Namhansan está a 522 metros de altitude em South Korea, Asia.
Este pico é classificado como Fold Mountain.
Altitude
522 m
Proeminência
— m
Coordenadas
37,480000, 127,180000
Tipo
fold_mountain
On this page
Comparação de altitudes
Sobre esta montanha
Namhansan (522m) is a fold mountain in South Korea, South Korea. Grade 1/5: accessible hike with popular trails suitable for beginners. Formed by tectonic compression, it displays layered rock strata typical of fold ranges. Clear trails and gentle slopes attract hikers of all experience levels.
The topographic contour map of Namhansan (522m) shows elongated parallel contours following the ridge axis. Contour lines are drawn at 25m intervals, with index contours (thicker lines) every 100m. The hypsometric color scale ranges from green (lower elevations) through yellow and orange to white (highest elevations near the 522m summit).
Perfil de elevação
The east–west elevation profile of Namhansan (522m) shows the terrain cross-section through the summit at 522m. 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 Namhansan (522m) uses a 25m contour interval. This means each line represents a 25m change in elevation. Closely spaced contours indicate steeper terrain, while widely spaced contours show gentler slopes.
The elevation profile is a cross-section through Namhansan (522m) from west to east, passing through the summit at 522m. 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.
Namhansan (522m) 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.
