Mount Bangeta은(는) Papua New Guinea에 위치하며 해발 3996 m입니다, Owen Stanley Range 소속, Oceania.
이 봉우리는 Fold Mountain으로 분류됩니다.
해발 고도
3996 m
독립 높이
— m
좌표
-6.333000, 146.933000
유형
fold_mountain
On this page
해발 고도 비교
이 산에 대하여
Mount Bangeta (3996m) 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 Bangeta (3996m) 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 3,996m summit).
고도 프로필
The east–west elevation profile of Mount Bangeta (3996m) in the Owen Stanley Range shows the terrain cross-section through the summit at 3,996m. 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 Bangeta (3996m) 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 Bangeta (3996m) from west to east, passing through the summit at 3,996m. 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 Bangeta (3996m) 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.
