Cerro Mohinora liegt auf 3250 Metern Höhe in Mexico, Teil der Sierra Madre, North America.
Dieser Gipfel wird als Fold Mountain klassifiziert.
Höhe
3250 m
Prominenz
— m
Koordinaten
26,090278, -107,053889
Typ
fold_mountain
On this page
Höhenvergleich
Über diesen Berg
Cerro Mohinora (3250m) 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 Mohinora (3250m) in the Sierra Madre 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 3,250m summit).
Höhenprofil
The east–west elevation profile of Cerro Mohinora (3250m) in the Sierra Madre shows the terrain cross-section through the summit at 3,250m. 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 Mohinora (3250m) 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 Cerro Mohinora (3250m) from west to east, passing through the summit at 3,250m. 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 Mohinora (3250m) 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.
