tectonic context
Plates, models, and what a boundary line is
Every plate boundary you have ever seen drawn belongs to a model. Model PB2002 divides Earth into fifty-two plates and marks thirteen more regions where it says a rigid plate does not describe the motion at all.
About: Pacific Plate · Persia–Tibet–Burma diffuse deformation zone
Fifty-two plates, and thirteen admissions
Model PB2002 comprises plate boundary curves in 229 segments, 52 plates as closed outlines, and 13 orogens — regions where deformation is distributed rather than confined to a boundary, so that the rigid-plate description fails.[1,2]
Those thirteen regions are the most interesting thing in the model, because they are where it declares its own limits. Their outlines delimit where a model stops working. They are not orogenic belts, and Bird gives them spelled-out names specifically, in his words, "to help prevent confusion between orogens and plates".[1]
A boundary is classified, and only sometimes
The model recognises seven classes of boundary step. Subduction requires convergent motion together with a Benioff zone of intermediate to deep earthquakes and/or a parallel volcanic arc with Quaternary activity — criteria which, the documentation notes, exclude the Alps, Zagros, Pamirs, Himalaya, Tien Shan and Taiwan. Convergence across the Himalaya is not in question. What the criteria exclude is the label.[1]
The other six classes combine oceanic or continental setting with divergent, strike-slip or convergent relative velocity. Oceanic means sea floor younger than 180 million years by magnetic anomaly, or water deeper than 2,000 metres; everything else, including transitional crust, counts as continental.[1]
Why Lithoen names the model on every line
A boundary’s position, its class and sometimes its existence depend on which model is being read. A plate that appears in one model may be part of a larger plate in another. Lithoen therefore names PB2002 on every plate geometry it publishes and draws no unattributed boundary anywhere.[1]
The Somali Plate is the clearest case. PB2002 separates it from Africa along the East African Rift, which is why the rift appears as a plate boundary on Lithoen’s map. Whether the rift has yet made two plates is a question about how much relative motion a model needs before it draws a line — not a fact about the rock.[1,2]
Commonly misunderstood
Often said
“There are about seven or eight tectonic plates.”
What the evidence supports
Model PB2002 has fifty-two, most of them dominantly oceanic, and thirteen further regions where no rigid plate describes the motion.
Supporting records: pb2002-composition · plate-is-not-continent
Often said
“A plate boundary is a fixed line that could in principle be surveyed.”
What the evidence supports
It is a line in a model, compiled from published sources at varying scales, whose class changes along its own length.
Supporting records: plate-boundary-is-model-dependent · pb2002-class-not-constant
Bracketed references link to the structured entity records whose claims support each paragraph. Last updated 2026-09-07.