Cerro El Plomo은(는) Chile에 위치하며 해발 5424 m입니다, Andes 소속, South America.
이 봉우리는 Fold Mountain으로 분류됩니다.
해발 고도
5424 m
독립 높이
— m
좌표
-33.233333, -70.233333
유형
fold_mountain
On this page
해발 고도 비교
이 산에 대하여
Cerro El Plomo (5424m) is a fold mountain in the Andes, Chile. Grade 3/5: strenuous climb with technical sections demanding experience. Formed by tectonic compression, it displays layered rock strata typical of fold ranges. Routes involve exposed ridge sections and require careful route-finding.
The topographic contour map of Cerro El Plomo (5424m) 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 5,424m summit). Above 3,800m, the estimated snow line at this latitude, contours transition to cooler tones indicating permanent snow and ice.
고도 프로필
The east–west elevation profile of Cerro El Plomo (5424m) in the Andes shows the terrain cross-section through the summit at 5,424m. 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 3,800m 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 El Plomo (5424m) 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 El Plomo (5424m) from west to east, passing through the summit at 5,424m. 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 El Plomo (5424m)'s latitude (33°), the estimated permanent snow line is approximately 3,800m. Since Cerro El Plomo (5424m) reaches 5,424m, about 1,624m of the mountain extends above the snow line. This is shown as a dashed blue line on the elevation profile.
Cerro El Plomo (5424m) 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.
