Taebaeksan stands at 1567 meters in South Korea, Asia.
This peak is classified as a Fold Mountain.
Elevation
1567 m
Prominence
— m
Coordinates
37.093611, 128.915556
Type
fold_mountain
On this page
Elevation Comparison
About This Mountain
Taebaeksan (1567m) 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 Taebaeksan (1567m) shows elongated parallel contours following the ridge axis. Contour lines are drawn at 50m intervals, with index contours (thicker lines) every 250m. The hypsometric color scale ranges from green (lower elevations) through yellow and orange to white (highest elevations near the 1,567m summit).
Elevation Profile
The east–west elevation profile of Taebaeksan (1567m) shows the terrain cross-section through the summit at 1,567m. 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 Taebaeksan (1567m) uses a 50m contour interval. This means each line represents a 50m change in elevation. Closely spaced contours indicate steeper terrain, while widely spaced contours show gentler slopes.
The elevation profile is a cross-section through Taebaeksan (1567m) from west to east, passing through the summit at 1,567m. 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.
Taebaeksan (1567m) 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.
