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Forggensee
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Forggensee

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Also known as Forgensee (misspelling), Roßhaupten Reservoir

Key facts

Dam.name
Forggensee
Dam.image
Aerial image of the Forggensee (view from the southwest).jpg
Dam.image_caption
Aerial view of the Forggensee
Dam.location
Ostallgäu
Dam.construction_began
1950–1954
Dam.dam_crosses
Lech, Füssener Ache, Mühlberger Ache
Dam.dam_height_thalweg
37 m
Dam.dam_height_foundation
41 m
Dam.dam_length
320 m
Dam.dam_width_crest
10 m
Dam.dam_width_base
<!--
Dam.dam_curve_radius
{} -->
Dam.dam_volume
650,000 m3
Dam.res_capacity_active
168 Mm3
Dam.res_catchment
1,594 km2
Dam.res_surface
15.2 km2
Dam.res_max_length
8.7 km
Dam.res_max_width
2.8 km

via Wikipedia infobox

Wikidata facts

Area
15.2
Elevation
785
Image
Aerial image of the Forggensee (view from the southwest).jpg
Width
2.8
Length
8.7
Show 4 more facts
Commons category
Forggensee
vertical depth
41
volume as quantity
0.65
inception
1950-00-00
Sources (1)

via Wikidata · CC0

~10 min read

Article

9 sections
Contents
  • Origin
  • Lake Füssen
  • Silting up of Lake Füssen
  • Reservoir
  • Conservation and archaeology
  • Recreation
  • Gallery
  • References
  • External links

thumb|The Forggensee from the north. In the background are the Tegelberg, [[Säuling, Thaneller and Tannheim Mountains, Neuschwanstein Castle may be seen in the foothills to the left; to the right is Füssen]] The Forggensee, also called the Roßhaupten Reservoir, is a reservoir located north of Füssen in the county of Ostallgäu in Bavaria, Germany and one of many lakes in the region around Hohenschwangau and Neuschwanstein castles. With a surface area of 15.2&nbsp;km2, it is the fifth-largest lake in Bavaria and the largest reservoir in Germany by area. The River Lech flows through it. The Forggensee is known primarily as a tourist destination for aquatic sports and recreation. Besides Füssen, other settlements on the lake include Halblech, Rieden am Forggensee and Roßhaupten. The lake takes its name from the former hamlet of Forggen which has been submerged by the reservoir.

== Origin == Following the climax of the last ice age, the Lech-Wertach foreland glacier, which covered the entire Ostallgäu, gradually melted back from its maximum extent at Kaufbeuren. In the course of its retreat, as in the entire Pre-Alpine area, new morainic ridges were formed from the masses of debris carried by the ice from the mountains piled up at the edge of the glacial tongue whenever the glacier halted temporarily or advanced briefly again. These ridges can still be seen in today's landscape.

Gallery (4)

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