The path leads from the former restaurant St. Linhart to the east. Passes the remains of walls of the old Romanesque church of St. Linhart, which formed the basis of the old settlement called Obora (Tiergarten), and the newer chapel (from 1838) of the same initiation. The area was part of the medieval royal fields belonging to the Loket Castle.
The bedrock is built by the medium grained and sometimes porphyric biotite granite of the younger intrusion complex (so called “erzgebirgsgranite”). Quaternary cover in these areas consists of deluvial (slope) sandy loams with a thickness of about 2-3 m. Interesting is the occurrence of small basaltic bodies east of the former restaurant.
Continue to the northeast, passing Russell's cottage, and we wind slightly downhill to a very special place called “Lesní Pobožnost” (“Forest Contemplation”) and then to the stone Book. From this memorial, the path crosses the forest road and goes through a meadow on the edge of the woods when it joins the westernmost part of the spa area, in the Křižíkova Street to the sanatorium Mánes and finally to the traditional tourist restaurant Malé Versailles (“Little Versailles”). In the vicinity of the final parts of the path, the coarse-grained “erzgebirgsgranite” occurs in the form of small rocks and in the road cuts.
The granites of the Karlovy Vary Pluton solidified millions years ago in depth of several kilometres and at temperature of around 700 °C. From the melt rock gradually crystallized major components: feldspar, quartz and mica. These minerals give unmistakable grainy granite structure. Place of creation granite magma lay much deeper, from 20 to 40 km, and possibly even further in the earth's interior. By the collision of two large continents - Laurasia and Gondwana - arose before about 320 million years the Variscan Mountains. In the inner there originates a rock melts which melt slowly rose into the upper crust, where solidified. To the Earth’s surface came the granite after millions of years-long denuding of overlying rocks.