Mount Loolmalasin cao 3648 mét tại Tanzania, Africa.
Đỉnh này được phân loại là Fault-Block Mountain.
Độ cao
3648 m
Độ nổi bật
— m
Tọa độ
-3,150000, 35,833000
Loại
fault_block
On this page
So sánh độ cao
Về ngọn núi này
Mount Loolmalasin (3648m) is a fault-block mountain in Tanzania. 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 Mount Loolmalasin (3648m) shows asymmetric contours — closely packed on the fault scarp, wider on the dip slope. 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 3,648m summit).
Hồ sơ độ cao
The east–west elevation profile of Mount Loolmalasin (3648m) shows the terrain cross-section through the summit at 3,648m. 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 Mount Loolmalasin (3648m) 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 Mount Loolmalasin (3648m) from west to east, passing through the summit at 3,648m. 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.
Mount Loolmalasin (3648m) is a fault-block mountain, tilted upward along a geological fault. One side shows tightly packed contours (the steep fault scarp), while the opposite side has wider spacing (the gentler dip slope).
