Beinn a' Bhuird terletak pada ketinggian 1197 meter di United Kingdom, bagian dari Scottish Highlands, Europe.
Puncak ini diklasifikasikan sebagai Fold Mountain.
Ketinggian
1197 m
Prominensi
— m
Koordinat
57,043333, -3,580000
Jenis
fold_mountain
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Perbandingan Ketinggian
Tentang gunung ini
Beinn a' Bhuird (1197m) is a fold mountain in the Scottish Highlands, United Kingdom. Grade 2/5: moderate trek requiring good physical fitness. Formed by tectonic compression, it displays layered rock strata typical of fold ranges.
The topographic contour map of Beinn a' Bhuird (1197m) in the Scottish Highlands shows elongated parallel contours following the ridge axis. Contour lines are drawn at 25m intervals, with index contours (thicker lines) every 100m. The hypsometric color scale ranges from green (lower elevations) through yellow and orange to white (highest elevations near the 1,197m summit).
Profil ketinggian
The east–west elevation profile of Beinn a' Bhuird (1197m) in the Scottish Highlands shows the terrain cross-section through the summit at 1,197m. 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 Beinn a' Bhuird (1197m) uses a 25m contour interval. This means each line represents a 25m change in elevation. Closely spaced contours indicate steeper terrain, while widely spaced contours show gentler slopes.
The elevation profile is a cross-section through Beinn a' Bhuird (1197m) from west to east, passing through the summit at 1,197m. 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.
Beinn a' Bhuird (1197m) 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.
