Meesapulimala culmine à 2640 mètres en India, faisant partie de Western Ghats, Asia.
Ce sommet est classé comme Fold Mountain.
Altitude
2640 m
Proéminence
— m
Coordonnées
10,083333, 77,216667
Type
fold_mountain
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Comparaison des altitudes
À propos de cette montagne
Meesapulimala (2640m) is a fold mountain in the Western Ghats, India. Grade 2/5: moderate trek requiring good fitness. A well-regarded peak in its region, offering accessible terrain and panoramic views for fit hikers.
The topographic contour map of Meesapulimala (2640m) in the Western Ghats 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 2,640m summit).
Profil d'altitude
The east–west elevation profile of Meesapulimala (2640m) in the Western Ghats shows the terrain cross-section through the summit at 2,640m. 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 Meesapulimala (2640m) 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 Meesapulimala (2640m) from west to east, passing through the summit at 2,640m. 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.
Meesapulimala (2640m) 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.
