Mount Superamare cao 3668 mét tại Papua New Guinea, thuộc Owen Stanley Range, Oceania.
Đỉnh này được phân loại là Fold Mountain.
Độ cao
3668 m
Độ nổi bật
— m
Tọa độ
-6,383000, 147,200000
Loại
fold_mountain
On this page
So sánh độ cao
Về ngọn núi này
Mount Superamare (3668m) is a fold mountain in the Owen Stanley Range, Papua New Guinea. Grade 4/5: technical ascent requiring mountaineering skills. A remote Pacific peak rising through dense tropical forest into alpine zones, with challenging access and dramatic relief.
The topographic contour map of Mount Superamare (3668m) in the Owen Stanley Range 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 3,668m summit).
Hồ sơ độ cao
The east–west elevation profile of Mount Superamare (3668m) in the Owen Stanley Range shows the terrain cross-section through the summit at 3,668m. 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 Superamare (3668m) 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 Superamare (3668m) from west to east, passing through the summit at 3,668m. 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 Superamare (3668m) 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.
