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Oceanic plate age (poster)

Visually accessible global map for poster print of oceanic plate age designed for color-blind readers.

Visually accessible global maps of oceanic plate age designed for color-blind readers. Highlighted are subduction zones (wide black lines) and other plate boundaries (thin black lines). Ages of the oceanic crust range from 0 (depicted in light colours) to approximately 200 Million years (depicted in dark colours), illustrating the dynamic process of ongoing plate motion and recycling through ocean-plate tectonics. This comprehensive representation is based on global seafloor age data from Müller et al. (1997), visualised on a custom Interrupted Mollweide map projection developed by Crameri et al. (2020a), with a specific focus on the world’s oceans. The ‘batlow‘ Scientific color map ensures accurate data representation and inclusivity for all readers.

  • Creator: Fabio Crameri
  • This version: 19.11.2023
  • License: Attribution-ShareAlike 4.0 International (CC BY-SA 4.0)
  • Specific citation: This graphic by Fabio Crameri using data from Müller et al. (1997) is available via the open-access s-ink.org repository.
  • Related references:
    Müller, R. D., et al. (1997). “Digital isochrons of the world’s ocean floor.” J. Geophys. Res. 102(B2): 3211-3214.
    Crameri, F., V. Magni, M. Domeier, G.E. Shephard, K. Chotalia, G. Cooper, C. Eakin, A.G. Grima, D. Gürer, A. Király, E. Mulyukova, K. Peters, B. Robert, and M. Thielmann (2020a), A transdisciplinary and community-driven database to unravel subduction zone initiation, Nature Communications, 11, 3750. doi:10.1038/s41467-020-17522-9
  • Printable version in CMYK and vector format
  • Suitable for light & dark backgrounds
  • Perceptually uniform colour map
  • Colour-vision deficiency friendly
  • Readable in black&white

Faulty or missing link? – Please report them via a reply below!

Oceanic plate age

Colour-blind friendly global oceanic plate age maps with plate boundaries.

Colour-blind friendly global oceanic plate age maps with subdution zones (wide black lines), other plate boundaries (thin black lines), and volcanoes (grey triangles). The ages vary between 0 and around 200 Ma due to ongoing plate motion and recycling (i.e., ocean-plate tectonics). The global oceanic plate age data from Müller et al. (1997) visualised on a custom Interrupted Mollweide map projection from Crameri et al. (2020a) focussing on the World’s oceans. The Scientific colour map ‘batlow‘ is used to represent data accurately and to all readers (Crameri et al., 2020b).

  • Creator: Fabio Crameri
  • This version: 03.09.2023
  • License: Attribution-ShareAlike 4.0 International (CC BY-SA 4.0)
  • Specific citation: This graphic by Fabio Crameri using data from Müller et al. (1997) is available via the open-access s-ink.org repository.
  • Related references:
    Müller, R. D., et al. (1997). “Digital isochrons of the world’s ocean floor.” J. Geophys. Res. 102(B2): 3211-3214.
    Crameri, F., V. Magni, M. Domeier, G.E. Shephard, K. Chotalia, G. Cooper, C. Eakin, A.G. Grima, D. Gürer, A. Király, E. Mulyukova, K. Peters, B. Robert, and M. Thielmann (2020a), A transdisciplinary and community-driven database to unravel subduction zone initiation, Nature Communications, 11, 3750. doi:10.1038/s41467-020-17522-9
    Crameri, F., G.E. Shephard, and P.J. Heron (2020b), The misuse of colour in science communication, Nature Communications, 11, 5444. doi:10.1038/s41467-020-19160-7
  • Additional map projection versions
  • Alternative colour map versions
  • Light & dark background versions
  • Perceptually uniform colour map
  • Colour-vision deficiency friendly
  • Readable in black&white

Faulty or missing link? – Please report them via a reply below!

Global-scale mantle flow (sketch)

A sketch outlining the link between the viscous convection within the Earth’s mantle and tectonic surface plate motions.

A sketch outlining the link between the viscous convection within the Earth’s mantle and tectonic surface plate motions, deforming Earth’s surface across wide areas. Shown are the relative positions and motion of some of Earth’s continental (brown) and oceanic plates (blue) captured by the hypothetical cross-section through the middle of the planet. The dynamic link between surface and mantle motion is highlighted by arrows representing first-order material flow direction. This global-scale mantle flow is believed to also affect the shape, position and mobility of large low shear-velocity provinces (LLSVPs; red) at the base of the mantle (yellow) just above the Earth’s core (orange).

  • Vector format
  • Transparent background
  • Suitable for light & dark background
  • Colour-vision deficiency friendly
  • Readable in black&white

Faulty or missing link? – Please report them via a reply below!

Ocean-plate age

Global seafloor age visualised on a custom Interrupted Mollweide map projection.

Maps of the age of oceanic plates, which varies between 0 and around 200 Ma due to ongoing plate motion and recycling (i.e., ocean-plate tectonics). Global sea-floor age data from Müller et al. (1997) visualised on a custom Interrupted Mollweide map projection from Crameri et al. (2020) focussing on the World’s oceans. The Scientific colour map ‘batlow‘ is used to represent data accurately and to all readers.

  • Creator: Fabio Crameri
  • This version: 20.08.2021
  • License: Attribution-ShareAlike 4.0 International (CC BY-SA 4.0)
  • Specific citation: This graphic by Fabio Crameri from Crameri et al. (2022) is available via the open-access s-Ink.org repository.
  • Related references:
    Crameri, F., G.E. Shephard, and E.O. Straume (2022, Pre-print), Effective high-quality science graphics from s-Ink.org, EarthArXiv, https://doi.org/10.31223/X51P78
    Müller, R. D., et al. (1997). “Digital isochrons of the world’s ocean floor.” J. Geophys. Res. 102(B2): 3211-3214.
    Crameri, F., V. Magni, M. Domeier, G.E. Shephard, K. Chotalia, G. Cooper, C. Eakin, A.G. Grima, D. Gürer, A. Király, E. Mulyukova, K. Peters, B. Robert, and M. Thielmann (2020), A transdisciplinary and community-driven database to unravel subduction zone initiation, Nature Communications, 11, 3750. doi:10.1038/s41467-020-17522-9
  • Additional map projection versions
  • Light & dark background versions
  • Perceptually uniform colour map
  • Colour-vision deficiency friendly
  • Readable in black&white

Faulty or missing link? – Please report them via a reply below!

Ocean-plate tectonics

A schematic highlighting Ocean-plate tectonics: ocean-plate formation, cooling and destruction as part of the planet’s global mantle convection.

A schematic highlighting the ocean-plate formation, cooling and destruction as part of the planet’s global mantle convection driven by the temperature gradient between its hot deep interior and the cold surface environment. Ocean-Plate Tectonics is the concept that describes not only the horizontal surface motion of the oceanic plate (grey arrow), but also highlights the pull from its subducted portion as the main driver (green arrow), distinguishes the oceanic plate (dark brown) from its continental counterpart, acknowledges the plate–mantle coupling that induces characteristic regional mantle-flow patterns (black flow lines), and describes the dynamics of the oceanic plate as part of the larger framework of global mantle convection that transports heat out of the interior (light-red arrow) due to the heat gradient between the planetary interior and outer space.

  • Variable content
  • Transparent background
  • Light & dark background versions
  • Vector format versions
  • Colour-vision deficiency friendly
  • Readable in black&white

Faulty or missing link? – Please report them via a reply below!

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