Stony debrises

The debris-covered peak of the Tetřeví vrch hill near Mlýny is overgrown by wood.


The slopes of Studenec hill are covered with vast fields of slope debris.
The debris fields on the slopes of Studenec hill consist of basalt blocks with approximately equal sizes.
From the debris slopes of the Studenec hill we have beautiful views into the surrounding landscape. On the right side we see the Lipnický vrch hill, behind of him the low range of the Jehla and in the background left there is the Zámecký vrch hill near of Česká Kamenice.
Through a debris field on the southwestern slope of Studenec hill leads a still visible old path.
An old path leading over the debris field on the southwestern slope of the Klíč hill.
The greatest debris fields are on the southern slope of the Studenec hill.
The debris fields on the Studenec are from all sides surrounded by wood.
During autumn the debris field of the Studenec are flanked by golden beeches.
A debris field under the peak of Studenec hill.
The borders of the debris fields here and there are flanked by tall-trunk trees.


The fields on the slopes of Studenec hill covered by phonolithe debris consist of relatively great boulders with dimensions sometimes exceeding 1 meter.
View from the peak of the Malý Stožec hill over its debris fields on the woods of its surroundings.
The debris fields of the Malý Stožec hill are on places overgrown with beeches and birches.
On the Malý Stožec a mosaic of diverse wild rocks, debris fields and woods had developed.
Rock debris on the northeastern slope of Malý Stožec hill.

The southwestern slope of Malý Stožec hill is covered by fields of phonolithic debris which on places merge into small open woods covering the debris fields.
The marked tourist path leading to the peak of Malý Stožec traverses debris fields.
Phonolithe detritus under the northern peak of Suchý vrch-hill.


Phonolithe debris on the slopes of Jedlová-hill.
Debris slope at the Chřibský vrch-hill.
A till now used old path to the southern peak od Hvozd hill climbs over a debris field overgrown by open wood.
Basaltic debris on the slope of the Střední vrch.


The most famous debris field of the Lužické hory mountains is on the southwestern slope of the Klíč hill.
Towards evening the debris field on the slope of Klíč hill is covered with shadows.
Foxgloves in the wood under the Klíč-hill.
The edge of the debris field on the Klíč hill is overgrown by an open forest.
The northern edge of the debris field of the Klíč hill.

The debris field of the Klíč hill looks beautifully also during winter.
The freshly snow-covered debris field on the Klíč hill has an extraordinary magic.
The debris fields on the Klíč hill have an extraordinary magic also on frosty days.
The debris of the slope of Klíč hill covered by white frost disappears in the frosty fog.
In the wintery fog it seems that on the Klíč hill the time is coming to a standstill.
Early frost at the north slope of Klíč hill.
During early spring the snow covering the debris fields of Klíč hill thaws only slowly.