Naude's Nek Pass está a 2589 metros de altitude em South Africa, parte de Drakensberg, Africa.
Este pico é classificado como Fold Mountain.
Altitude
2589 m
Proeminência
— m
Coordenadas
-30,933300, 28,366700
Tipo
fold_mountain
On this page
Comparação de altitudes
Sobre esta montanha
Naude's Nek Pass (2589m) is a fold mountain in the Drakensberg, South Africa. Grade 2/5: moderate trek requiring good fitness. An African peak dominating the surrounding landscape, offering panoramic views across forests and savanna plains.
The topographic contour map of Naude's Nek Pass (2589m) 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 2,589m summit).
Perfil de elevação
The east–west elevation profile of Naude's Nek Pass (2589m) in the Drakensberg shows the terrain cross-section through the summit at 2,589m. 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 Naude's Nek Pass (2589m) 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 Naude's Nek Pass (2589m) from west to east, passing through the summit at 2,589m. 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.
Naude's Nek Pass (2589m) 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.
