Jabal An-Nabi Shu'ayb находится на высоте 3666 метров в Yemen, Asia.
Эта вершина классифицируется как Fold Mountain.
Высота
3666 m
Относительная высота
— m
Координаты
15,283333, 43,950000
Тип
fold_mountain
On this page
Сравнение высот
Об этой горе
Jabal An-Nabi Shu'ayb (3666m) is a fold mountain in Yemen. Grade 2/5: moderate trek requiring good fitness. A notable mountain summit offering dramatic scenery and varied climbing terrain for those with alpine experience.
The topographic contour map of Jabal An-Nabi Shu'ayb (3666m) 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 3,666m summit).
Высотный профиль
The east–west elevation profile of Jabal An-Nabi Shu'ayb (3666m) shows the terrain cross-section through the summit at 3,666m. 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 Jabal An-Nabi Shu'ayb (3666m) 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 Jabal An-Nabi Shu'ayb (3666m) from west to east, passing through the summit at 3,666m. 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.
Jabal An-Nabi Shu'ayb (3666m) 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.
