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Núpsvötn from air (40)

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Sand hills  In Núpsvötn river, South Iceland
Sand hills In Núpsvötn river, South Iceland Westernmost at Skeiðarársandur, Núpsvötn lakes are to be found. They are nourished by the rock stream Núpsá and the glacier river Súla. Súla flows down from the edge of Skeiðarárjökull glacier, at the corner of Eystrafjall mountain. The rivers merge into one river-bed some way above the bridge over Núpsvötn. When the main road was laid in 1974 both of the rivers were hindered with levees. In the first part of the 20th century, Súla-debacles from the lagoon Grænalón were massive, around 5-10 thousand m³/sec, and when Grænalón emptied the water level lowered about 150-200 m. These days it will only lower about 20 m and the quantity of water will peak at approx. 2000 m³/sec.
Abstract in the river Núpsvötn
Abstract in the river Núpsvötn Núpsvötn. Westernmost at Skeiðarársandur, Núpsvötn lakes are to be found. They are nourished by the rock stream Núpsá and the glacier river Súla. Súla flows down from the edge of Skeiðarárjökull glacier, at the corner of Eystrafjall mountain. The rivers merge into one river-bed some way above the bridge over Núpsvötn. When the main road was laid in 1974 both of the rivers were hindered with levees. In the first part of the 20th century, Súla-debacles from the lagoon Grænalón were massive, around 5-10 thousand m³/sec, and when Grænalón emptied the water level lowered about 150-200 m. These days it will only lower about 20 m and the quantity of water will peak at approx. 2000 m³/sec. Icelandic Stock Photos are an attractive and economical way to satisfy your creative requirements. On www.IceStockPhotos.com you can find more than 8.000 #Professional high resolution photos from #Iceland to suit your design requirements. All the #PHOTOS you need from #Iceland. http://www.icestockphotos.com
Núpsvötn river
Núpsvötn river Abstract in the river Núpsvötn Westernmost at Skeiðarársandur, Núpsvötn lakes are to be found. They are nourished by the rock stream Núpsá and the glacier river Súla. Súla flows down from the edge of Skeiðarárjökull glacier, at the corner of Eystrafjall mountain. The rivers merge into one river-bed some way above the bridge over Núpsvötn. When the main road was laid in 1974 both of the rivers were hindered with levees. In the first part of the 20th century, Súla-debacles from the lagoon Grænalón were massive, around 5-10 thousand m³/sec, and when Grænalón emptied the water level lowered about 150-200 m. These days it will only lower about 20 m and the quantity of water will peak at approx. 2000 m³/sec.
Two lanes in the river Núpsvötn
Two lanes in the river Núpsvötn Núpsvötn is next to Sandgígjur and is located in South, Iceland. Núpsvötn has a length of 0.7 kilometres. But it is splittet in seperate ways
Pattern in Núpsvötn river
Pattern in Núpsvötn river Núpsvötn is next to Sandgígjur and is located in South, Iceland. Núpsvötn has a length of 0.7 kilometres. But it is splittet in seperate ways
Núpsvötn river
Núpsvötn river Abstract in the river Núpsvötn
Núpsvötn river
Núpsvötn river Abstract in the river Núpsvötn
Núpsvötn river
Núpsvötn river Abstract in the river Núpsvötn
One lane in the river Núpsvötn
One lane in the river Núpsvötn Núpsvötn is next to Sandgígjur and is located in South, Iceland. Núpsvötn has a length of 0.7 kilometres. But it is splittet in seperate ways
Pattern inNúpsvötn river
Pattern inNúpsvötn river Núpsvötn is next to Sandgígjur and is located in South, Iceland. Núpsvötn has a length of 0.7 kilometres. But it is splittet in seperate ways