Djebel Ank cao 1544 mét tại Tunisia, thuộc Atlas Mountains, Africa.
Đỉnh này được phân loại là Fold Mountain.
Độ cao
1544 m
Độ nổi bật
— m
Tọa độ
35,650000, 8,500000
Loại
fold_mountain
On this page
So sánh độ cao
Về ngọn núi này
Djebel Ank (1544m) is a fold mountain in the Atlas Mountains, Tunisia. Grade 1/5: accessible hike. A regional summit offering rewarding walks through varied landscapes with notable views from the top.
The topographic contour map of Djebel Ank (1544m) in the Atlas Mountains 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 1,544m summit).
Hồ sơ độ cao
The east–west elevation profile of Djebel Ank (1544m) in the Atlas Mountains shows the terrain cross-section through the summit at 1,544m. 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 Djebel Ank (1544m) 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 Djebel Ank (1544m) from west to east, passing through the summit at 1,544m. 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.
Djebel Ank (1544m) 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.
