Mutnovsky Volcano terletak pada ketinggian 2322 meter di Russia, Europe.
Puncak ini diklasifikasikan sebagai Stratovolcano.
Ketinggian
2322 m
Prominensi
— m
Koordinat
52,450000, 158,200000
Jenis
stratovolcano
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Perbandingan Ketinggian
Vulkanik
Tentang gunung ini
Mutnovsky Volcano (2322m) is a stratovolcano in Russia. Grade 3/5: strenuous climb with technical sections. A well-regarded peak in its region, offering accessible terrain and panoramic views for fit hikers.
The topographic contour map of Mutnovsky Volcano (2322m) shows near-circular, closely spaced contours indicating steep conical 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 2,322m summit).
Profil ketinggian
The east–west elevation profile of Mutnovsky Volcano (2322m) shows the terrain cross-section through the summit at 2,322m. 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 Mutnovsky Volcano (2322m) 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 Mutnovsky Volcano (2322m) from west to east, passing through the summit at 2,322m. 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, Mutnovsky Volcano (2322m) 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.
