Indian Plate

The Indian Plate is the 10th-largest of the 52 plates in the PB2002 plate model, covering 12.4 million km² (4.8 million sq mi), or 2.4% of Earth’s surface. India, Bangladesh, Sri Lanka, eastern Pakistan, parts of Nepal and Myanmar, and the central Indian Ocean floor.

Indian Plate on the globe, with its boundaries coloured by typeIndian PlateEurasian PlateSomali PlateAustralian PlateArabian Plate
Indian Plate Convergent Divergent Transform
Area
12.4 million km² (4.8 million sq mi)
Share of Earth’s surface
2.4%
Speed across the plate
4.8 to 6.0 cm a year (1.9 to 2.4 in)
Direction at its center
Toward the northeast
Length of its edges
17,110 km (10,630 mi)
Neighboring plates
5
Edges by type
52% convergent · 23% divergent · 25% transform
Volcanoes on it
1 active in the past ~12,000 years

What happens at its edges

Its collision with Eurasia, under way for roughly 50 million years, raised the Himalaya and the Tibetan Plateau and still causes earthquakes across the region. In this model the broad collision belt is mapped as a deforming zone.

Many maps join it to the Australian Plate as the Indo-Australian Plate. Its long eastern edge with the Burma Plate runs past the Andaman and Nicobar Islands to the sea off northern Sumatra.

How fast it moves, and which way

At its center (13.0°N, 77.5°E) the Indian Plate moves about 5.7 cm (2.2 in) a year toward the northeast. Because a plate turns around a pole rather than sliding in a straight line, the speed changes across it: from 4.8 cm (1.9 in) a year to 6.0 cm (2.4 in) a year, with an area-weighted average of 5.6 cm a year. That average makes it the 18th fastest of the 52 plates.

These figures are measured against the average motion of all the plates together (the “no-net-rotation” frame), which is how plate speeds are usually quoted. Measured against the Eurasian Plate instead, the Indian Plate moves about 4.7 cm (1.9 in) a year toward the north-northeast at its center.

In the model it rotates about a pole at 45.1°N, 0.5°E at 0.538° per million years. The speeds are averages over years to millions of years of measurement; earthquakes move the ground near a boundary in sudden steps instead.

Neighboring plates and boundaries

Its edges run for 17,110 km (10,630 mi): 52% convergent, where plates move together; 23% divergent, where they move apart; and 25% transform, where they slide past each other. It sinks beneath the Burma Plate at subduction zones.

NeighborShared edgeBoundary typesRelative speed
Eurasian Plate6,040 km (3,750 mi)Convergent 72% · Transform 26%4.7 cm a yearup to 5.4 cm
Somali Plate3,820 km (2,370 mi)Divergent 65% · Transform 32%3.0 cm a yearup to 3.6 cm
Australian Plate3,600 km (2,240 mi)Convergent 64% · Divergent 29% · Transform 6%0.5 cm a yearup to 1.1 cm
Burma Plate2,010 km (1,250 mi)Convergent 75% · Transform 25%2.5 cm a yearup to 5.1 cm
Arabian Plate1,660 km (1,030 mi)Transform 49% · Convergent 34% · Divergent 17%0.7 cm a yearup to 0.7 cm

Relative speed is how fast the two plates move against each other along their shared edge, averaged over its length.

Countries and territories on the Indian Plate

3 lie entirely on it; the other 5 are split between plates. The share is the part of each country’s land on this plate.

Volcanoes on the Indian Plate

The Smithsonian Global Volcanism Program lists 1 volcano on this plate that has been active in roughly the past 12,000 years. The most recent eruptions on record:

Where the edges are blurred

Parts of this plate lie in the Ninety East-Sumatra and Persia-Tibet-Burma zones, which the model marks as broad belts of deformation rather than sharp plate edges. There the motion between plates is spread over many faults, and a single boundary line is a simplification.

Sources

Outline, area, boundary types and motion: Bird, P. (2003), An updated digital model of plate boundaries, Geochemistry Geophysics Geosystems, 4(3), 1027, doi:10.1029/2001GC000252. Released by its author into the public domain (CC0 1.0). Areas are the model’s published figures; speeds, directions, boundary lengths and countries are calculated from its outlines, boundary steps and rotation poles.

Volcanoes: Global Volcanism Program, Smithsonian Institution, Volcanoes of the World (v. 5.4.0). Country outlines: Natural Earth.