Mount Suckling terletak pada ketinggian 3676 meter di Papua New Guinea, bagian dari Owen Stanley Range, Oceania.
Puncak ini diklasifikasikan sebagai Fold Mountain.
Ketinggian
3676 m
Prominensi
— m
Koordinat
-9,650000, 148,016700
Jenis
fold_mountain
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Perbandingan Ketinggian
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Mount Suckling (3676m) 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 Suckling (3676m) 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 3,676m summit).
Profil ketinggian
The east–west elevation profile of Mount Suckling (3676m) in the Owen Stanley Range shows the terrain cross-section through the summit at 3,676m. 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 Suckling (3676m) 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 Suckling (3676m) from west to east, passing through the summit at 3,676m. 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 Suckling (3676m) 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.
