Pedra do Sino culmine à 2263 mètres en Brazil, South America.
Ce sommet est classé comme Fold Mountain.
Altitude
2263 m
Proéminence
— m
Coordonnées
-22,451944, -43,181944
Type
fold_mountain
On this page
Comparaison des altitudes
À propos de cette montagne
Pedra do Sino (2263m) is a fold mountain in Brazil. Grade 3/5: strenuous climb with technical sections. A well-regarded peak in its region, offering accessible terrain and panoramic views for fit hikers.
The topographic contour map of Pedra do Sino (2263m) 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 2,263m summit).
Profil d'altitude
The east–west elevation profile of Pedra do Sino (2263m) shows the terrain cross-section through the summit at 2,263m. 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 Pedra do Sino (2263m) 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 Pedra do Sino (2263m) from west to east, passing through the summit at 2,263m. 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.
Pedra do Sino (2263m) 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.
