Mount Anderson se alza a 4150 metros en Antarctica, Antarctica.
Este pico se clasifica como Fold Mountain.
Altitud
4150 m
Prominencia
— m
Coordenadas
-78,450000, -85,516667
Tipo
fold_mountain
On this page
Comparación de altitudes
Sobre esta montaña
Mount Anderson (4150m) is a fold mountain in Antarctica. Grade 5/5: extreme expedition where supplemental oxygen is typically required. A prominent peak rising above surrounding terrain with rewarding routes for experienced mountaineers and hikers.
The topographic contour map of Mount Anderson (4150m) 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 4,150m summit). Above 300m, the estimated snow line at this latitude, contours transition to cooler tones indicating permanent snow and ice.
Perfil de elevación
The east–west elevation profile of Mount Anderson (4150m) shows the terrain cross-section through the summit at 4,150m. 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 300m 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 Mount Anderson (4150m) 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 Anderson (4150m) from west to east, passing through the summit at 4,150m. 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 Mount Anderson (4150m)'s latitude (78°), the estimated permanent snow line is approximately 300m. Since Mount Anderson (4150m) reaches 4,150m, about 3,850m of the mountain extends above the snow line. This is shown as a dashed blue line on the elevation profile.
Mount Anderson (4150m) 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.
