Mid-Ocean Ridge Map
The mid-ocean ridge is an underwater mountain range that forms where tectonic plates spread apart. PB2002 maps 67,367 km of spreading ridge; NOAA puts the whole system at nearly 65,000 km.
- Mid-ocean ridge. An underwater mountain range that forms along divergent plate boundaries, where new ocean floor is made. Source
- Rift. A valley where the crust is being pulled apart, such as the East African Rift, which may in time become a new ocean. Source
Data source: PB2002 plate model, Bird (2003), converted by Hugo Ahlenius, Nordpil, ODC-By 1.0. Download: GeoJSON .
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What the map shows
A mid-ocean ridge Mid-ocean ridge. An underwater mountain range that forms along divergent plate boundaries, where new ocean floor is made. Source forms along a divergent boundary on the sea floor. NOAA describes the system as nearly 65,000 km long. The solid red lines are every step PB2002 classes as an oceanic spreading ridge. The dashed lines are continental rifts Rift. A valley where the crust is being pulled apart, such as the East African Rift, which may in time become a new ocean. Source , where the same pulling apart happens on land.
Key facts
- The mid-ocean ridge system is nearly 65,000 km long, and the top of the ridge lies on average about 2,500 m below the sea surface. NOAA Ocean Exploration, What is the mid-ocean ridge?
- PB2002 maps 67,367 km of oceanic spreading ridge, 4% more than NOAA's figure. Each source draws and measures the ridge its own way. Bird (2003)
- 61 pairs of plates are separated by a spreading ridge. The longest is African and South American, at 8,169 km.
- The fastest spreading pair is Nazca and Pacific, at a mean 14.1 cm/yr. Among pairs with over 500 km of ridge, North American and South American is slowest, at 0.2 cm/yr.
- The Mid-Atlantic Ridge spreads 2 to 5 cm a year and has a deep rift valley along its crest. The East Pacific Rise spreads 6 to 16 cm a year and has no rift valley. NOAA Ocean Exploration, What is the mid-ocean ridge?
- Iceland straddles the Mid-Atlantic Ridge, so the spreading can be studied on land there. USGS, Understanding plate motions
Spreading ridges by plate pair
Every pair of plates with a spreading ridge between them in PB2002, longest first. Sort by any column.
| Plates | Length (km) | Mean spreading (cm/yr) | Top spreading (cm/yr) |
|---|---|---|---|
| African and South American | 8,169 | 3.2 | 3.4 |
| Australian and Antarctic | 7,457 | 6.8 | 7.2 |
| North American and Eurasian | 7,324 | 1.7 | 2.3 |
| Pacific and Antarctic | 5,322 | 7.6 | 9.5 |
| Nazca and Pacific | 3,296 | 14.1 | 15.1 |
| Somali and Antarctic | 3,271 | 1.1 | 1.4 |
| North American and African | 2,956 | 2.3 | 2.5 |
| Somali and Indian | 2,487 | 3.0 | 3.6 |
| Cocos and Nazca | 2,062 | 5.3 | 6.6 |
| Australian and Somali | 1,763 | 4.1 | 4.9 |
| Cocos and Pacific | 1,743 | 10.0 | 12.6 |
| African and Antarctic | 1,475 | 1.4 | 1.4 |
| Philippine Sea and Mariana | 1,294 | 3.5 | 5.6 |
| Antarctic and Nazca | 1,291 | 5.7 | 5.8 |
| Somali and Arabian | 1,101 | 2.4 | 2.8 |
| Pacific and Juan de Fuca | 1,073 | 5.6 | 5.6 |
| Indian and Australian | 1,059 | 0.3 | 0.5 |
| Kermadec and Australian | 1,006 | 3.3 | 5.1 |
| North American and South American | 992 | 0.2 | 0.3 |
| Caroline and Philippine Sea | 754 | 0.4 | 0.8 |
| Eurasian and African | 633 | 0.4 | 0.5 |
| Sandwich and Scotia | 620 | 7.2 | 8.1 |
| Easter and Pacific | 613 | 8.4 | 13.7 |
| Australian and Conway Reef | 599 | 3.3 | 5.5 |
| Conway Reef and New Hebrides | 599 | 8.3 | 11.8 |
| Antarctic and South American | 569 | 1.7 | 1.8 |
| Australian and Woodlark | 549 | 3.1 | 4.0 |
| Juan Fernandez and Pacific | 499 | 13.3 | 20.2 |
| New Hebrides and Pacific | 497 | 1.4 | 2.3 |
| Easter and Nazca | 481 | 6.9 | 11.5 |
| Tonga and Australian | 467 | 6.1 | 9.3 |
| Scotia and Antarctic | 437 | 1.1 | 1.2 |
| Balmoral Reef and New Hebrides | 423 | 3.0 | 3.9 |
| Sunda and Burma | 403 | 3.7 | 4.5 |
| Pacific and Balmoral Reef | 374 | 2.2 | 2.2 |
| North American and Pacific | 348 | 4.7 | 4.9 |
| Rivera and Pacific | 316 | 6.5 | 8.0 |
| Indian and Arabian | 282 | 0.7 | 0.7 |
| Niuafo'ou and Australian | 259 | 8.4 | 9.2 |
| Juan Fernandez and Nazca | 244 | 4.5 | 8.2 |
| Tonga and Niuafo'ou | 190 | 10.4 | 12.6 |
| Pacific and Niuafo'ou | 175 | 13.8 | 13.9 |
| Futuna and Pacific | 175 | 4.4 | 4.9 |
| Galapagos and Pacific | 167 | 11.6 | 12.3 |
| Galapagos and Nazca | 167 | 3.2 | 3.9 |
| Aegean Sea and Anatolia | 134 | 1.9 | 1.9 |
| Manus and South Bismarck | 133 | 10.2 | 15.6 |
| Scotia and South American | 120 | 0.5 | 0.5 |
| Juan Fernandez and Antarctic | 119 | 5.9 | 7.4 |
| Caribbean and North American | 119 | 1.7 | 1.7 |
| Galapagos and Cocos | 106 | 0.9 | 1.1 |
| North Bismarck and Manus | 100 | 4.7 | 8.4 |
| New Hebrides and Australian | 85 | 12.8 | 12.9 |
| Amur and Okinawa | 77 | 0.4 | 0.5 |
| Pacific and Caroline | 71 | 1.1 | 1.1 |
| Niuafo'ou and Futuna | 60 | 10.9 | 11.1 |
| Balmoral Reef and Australian | 58 | 6.9 | 6.9 |
| Nazca and Panama | 58 | 4.0 | 4.0 |
| Yangtze and Okinawa | 56 | 4.5 | 4.5 |
| Woodlark and Birds Head | 54 | 6.1 | 6.1 |
| Pacific and Australian | 7 | 2.9 | 2.9 |
Data source: PB2002 plate model, Bird (2003), converted by Hugo Ahlenius, Nordpil, ODC-By 1.0. Download: GeoJSON .
Longest unbroken ridge segments
| Plates | Length (km) | Mean spreading (cm/yr) | Near |
|---|---|---|---|
| North American and Eurasian | 1,251 | 1.0 | 84°N, 109°E |
| North American and Eurasian | 1,014 | 1.5 | 74°N, 9°E |
| North American and South American | 992 | 0.2 | 16°N, 51°W |
| Caroline and Philippine Sea | 754 | 0.4 | 4°N, 133°E |
| Indian and Australian | 725 | 0.3 | 7°S, 72°E |
| Australian and Antarctic | 623 | 6.9 | 43°S, 92°E |
| African and South American | 592 | 3.3 | 43°S, 16°W |
| Australian and Antarctic | 589 | 7.0 | 50°S, 136°E |
| Cocos and Nazca | 587 | 6.0 | 1°N, 88°W |
| Cocos and Pacific | 522 | 11.5 | 6°N, 103°W |
Data source: PB2002 plate model, Bird (2003), converted by Hugo Ahlenius, Nordpil, ODC-By 1.0.
Transform faults cut the ridge into short pieces, so the longest unbroken segments are much shorter than the ridge between a pair of plates. See them on the transform boundary map, compare the subduction zones map, or read why tectonic plates move.
Print this map Plate boundaries worksheet. Label the boundary types, with an answer keyGlossary
- Mid-ocean ridge
- An underwater mountain range that forms along divergent plate boundaries, where new ocean floor is made. Source
- Rift
- A valley where the crust is being pulled apart, such as the East African Rift, which may in time become a new ocean. Source
- Divergent boundary
- Plates pull away from each other and new crust forms between them. Source
- Transform boundary
- Plates slide horizontally past each other. Crust is neither made nor destroyed. Source
- Relative plate velocity
- How fast one plate moves compared with its neighbor across a boundary, in millimeters per year. Source
Mid-ocean ridge FAQ
What is a mid-ocean ridge?
How long is the mid-ocean ridge?
Which mid-ocean ridge spreads fastest?
Is the Mid-Atlantic Ridge the same as the mid-ocean ridge?
What are the dashed lines on the map?
Sources: NOAA Ocean Exploration, What is the mid-ocean ridge?; USGS, Understanding plate motions; Bird (2003) for lengths and speeds.