There was a time when the sea covered the lowlands of North Germany, and the waves of a deep bay washed the slopes of the Siebengebirge. Then the bed of the Rhine lay in the highlands, which it gradually washed away until the surface of the river was far, far below the level of its old bed; and then the volcanoes poured forth their streams of lava over the surrounding plains.
In the course of time the surface of the country has changed so that these lava beds now lie on the mountain sides overhanging the valleys of to-day. Some of the volcanoes sent forth melted stones and ashes from their summits, and streams of lava from their sides, while the craters of others cracked and then sank in, throwing their debris over the neighboring country. In the Eifel there are many such funnels which now contain water forming beautiful lakes (Maaren), which add much to the scenery of the Eifel. The Laachersee is the largest of these lakes. In the mean time the channel of the Rhine had been worn away almost to its present level, but the mountains still sent forth their streams of lava, which stopped brooks and filled the ravines, and even the Rhine itself was dammed up by the great stream from Fornicherkopf forming what was formerly the Neuwied. The old lava stream which obstructed the river is still to be seen in a towering wall of rock, extending close beside the road and track that follow the shore.
CRATER AND LAKE ON TOP OF THE MOSENBERGE.
After having made these observations, we descend from the height which afforded us the view of the Vinrt Valley. A clear brook flows through green meadows and variegated fields stretch along the mountain sides, while modest little villages are scattered among the fruit trees. On the other side of the valley rises the Herchenberg, an extinct volcano. As we climb its sides we see traces of the former devastation. Loose ashes cover the ground, bits of mica glittering in the sun, and on the summit we find enormous masses of stone which were melted and then baked together. In the center lies the old crater, a quiet, barren place bearing very little vegetation, but from its wall an excellent view of the surrounding country can be obtained. Not far from this mountain lies the mighty Bausenberg, with its immense, well preserved crater, only one side of which has been broken away, and which is covered with a thick growth of bushes. The ledges of this mountain are full of interest for the mineralogist. Nearer to Lake Laach are the Wahnenkopfe, the proud Veitskopf, and other cone-shaped peaks. To these we direct our steps, and after a long tramp over the rolling, cultivated plateau, we climb the wood-covered sides of the great basin in whose depths the Laachersee lies. From the shore of this lake rise the high volcanic peaks which tower above all the other mountains.
LAKE GEMUNDEN.
Tired from our climb through the ashes, which are heated by the sun, we rest in the shade of a beech-wood, looking through the leaves into the valley below us, with the old cloisters and the high Roman church which the monks once built on the banks of the lake.
THE CRATER OF THE HERCHENBERGES.