Cerro Solo terletak pada ketinggian 6205 meter di Argentina, bagian dari Andes, South America.
Puncak ini diklasifikasikan sebagai Fold Mountain.
Ketinggian
6205 m
Prominensi
— m
Koordinat
-49,200000, -73,066667
Jenis
fold_mountain
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Perbandingan Ketinggian
Tentang gunung ini
Cerro Solo (6205m) is a fold mountain in the Andes, Argentina. Grade 4/5: technical ascent requiring mountaineering skills and equipment. Formed by tectonic compression, it displays layered rock strata typical of fold ranges.
The topographic contour map of Cerro Solo (6205m) in the Andes 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 6,205m summit). Above 3,200m, the estimated snow line at this latitude, contours transition to cooler tones indicating permanent snow and ice.
Profil ketinggian
The east–west elevation profile of Cerro Solo (6205m) in the Andes shows the terrain cross-section through the summit at 6,205m. 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 Cerro Solo (6205m) 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 Cerro Solo (6205m) from west to east, passing through the summit at 6,205m. 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 Cerro Solo (6205m)'s latitude (49°), the estimated permanent snow line is approximately 3,200m. Since Cerro Solo (6205m) reaches 6,205m, about 3,005m of the mountain extends above the snow line. This is shown as a dashed blue line on the elevation profile.
Cerro Solo (6205m) 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.
