Jabel Marra, Sudan'da 3042 metre yüksekliğe sahiptir, Africa.
Bu zirve Caldera olarak sınıflandırılır.
Yükselti
3042 m
Belirginlik
— m
Koordinatlar
12,953600, 24,275000
Tür
caldera
On this page
Yükselti Karşılaştırması
Volkanik
Bu dağ hakkında
Jabel Marra (3042m) is a peak in Sudan, Sudan. Grade 3/5: strenuous climb with technical sections demanding experience. A notable regional high point with well-established approach routes. Routes involve exposed ridge sections and require careful route-finding.
The topographic contour map of Jabel Marra (3042m) shows near-circular contours that open inward, revealing the collapsed crater basin. 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 3,042m summit).
Yükseklik profili
The east–west elevation profile of Jabel Marra (3042m) shows the terrain cross-section through the summit at 3,042m. 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 Jabel Marra (3042m) 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 Jabel Marra (3042m) from west to east, passing through the summit at 3,042m. 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.
The contour map of Jabel Marra (3042m) reveals a large caldera — a basin formed when the magma chamber beneath the volcano emptied during a massive eruption, causing the summit to collapse inward.
