Himalayas
A flagship mountain record tying together altitude, ice, river headwaters, and connected upland systems.
The mountain hub collects major ranges, elevated landforms, and cryosphere-linked uplands. It supports records focused on relief, elevation, glaciers, source basins, and the structure of linked highland regions.
These pages give the mountain section a stable spine and enough depth to support future additions like volcanic arcs, plateaus, and alpine basins.
A flagship mountain record tying together altitude, ice, river headwaters, and connected upland systems.
A high-latitude mountain arc shaped by active faults, central massifs, valley glaciers, river headwaters, and a strong climate divide.
An Arctic mountain system shaped by folded ridges, glacial valleys, permafrost, divided drainage, and a strong climate boundary.
A continental-scale cordillera linking volcanic belts, altiplano basins, Pacific margins, and sharp climatic contrasts.
A compact European highland system known for classic alpine landforms, glaciation, and major watershed divides.
New Zealand's axial mountain range, shaped by Alpine Fault uplift, glacial relief, divided drainage, and a strong west-east rainfall contrast.
A central and eastern European mountain arc framing the Pannonian Basin, Danube tributaries, high massifs, and forested ridges.
A Franco-Iberian range linking Atlantic and Mediterranean margins, glacial basins, drainage divides, and sharp climate contrasts.
A Nordic highland belt linking Caledonian structure, glacial plateaus, fjords, divided drainage, and strong west-east climate contrasts.
An eastern North American upland system shaped by ancient folds, long ridges, dissected plateaus, and divided drainage.
A severe high-mountain region where extreme relief, immense glaciers, and very high peaks dominate the landscape.
A high mountain system linking deep valleys, active relief, divided drainage, snow and ice, and the western Asian highlands.
A high inner Asian mountain knot linking sharp western relief, broad eastern basins, glaciers, and divided headwaters.
An Antarctic mountain belt linking rift-flank uplift, outlet glaciers, dry valleys, and the divide between East and West Antarctica.
A Central Asian mountain system linking high peaks, glaciers, interior basins, desert margins, and source-region runoff.
A northern Tibetan Plateau mountain system linking high massifs, glaciers, interior-basin headwaters, dry piedmonts, and active relief.
A central Honshu mountain system linking three high ranges, active uplift, deep valleys, river divides, and contrasting maritime snowfall.
An inner Asian highland system linking glaciated massifs, Ob and Irtysh headwaters, enclosed basins, and strong continental climate gradients.
A North American mountain system linking continental divides, intermontane basins, plateaus, and major river headwaters.
A California range defined by tilted-block relief, granite high country, snowpack-fed rivers, and a Great Basin rain shadow.
A Pacific-margin mountain belt shaped by subduction volcanism, glaciated relief, snow-fed rivers, and a pronounced eastern rain shadow.
A Pacific coastal system of granitic massifs, icefields, fjords, cross-range rivers, heavy maritime precipitation, and an interior rain shadow.
A North African range where uplift, Mediterranean influence, and desert-margin transitions meet along a complex mountain belt.
A Western Asian fold belt linking parallel ridges, Iranian Plateau margins, Mesopotamian drainage, and dryland climate transitions.
An eastern Australian upland system organizing escarpments, river catchments, and long stretches of elevated terrain.
A high-relief mountain barrier between the Black and Caspian seas with glaciers, sharp elevation gradients, and major divides.
An ancient Eurasian range linking low-to-moderate relief, river divides, continental climates, and the boundary between major plains.
A southern African escarpment and mountain region notable for basalt uplands, cliffed fronts, and plateau-edge relief.
An equatorial East African fault-block range linking ancient crystalline massifs, deep valleys, glacial terrain, heavy rainfall, and Nile-basin headwaters.
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