Cerro PotosiはMexicoに位置し、標高3713 mです, Sierra Madreの一部, North America.
この山はFold Mountainに分類されます。
標高
3713 m
山頂卓越度
— m
座標
24.882500, -99.983056
種別
fold_mountain
On this page
標高比較
この山について
Cerro Potosi (3713m) is a fold mountain in the Sierra Madre, Mexico. Grade 2/5: moderate trek requiring good fitness. A notable mountain summit offering dramatic scenery and varied climbing terrain for those with alpine experience.
The topographic contour map of Cerro Potosi (3713m) in the Sierra Madre 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 3,713m summit).
標高プロフィール
The east–west elevation profile of Cerro Potosi (3713m) in the Sierra Madre shows the terrain cross-section through the summit at 3,713m. The color gradient transitions from green (valley floor) to white (summit zone), with the red summit marker indicating the peak.
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 Potosi (3713m) 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 Potosi (3713m) from west to east, passing through the summit at 3,713m. 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.
Cerro Potosi (3713m) 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.
