Sani Pass terletak pada ketinggian 2874 meter di Lesotho, bagian dari Drakensberg, Africa.
Puncak ini diklasifikasikan sebagai Fold Mountain.
Ketinggian
2874 m
Prominensi
— m
Koordinat
-29,583300, 29,283300
Jenis
fold_mountain
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Perbandingan Ketinggian
Tentang gunung ini
Sani Pass (2874m) is a fold mountain in the Drakensberg, Lesotho. 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 Sani Pass (2874m) in the Drakensberg 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 2,874m summit).
Profil ketinggian
The east–west elevation profile of Sani Pass (2874m) in the Drakensberg shows the terrain cross-section through the summit at 2,874m. 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 Sani Pass (2874m) 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 Sani Pass (2874m) from west to east, passing through the summit at 2,874m. 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.
Sani Pass (2874m) 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.
