EarthMapped How many plates
World map of the 52 PB2002 tectonic plates by size groupAFRICANANTARCTICSOMALIINDIANAUSTRALIANEURASIANNORTH AMERICANSOUTH AMERICANNAZCAPACIFICARABIANSUNDACARIBBEANCOCOSOKHOTSKJUAN DE FUCAPHILIPPINE SEAAMURSCOTIAYANGTZE

How Many Tectonic Plates Are There?

There are 52 tectonic plates in the PB2002 model: 7 major, 13 minor and 32 microplates by area.

  • Microplate. A small fragment of a plate, common in wide plate boundary zones such as the Mediterranean-Alpine region. Source

Data source: PB2002 plate model, Bird (2003), converted by Hugo Ahlenius, Nordpil, ODC-By 1.0. Download: CSV .

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Major, minor and microplates

No standard rule splits plates into major and minor. We group the 52 PB2002 plates by area: over 20.0 million km² is major, 1.0 million km² to 20.0 million km² is minor, and smaller ones are microplates Microplate. A small fragment of a plate, common in wide plate boundary zones such as the Mediterranean-Alpine region. Source . These thresholds sit at the largest gaps between plate areas.

Key facts

  1. PB2002 divides Earth's surface into 52 plates: the 14 large plates of the older NUVEL-1A model plus 38 small ones. Bird (2003)
  2. The 7 major plates (over 20 million km² each) cover 81% of Earth's surface.
  3. The 32 microplates (under 1 million km² each) cover only 2% of the surface between them.
  4. The smallest plate in PB2002 is Manus, at 8,229 km².
  5. USGS describes the outer layer as broken into "a dozen or more large and small plates". USGS, Historical perspective
  6. Plates range from a few hundred to thousands of kilometers across. The Pacific and Antarctic plates are among the largest. USGS, What is a tectonic plate?

Why sources disagree

The number you read depends on which model a source follows and where it stops counting.

  • 7: the plates over 20.0 million km² in our area split. There is no official list of major plates, so a list of 7 depends on where its author draws the line.
  • A dozen or more: the wording USGS uses for the large and small plates of the outer layer.
  • 14: the large plates of the NUVEL-1A motion model, which Bird (2003) kept as the base of PB2002.
  • 52: PB2002, which adds 38 small plates, many of them inside broad plate boundary zones. Bird did not split mountain belts such as the Alps into plates, so even 52 is a simplification.

All 52 plates

Every PB2002 plate, largest first. Sort by any column.

The 52 PB2002 tectonic plates
RankPlateGroupArea (million km²)Share of EarthIn NUVEL-1A 14
1 Pacific Major 104.59 20.5% Yes
2 African Major 58.48 11.5% Yes
3 Antarctic Major 58.15 11.4% Yes
4 North American Major 55.43 10.9% Yes
5 Eurasian Major 48.56 9.5% Yes
6 Australian Major 45.99 9% Yes
7 South American Major 41.83 8.2% Yes
8 Somali Minor 19.15 3.8% No
9 Nazca Minor 16.10 3.2% Yes
10 Indian Minor 12.44 2.4% Yes
11 Sunda Minor 8.92 1.7% No
12 Philippine Sea Minor 5.44 1.1% Yes
13 Amur Minor 5.30 1% No
14 Arabian Minor 4.90 1% Yes
15 Okhotsk Minor 3.04 0.6% No
16 Caribbean Minor 2.96 0.6% Yes
17 Cocos Minor 2.93 0.6% Yes
18 Yangtze Minor 2.20 0.4% No
19 Scotia Minor 1.70 0.3% No
20 Caroline Minor 1.53 0.3% No
21 North Andes Micro 0.97 0.2% No
22 Altiplano Micro 0.83 0.2% No
23 Banda Sea Micro 0.70 0.1% No
24 New Hebrides Micro 0.64 0.1% No
25 Anatolia Micro 0.58 0.1% No
26 Birds Head Micro 0.53 0.1% No
27 Burma Micro 0.51 0.1% No
28 Kermadec Micro 0.51 0.1% No
29 Woodlark Micro 0.45 0.1% No
30 Mariana Micro 0.42 0.1% No
31 Molucca Sea Micro 0.42 0.1% No
32 North Bismarck Micro 0.39 0.1% No
33 Timor Micro 0.35 0.1% No
34 Okinawa Micro 0.32 0.1% No
35 Aegean Sea Micro 0.32 0.1% No
36 South Bismarck Micro 0.31 0.1% No
37 Panama Micro 0.27 0.1% No
38 Juan de Fuca Micro 0.26 0.1% Yes
39 Tonga Micro 0.25 0% No
40 Balmoral Reef Micro 0.20 0% No
41 Sandwich Micro 0.18 0% No
42 Easter Micro 0.17 0% No
43 Conway Reef Micro 0.14 0% No
44 Solomon Sea Micro 0.13 0% No
45 Niuafo'ou Micro 0.12 0% No
46 Maoke Micro 0.12 0% No
47 Rivera Micro 0.10 0% No
48 Juan Fernandez Micro 0.10 0% No
49 Shetland Micro 0.07 0% No
50 Futuna Micro 0.03 0% No
51 Galapagos Micro 0.01 0% No
52 Manus Micro 0.01 0% No

Data source: PB2002 plate model, Bird (2003), converted by Hugo Ahlenius, Nordpil, ODC-By 1.0. Download: CSV .

See the largest tectonic plate, every plate on the tectonic plates list, or where they meet on the plate boundaries map.

Print this map Tectonic plates worksheet. Number the plates, with an answer key

Glossary

Microplate
A small fragment of a plate, common in wide plate boundary zones such as the Mediterranean-Alpine region. Source
Plate boundary zone
A broad belt where the edges of plates are not clearly defined and the boundary is spread across many small blocks. Source
Divergent boundary
Plates pull away from each other and new crust forms between them. Source
Convergent boundary
Plates move toward each other and crust is destroyed as one plate dives under another. Source

All terms in the glossary

Tectonic plate count FAQ

How many tectonic plates are there?
There are 52 tectonic plates in the PB2002 model: 7 major, 13 minor and 32 microplates by area. The count depends on the model: USGS says a dozen or more, and the NUVEL-1A model used 14.
What are the 7 major tectonic plates?
By area in PB2002, the plates over 20 million km² are Pacific Plate, African Plate, Antarctic Plate, North American Plate, Eurasian Plate, Australian Plate and South American Plate.
Why do sources give different numbers of plates?
Each model draws its own line between a plate and a fragment of a plate boundary zone. The NUVEL-1A motion model described 14 large plates. Peter Bird (2003) kept those and added 38 small plates, many of them inside boundary zones, for 52 in all.
What is the smallest tectonic plate?
In PB2002 it is the Manus Plate, at about 8,229 km².
Is the number of plates changing?
Yes, slowly. Plates split along rifts and join when the ocean between them closes. USGS points to the East African Rift as a place where Africa may split and a new ocean may form.

Sources: Bird (2003); USGS, Historical perspective; USGS, What is a tectonic plate?; USGS, Understanding plate motions.