Nevado Santa Isabel cao 4965 mét tại Colombia, thuộc Andes, South America.
Đỉnh này được phân loại là Stratovolcano.
Độ cao
4965 m
Độ nổi bật
— m
Tọa độ
4,816667, -75,383333
Loại
stratovolcano
On this page
So sánh độ cao
Núi lửa
Về ngọn núi này
Nevado Santa Isabel (4965m) is a stratovolcano in the Andes, Colombia. 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 Nevado Santa Isabel (4965m) in the Andes 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 4,965m summit).
Hồ sơ độ cao
The east–west elevation profile of Nevado Santa Isabel (4965m) in the Andes shows the terrain cross-section through the summit at 4,965m. 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 Nevado Santa Isabel (4965m) 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 Nevado Santa Isabel (4965m) from west to east, passing through the summit at 4,965m. 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, Nevado Santa Isabel (4965m) 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.
