Yushan Xifeng culmine à 3518 mètres en Taiwan, Asia.
Ce sommet est classé comme Fold Mountain.
Altitude
3518 m
Proéminence
— m
Coordonnées
23,466700, 120,933300
Type
fold_mountain
On this page
Comparaison des altitudes
À propos de cette montagne
Yushan Xifeng (3518m) is a fold mountain in Taiwan, Taiwan. Grade 3/5: strenuous climb with technical sections demanding experience. Formed by tectonic compression, it displays layered rock strata typical of fold ranges. Routes involve exposed ridge sections and require careful route-finding.
The topographic contour map of Yushan Xifeng (3518m) 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 3,518m summit).
Profil d'altitude
The east–west elevation profile of Yushan Xifeng (3518m) shows the terrain cross-section through the summit at 3,518m. 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 Yushan Xifeng (3518m) 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 Yushan Xifeng (3518m) from west to east, passing through the summit at 3,518m. 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.
Yushan Xifeng (3518m) 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.
