Mount Sumbing은(는) Indonesia에 위치하며 해발 3371 m입니다, Asia.
이 봉우리는 Stratovolcano으로 분류됩니다.
해발 고도
3371 m
독립 높이
— m
좌표
-7.384722, 110.071667
유형
stratovolcano
On this page
해발 고도 비교
화산
이 산에 대하여
Mount Sumbing (3371m) is a stratovolcano in Indonesia, Indonesia. Grade 2/5: moderate trek requiring good physical fitness. This stratovolcano rises steeply from the surrounding terrain with a classic conical profile. Well-marked paths and reasonable gradients make it achievable for fit hikers.
The topographic contour map of Mount Sumbing (3371m) 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 3,371m summit).
고도 프로필
The east–west elevation profile of Mount Sumbing (3371m) shows the terrain cross-section through the summit at 3,371m. 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 Sumbing (3371m) 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 Sumbing (3371m) from west to east, passing through the summit at 3,371m. 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 Sumbing (3371m) 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.
