Torres del Paine stands at 2884 meters in Chile, part of the Patagonian Andes, South America.
This peak is classified as a Fold Mountain.
Elevation
2884 m
Prominence
— m
Coordinates
-51.003333, -73.003889
Type
fold_mountain
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Elevation Comparison
About This Mountain
Torres del Paine (2884m) is a fold mountain in the Patagonian Andes, Chile. Grade 5/5: extreme expedition where supplemental oxygen is typically required. Formed by tectonic compression, it displays layered rock strata typical of fold ranges.
The topographic contour map of Torres del Paine (2884m) in the Patagonian Andes 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 2,884m summit). Above 2,500m, the estimated snow line at this latitude, contours transition to cooler tones indicating permanent snow and ice.
Elevation Profile
The east–west elevation profile of Torres del Paine (2884m) in the Patagonian Andes shows the terrain cross-section through the summit at 2,884m. 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 2,500m 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 Torres del Paine (2884m) 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 Torres del Paine (2884m) from west to east, passing through the summit at 2,884m. 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 Torres del Paine (2884m)'s latitude (51°), the estimated permanent snow line is approximately 2,500m. Since Torres del Paine (2884m) reaches 2,884m, about 384m of the mountain extends above the snow line. This is shown as a dashed blue line on the elevation profile.
Torres del Paine (2884m) 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.
