Ol Doinyo Lengai은(는) Tanzania에 위치하며 해발 2962 m입니다, East African Rift 소속, Africa.
이 봉우리는 Stratovolcano으로 분류됩니다.
해발 고도
2962 m
독립 높이
— m
좌표
-2.766667, 35.916667
유형
stratovolcano
On this page
해발 고도 비교
화산
이 산에 대하여
Ol Doinyo Lengai (2962m) is a stratovolcano in the East African Rift, Tanzania. Grade 3/5: strenuous climb with technical sections demanding experience. This stratovolcano rises steeply from the surrounding terrain with a classic conical profile.
The topographic contour map of Ol Doinyo Lengai (2962m) in the East African Rift 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 2,962m summit).
고도 프로필
The east–west elevation profile of Ol Doinyo Lengai (2962m) in the East African Rift shows the terrain cross-section through the summit at 2,962m. 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 Ol Doinyo Lengai (2962m) 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 Ol Doinyo Lengai (2962m) from west to east, passing through the summit at 2,962m. 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, Ol Doinyo Lengai (2962m) 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.
