Taal Volcano, Philippines'da 311 metre yüksekliğe sahiptir, Asia.
Bu zirve Caldera olarak sınıflandırılır.
Yükselti
311 m
Belirginlik
— m
Koordinatlar
14,002200, 120,993600
Tür
caldera
On this page
Yükselti Karşılaştırması
Volkanik
Bu dağ hakkında
Taal Volcano (311m) is a peak in Philippines, Philippines. Grade 1/5: accessible hike with popular trails suitable for beginners. A distinctive summit within its local topography. Clear trails and gentle slopes attract hikers of all experience levels.
The topographic contour map of Taal Volcano (311m) shows near-circular contours that open inward, revealing the collapsed crater basin. Contour lines are drawn at 10m intervals, with index contours (thicker lines) every 50m. The hypsometric color scale ranges from green (lower elevations) through yellow and orange to white (highest elevations near the 311m summit).
Yükseklik profili
The east–west elevation profile of Taal Volcano (311m) shows the terrain cross-section through the summit at 311m. 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 Taal Volcano (311m) uses a 10m contour interval. This means each line represents a 10m change in elevation. Closely spaced contours indicate steeper terrain, while widely spaced contours show gentler slopes.
The elevation profile is a cross-section through Taal Volcano (311m) from west to east, passing through the summit at 311m. 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.
The contour map of Taal Volcano (311m) reveals a large caldera — a basin formed when the magma chamber beneath the volcano emptied during a massive eruption, causing the summit to collapse inward.
