Lofoten Himmeltindan, Norway'da 964 metre yüksekliğe sahiptir, Scandinavian Mountains'ın bir parçası, Europe.
Bu zirve Fold Mountain olarak sınıflandırılır.
Yükselti
964 m
Belirginlik
— m
Koordinatlar
68,195833, 14,450000
Tür
fold_mountain
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Yükselti Karşılaştırması
Bu dağ hakkında
Lofoten Himmeltindan (964m) is a fold mountain in the Scandinavian Mountains, Norway. Grade 2/5: moderate trek requiring good fitness. A Scandinavian peak characterized by glacially sculpted terrain, fjord vistas, and Arctic or subarctic conditions.
The topographic contour map of Lofoten Himmeltindan (964m) in the Scandinavian Mountains 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 964m summit).
Yükseklik profili
The east–west elevation profile of Lofoten Himmeltindan (964m) in the Scandinavian Mountains shows the terrain cross-section through the summit at 964m. 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 Lofoten Himmeltindan (964m) 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 Lofoten Himmeltindan (964m) from west to east, passing through the summit at 964m. 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.
Lofoten Himmeltindan (964m) 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.
