Plates Kenny Lienhard
Plates

Plate 6 of 52

Australia

Kenny Lienhard, Plates, 2026

Palette
Oxide, from desert
Structure
Domino faults
Drift
6.9 cm a year, north-northeast
Era
Sahul
45,984,768 km², a major plate

How it is made

Finished

The Plate in detail

Australia, seed 6

Plate 6 of 52 · one of one

Traits

Palette
Oxide
Structure
Domino faults
Event
Unconformity
Faults
Two
Scale
Standard
Hang
Level
Accent
Single
Era
Sahul
Heading
North-northeast, 30.0°
Speed
6.87 cm a year

History

The past. Sahul: with the sea about 120 metres lower, Australia, New Guinea and Tasmania were one continent, and more than two million square kilometres of today’s shallow seas were dry land, from the plains of the Gulf of Carpentaria, where a lake grew larger than Tasmania, to the land bridge across Bass Strait. Sahul was already whole when the timeline begins; the rising sea drowned most of it between 14,676 and 8,076 years ago. The lines that stand for the sea turn halfway to the colour of land, all at once, and only across those spans.

4.4 billion years ago
Zircon crystals formed that are among the oldest known pieces of Earth; they survive in younger rocks on this plate.
136 million years ago
A new ocean ridge began to split India away from this plate's western edge.
83.5 million years ago
After a long rift, Australia broke away from Antarctica.
83 million years ago
The Tasman Sea began to open as the Lord Howe Rise drifted away from Australia.
51.5 million years ago
A major reorganization of plate motions changed how Australia and Antarctica moved apart.
16 million years ago
This part of the Indian Ocean floor began to press slowly against India, and a wide zone between them began to buckle.
8 million years ago
The squeeze doubled in speed, and the ocean floor between this plate and India folded into long waves.
6 million years ago
The northern edge of the Australian continent began to jam into the volcanic arc to its north, pushing up Timor.
6 million years ago
Far south of New Zealand, the Macquarie part of this plate began to move on its own as a small rigid plate.

Sources: Williams et al. 2018, Quaternary Science Reviews 182:144; Reeves et al. 2013, Quaternary Science Reviews 74:97 · Wilde et al. 2001, Nature 409:175 · Gibbons, Whittaker and Muller 2013, Journal of Geophysical Research 118:808 · Williams, Whittaker and Muller 2011, Tectonics 30:TC6012 · Gaina et al. 1998, Journal of Geophysical Research 103:12413 · Whittaker et al. 2007, Science 318:83 · Bull et al. 2010, Geology 38:307 · Royer and Gordon 1997, Science 277:1268 · Cochran 1990, Proceedings ODP Scientific Results 116 · Harris 2011, in Arc-Continent Collision (Springer) p.163 · Cande and Stock 2004, Geophysical Journal International 157:399

Technical notes

The file

90,012bytes, the whole work
74,112bytes of engine, gzip and base64
0network requests
2048 pxdrawn on up to 8 workers, at your screen’s size

One HTML file: the engine (151,144 bytes minified), this plate's data and a small loader. It reads your clock and slides the view to where the plate is today.

engine sha256 a7fbc03acc0fc9ba343881bb88ddaf2b7564564d8bc9cbed16e75e47e01fb3f2

Sources

  • The plate, its outline and its motionBird, P. (2003). An updated digital model of plate boundaries. Geochemistry, Geophysics, Geosystems 4(3), 1027.
  • What covers it, which chose the paletteESA CCI Land Cover and Water Bodies, ETOPO 2022, Köppen-Geiger climate maps, NSIDC Sea Ice Index.

The work

Live

One HTML file that drifts with your clock, a few centimetres a year.