يقع Coma Pedrosa على ارتفاع 2942 متر في Andorra, جزء من Pyrenees, Europe.
تُصنّف هذه القمة على أنها Fold Mountain.
الارتفاع
2942 m
البروز
— m
الإحداثيات
42,591667, 1,444167
النوع
fold_mountain
On this page
مقارنة الارتفاعات
عن هذا الجبل
Coma Pedrosa (2942m) is a fold mountain in the Pyrenees, Andorra. Grade 2/5: moderate trek requiring good physical fitness. Formed by tectonic compression, it displays layered rock strata typical of fold ranges. Well-marked paths and reasonable gradients make it achievable for fit hikers.
The topographic contour map of Coma Pedrosa (2942m) in the Pyrenees 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 2,942m summit).
المخطط الارتفاعي
The east–west elevation profile of Coma Pedrosa (2942m) in the Pyrenees shows the terrain cross-section through the summit at 2,942m. 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 Coma Pedrosa (2942m) 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 Coma Pedrosa (2942m) from west to east, passing through the summit at 2,942m. 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.
Coma Pedrosa (2942m) 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.
