Injasuti terletak pada ketinggian 3459 meter di South Africa, bagian dari Drakensberg, Africa.
Puncak ini diklasifikasikan sebagai Fold Mountain.
Ketinggian
3459 m
Prominensi
— m
Koordinat
-29,066700, 29,566700
Jenis
fold_mountain
On this page
Perbandingan Ketinggian
Tentang gunung ini
Injasuti (3459m) is a fold mountain in the Drakensberg, South Africa. Grade 3/5: strenuous climb with technical sections. An African peak dominating the surrounding landscape, offering panoramic views across forests and savanna plains.
The topographic contour map of Injasuti (3459m) in the Drakensberg shows elongated parallel contours following the ridge axis. Contour lines are drawn at 100m intervals, with index contours (thicker lines) every 500m. The hypsometric color scale ranges from green (lower elevations) through yellow and orange to white (highest elevations near the 3,459m summit).
Profil ketinggian
The east–west elevation profile of Injasuti (3459m) in the Drakensberg shows the terrain cross-section through the summit at 3,459m. 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 Injasuti (3459m) uses a 100m contour interval. This means each line represents a 100m change in elevation. Closely spaced contours indicate steeper terrain, while widely spaced contours show gentler slopes.
The elevation profile is a cross-section through Injasuti (3459m) from west to east, passing through the summit at 3,459m. 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.
Injasuti (3459m) 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.
