Binderup Å river |
Here at Vokslev was once a lively industry, here was digged chalk for more than 100 years. Todays visitors often come to see profiles in the chalk, if they are interested in the geology or in the chalk-industry. The profiles in the chalk show both the soft, white chalk from the Cretaceous period, which was used for building-material and the hard chalk from the tertiary period, which could be sawed out for building-stone. The chalk pit gives good opportunities for fossile-hunting (mostly sea urchin and bryozo).
At the mill |
The chalk pit in Vokslev is unique caused by the demarcation-line between the deposits, which places it among geological localitites of international importance. The stratum was deposited in the sea about 65 milllion years ago, the demarcation-line is marked by a thin layer of clay. In the Cretaceous period was the land dominated by dinosaurs, and there were only few rat-like mammals. The fossils show that on the line between the Cretaceous period and tertiary period disappeared 2/3 of all animal- and plant-species during a very short time. The dinosaurs died out.
It has not yet been finally clarified what happened in this largest event in life's existence on earth, but maybe the guess of the riddle is found in the thin layer of clay. Where this layer of clay is found in various places on earth it shows that it contains rare elements and minerals, which normally are not found on the surface of the earth, but is known from meteors. Maybe the earth was hit 65 million years ago by a colossal meteor, which whirled up dust and earth into the atmosphere. The sun was eclipsed, maybe for decades, and most animal and plants became extinct. An effect like this can also happen in a large volcanic eruption, but the discovery of a 300 km large, assumed impact-crater in Mexico - age 65 million years - seems to reinforce the meteor-theory.
Ancient privy |
Blå mosaikguldsmed(Aeshna cyanea) |
Parsnip sent out its summer-scent |
Common Ragwort, poisonous |
The idyllic Binderup å-river has avoided destructive regulations. The river has a good fall and a bottom of stone and gravel. In the water is a rich life of small animals and a large population of trout. At Hule Mølle (mill) are fish-steps for the sea-trout.
The exhibition at Vokslev kalkgrube describes the history of the chalk pit and the cultural environment around the river and the mill. There is a parking-place and a resting place with tables and benches.
Vokslev kalkgrube is a part of a biking-route called "Geologisk set" ( Geologically seen) = "Vokslevruten".
Fishing license at Møllegården for a 500 m long stretch af Binderup river south of the mill.
The chalk pit is owned by the Danish state, while the river valley and the slope at the river are private.
Along the Vokslev-nature path on a windy day in the sunny flower-field. |
Nibe |
The small town Nibe (ab. 4.500 inhabitants) has a beautiful place by Limfjorden. It started as a fishing village in the Middle ages, especially had it a rich herring-fishing and trade with the Hanseatics, which brought wealth to the town. The old part of town has kept some of its medieval mark in the cosy streets with the low houses.
Troldkirke |
Troldkirke.
Upon a hill with a fantastic view to the waters of Limfjorden lies one of the finest long dolmens in Denmark. It is about 60 m long, 12 m broad and surrounded by 47 large stones, of which the gable stones are several meters tall. The dolmen is called Troldkirken (the Troll-church), because a troll on the other side of Limfjorden once got mad at Sønderholm church. The troll hated the bell-ringing and threw a giant stone across the fjord in order to crush the tower. The stone ended at the place Troldkirke. It is the cover stone, which weighs supposedly 6-8 tons.
Klitgård Fishing-place |
Source: Kulturhistorie,.dk, Politikens store Danmarksbog, Se dit Danmark.
photo Vokslev 2007; Nibe,Troldkirke, Klitgård 2006: grethe bachmann.