Mount Bromo находится на высоте 2329 метров в Indonesia, Asia.
Эта вершина классифицируется как Caldera.
Высота
2329 m
Относительная высота
— m
Координаты
-7,943333, 112,953333
Тип
caldera
On this page
Сравнение высот
Вулканический
Об этой горе
Mount Bromo (2329m) is a peak in Indonesia, Indonesia. Grade 1/5: accessible hike with popular trails suitable for beginners. A notable regional high point with well-established approach routes. Clear trails and gentle slopes attract hikers of all experience levels.
The topographic contour map of Mount Bromo (2329m) shows near-circular contours that open inward, revealing the collapsed crater basin. 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 2,329m summit).
Высотный профиль
The east–west elevation profile of Mount Bromo (2329m) shows the terrain cross-section through the summit at 2,329m. 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 Bromo (2329m) 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 Mount Bromo (2329m) from west to east, passing through the summit at 2,329m. 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 Mount Bromo (2329m) 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.
