The “Papenvoortse Dijk”, a sandy path that runs between Nuenen (the village where I live) and Helmond, is the watershed between 2 local streams. Northern Red Oaks (Quercus rubra/Amerikaanse Eik) flank this dike; the leaves have deep red colors this time of year. The ridge of sand is deposited during the last ice age about 10.000 years ago. On the old topographic map of 1704 AD this dike was clearly visible. At that time it was a local ‘highway’ for farm carts loaded with sods of turf and dung. Miraculously, this connection survived as a sandy path in todays dense network of tarmac roads.
Wednesday, 28 October 2009
Papenvoortse Dijk
The “Papenvoortse Dijk”, a sandy path that runs between Nuenen (the village where I live) and Helmond, is the watershed between 2 local streams. Northern Red Oaks (Quercus rubra/Amerikaanse Eik) flank this dike; the leaves have deep red colors this time of year. The ridge of sand is deposited during the last ice age about 10.000 years ago. On the old topographic map of 1704 AD this dike was clearly visible. At that time it was a local ‘highway’ for farm carts loaded with sods of turf and dung. Miraculously, this connection survived as a sandy path in todays dense network of tarmac roads.
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