Cima di Vezzana liegt auf 3192 Metern Höhe in Italy, Teil der Dolomites, Europe.
Dieser Gipfel wird als Fold Mountain klassifiziert.
Höhe
3192 m
Prominenz
— m
Koordinaten
46,300000, 11,833333
Typ
fold_mountain
On this page
Höhenvergleich
Über diesen Berg
Cima di Vezzana (3192m) is a fold mountain in the Dolomites, Italy. Grade 3/5: strenuous climb with technical sections demanding experience. Formed by tectonic compression, it displays layered rock strata typical of fold ranges.
The topographic contour map of Cima di Vezzana (3192m) in the Dolomites shows elongated parallel contours following the ridge axis. Contour lines are drawn at 50m intervals, with index contours (thicker lines) every 250m. The hypsometric color scale ranges from green (lower elevations) through yellow and orange to white (highest elevations near the 3,192m summit).
Höhenprofil
The east–west elevation profile of Cima di Vezzana (3192m) in the Dolomites shows the terrain cross-section through the summit at 3,192m. The color gradient transitions from green (valley floor) to white (summit zone), with the red summit marker indicating the peak.
Frequently Asked Questions
The contour map uses a hypsometric color scale where green represents lower elevations, yellow and orange indicate mid-range altitudes, and white marks the highest zones near the summit. Thicker contour lines (index contours) are drawn at wider intervals to help you quickly estimate elevation.
The contour map of Cima di Vezzana (3192m) uses a 50m contour interval. This means each line represents a 50m change in elevation. Closely spaced contours indicate steeper terrain, while widely spaced contours show gentler slopes.
The elevation profile is a cross-section through Cima di Vezzana (3192m) from west to east, passing through the summit at 3,192m. It reveals the mountain's shape, steepness, and relative height compared to the surrounding terrain. The horizontal axis shows distance in kilometers from the peak.
Cima di Vezzana (3192m) was formed by tectonic folding, which compressed rock layers into long, parallel ridges. The contour map shows elongated lines that follow the axis of the fold, rather than circular patterns.
