Mont Blanc du Tacul位于France，海拔4248米, 属于Alps, Europe.
该山峰被归类为Fold Mountain。
海拔
4248 m
相对高度
— m
坐标
45.855556, 6.889167
类型
fold_mountain
On this page
海拔对比
关于这座山
Mont Blanc du Tacul (4248m) is a fold mountain in the Alps, France. Grade 3/5: strenuous climb with technical sections demanding experience. Formed by tectonic compression, it displays layered rock strata typical of fold ranges.
The topographic contour map of Mont Blanc du Tacul (4248m) in the Alps 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 4,248m summit). Above 3,200m, the estimated snow line at this latitude, contours transition to cooler tones indicating permanent snow and ice.
海拔剖面
The east–west elevation profile of Mont Blanc du Tacul (4248m) in the Alps shows the terrain cross-section through the summit at 4,248m. The color gradient transitions from green (valley floor) to white (summit zone), with the red summit marker indicating the peak. The dashed blue snow line at 3,200m marks the approximate elevation above which permanent snow persists year-round.
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 Mont Blanc du Tacul (4248m) 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 Mont Blanc du Tacul (4248m) from west to east, passing through the summit at 4,248m. 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.
At Mont Blanc du Tacul (4248m)'s latitude (46°), the estimated permanent snow line is approximately 3,200m. Since Mont Blanc du Tacul (4248m) reaches 4,248m, about 1,048m of the mountain extends above the snow line. This is shown as a dashed blue line on the elevation profile.
Mont Blanc du Tacul (4248m) 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.
