يقع Mount Flume على ارتفاع 1328 متر في United States, جزء من Appalachian Mountains, North America.
تُصنّف هذه القمة على أنها Fold Mountain.
الارتفاع
1328 m
البروز
— m
الإحداثيات
44,108900, -71,627800
النوع
fold_mountain
On this page
مقارنة الارتفاعات
عن هذا الجبل
Mount Flume (1328m) is a fold mountain in the Appalachian Mountains, United States. Grade 2/5: moderate trek requiring good physical fitness. Formed by tectonic compression, it displays layered rock strata typical of fold ranges.
The topographic contour map of Mount Flume (1328m) in the Appalachian Mountains shows elongated parallel contours following the ridge axis. Contour lines are drawn at 25m intervals, with index contours (thicker lines) every 100m. The hypsometric color scale ranges from green (lower elevations) through yellow and orange to white (highest elevations near the 1,328m summit).
المخطط الارتفاعي
The east–west elevation profile of Mount Flume (1328m) in the Appalachian Mountains shows the terrain cross-section through the summit at 1,328m. 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 Flume (1328m) uses a 25m contour interval. This means each line represents a 25m 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 Flume (1328m) from west to east, passing through the summit at 1,328m. 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.
Mount Flume (1328m) was formed by tectonic folding, which compressed rock layers into long, parallel ridges. The contour map shows elongated lines that follow the axis of the fold, rather than circular patterns.
