Mount Mikeno은(는) DR Congo에 위치하며 해발 4437 m입니다, Virunga Mountains 소속, Africa.
이 봉우리는 Stratovolcano으로 분류됩니다.
해발 고도
4437 m
독립 높이
— m
좌표
-1.447000, 29.449000
유형
stratovolcano
On this page
해발 고도 비교
화산
이 산에 대하여
Mount Mikeno (4437m) is a stratovolcano in the Virunga Mountains, DR Congo. Grade 5/5: extreme expedition where supplemental oxygen is typically required. A prominent peak rising above surrounding terrain with rewarding routes for experienced mountaineers and hikers.
The topographic contour map of Mount Mikeno (4437m) in the Virunga Mountains shows near-circular, closely spaced contours indicating steep conical slopes. Contour lines are drawn at 100m intervals, with index contours (thicker lines) every 500m. The hypsometric color scale ranges from green (lower elevations) through yellow and orange to white (highest elevations near the 4,437m summit).
고도 프로필
The east–west elevation profile of Mount Mikeno (4437m) in the Virunga Mountains shows the terrain cross-section through the summit at 4,437m. 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 Mount Mikeno (4437m) uses a 100m contour interval. This means each line represents a 100m change in elevation. Closely spaced contours indicate steeper terrain, while widely spaced contours show gentler slopes.
The elevation profile is a cross-section through Mount Mikeno (4437m) from west to east, passing through the summit at 4,437m. 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, Mount Mikeno (4437m) 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.
