Piz Ciavazes se alza a 2831 metros en Italy, parte de Dolomites, Europe.
Este pico se clasifica como Fold Mountain.
Altitud
2831 m
Prominencia
— m
Coordenadas
46,508056, 11,761667
Tipo
fold_mountain
On this page
Comparación de altitudes
Sobre esta montaña
Piz Ciavazes (2831m) is a fold mountain in the Dolomites, Italy. Grade 4/5: technical ascent requiring mountaineering skills. A well-known Alpine summit offering rewarding views and accessible routes for fit hikers.
The topographic contour map of Piz Ciavazes (2831m) 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 2,831m summit).
Perfil de elevación
The east–west elevation profile of Piz Ciavazes (2831m) in the Dolomites shows the terrain cross-section through the summit at 2,831m. 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 Piz Ciavazes (2831m) 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 Piz Ciavazes (2831m) from west to east, passing through the summit at 2,831m. 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.
Piz Ciavazes (2831m) 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.
