Med udsigt til Ø bakker Traditional Cache
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En af de lette, lige i hovedhøjde...SÅ er der mere tid til at beundre udsigten :-)
Her deler Nørreådalen sig på begge sider af Ø bakker.
Geologi
Under den sidste istid var de brede jyske ådale banen for det smeltevand, der løb mod vest under isen. Ved istidens slutning søgte smeltevandet fra det isdækkede Østjylland gennem Nørreådalen frem til Hald Sø og videre ud over Karup Hedeslette. I perioden indtil Kattegat blev isfrit, strømmede samtidig smeltevand fra Gudenådalen ud ved Hjarbæk Fjord.
Senere ved havstigningen i stenalderen gik Randers Fjord ind til Vejrum, og bakken Ø var på det tidspunkt en regulær ø. Ved efterfølgende landhævning blev fjordbunden efterhånden tørlagt til Randers, og i dag gennemstrømmes Nørreådalen af vandrige, men nu regulerede åløb.
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GB:
Maybe to easy, right in front og Your head ... SO there is more time to admire the view :-)
Nørre Ådalen are going to be on both sides of the east hills.
Geology
During the last ice age was the broad jyske Aadal path for melt water, which flowed westward under the ice. By the end of glacial melt water requested from the ice covered Østjylland through Nørre Ådalens to Hald Lake and beyond Karup Heath Light. In the period up to the Kattegat was free of ice, melt water flowed simultaneously from Gudenå Valley during Hjarbæk Fjord.
Later at havstigningen in Randers Fjord Stone Age went into Vejrum and tray E was at the time of a regular island. In subsequent land uplift was fjord bottom gradually drained to Randers, and today through Nørre Ådalens water rich, but now regulated åløb.
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ont cå geæ
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