Monte Sibilla ตั้งอยู่ที่ความสูง 2173 เมตร ในItaly, เป็นส่วนหนึ่งของApennines, Europe.
ยอดเขานี้จัดอยู่ในประเภท Fold Mountain
ความสูง
2173 m
ความโดดเด่น
— m
พิกัด
42.873333, 13.255833
ประเภท
fold_mountain
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Monte Sibilla (2173m) is a fold mountain in the Apennines, Italy. Grade 1/5: accessible hike. A well-known Alpine summit offering rewarding views and accessible routes for fit hikers.
The topographic contour map of Monte Sibilla (2173m) in the Apennines 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 2,173m summit).
โปรไฟล์ระดับความสูง
The east–west elevation profile of Monte Sibilla (2173m) in the Apennines shows the terrain cross-section through the summit at 2,173m. 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 Monte Sibilla (2173m) 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 Monte Sibilla (2173m) from west to east, passing through the summit at 2,173m. 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.
Monte Sibilla (2173m) 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.
