Kaimon-dake se alza a 924 metros en Japan, Asia.
Este pico se clasifica como Stratovolcano.
Altitud
924 m
Prominencia
— m
Coordenadas
31,200000, 130,564167
Tipo
stratovolcano
On this page
Comparación de altitudes
Volcánico
Sobre esta montaña
Kaimon-dake (924m) is a stratovolcano in Japan, Japan. Grade 1/5: accessible hike with popular trails suitable for beginners. This stratovolcano rises steeply from the surrounding terrain with a classic conical profile. Clear trails and gentle slopes attract hikers of all experience levels.
The topographic contour map of Kaimon-dake (924m) shows near-circular, closely spaced contours indicating steep conical slopes. 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 924m summit).
Perfil de elevación
The east–west elevation profile of Kaimon-dake (924m) shows the terrain cross-section through the summit at 924m. 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 Kaimon-dake (924m) 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 Kaimon-dake (924m) from west to east, passing through the summit at 924m. 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.
As a stratovolcano, Kaimon-dake (924m) was built by alternating layers of lava and ash. The summit crater is visible on the contour map as a small depression within the tightly spaced concentric contours near the peak.
