Hachimantai, Japan'da 1613 metre yüksekliğe sahiptir, Asia.
Bu zirve Shield Volcano olarak sınıflandırılır.
Yükselti
1613 m
Belirginlik
— m
Koordinatlar
39,957500, 140,853611
Tür
shield_volcano
On this page
Yükselti Karşılaştırması
Volkanik
Bu dağ hakkında
Hachimantai (1613m) is a shield volcano in Japan, Japan. Grade 1/5: accessible hike with popular trails suitable for beginners. Its broad shield form reflects effusive volcanic activity over geological time. Clear trails and gentle slopes attract hikers of all experience levels.
The topographic contour map of Hachimantai (1613m) shows widely spaced, gently curving contours reflecting broad, low-angle slopes. 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 1,613m summit).
Yükseklik profili
The east–west elevation profile of Hachimantai (1613m) shows the terrain cross-section through the summit at 1,613m. 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 Hachimantai (1613m) 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 Hachimantai (1613m) from west to east, passing through the summit at 1,613m. 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.
Hachimantai (1613m) is a shield volcano, built almost entirely from fluid lava flows. The contour map shows widely spaced lines, reflecting slopes that rarely exceed 5–10 degrees — much gentler than a stratovolcano.
