The western Alps
are truncated by younger Rhone rift faults; the Rhone and Rhine rift
valleys, as well as the transform fault zone (from Basel, Switzerland
to Dijon, France) developed about 23 million years ago.
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STS106-702-86
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The great Alpine folds have been cut by younger structures such as
the Rhone rift and the Basel-Dijon transform fault zone. The
transform zone connects the Rhone and Rhine rift segments; it is
expressed as NE-trending fault valleys (zones of horizontal shear)
and narrow, dagger-like folds, which are deformed Alpine structures.
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