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EIGEN-6C4 Geoid Globe

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P1S
H2C
A1
X1E
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P2S
A1 mini
P1P
H2S
H2D
X1
X1 Carbon
X2D
A2L

PLA - 0.2mm layer, 4 walls, 5% infill
PLA - 0.2mm layer, 4 walls, 5% infill
Designer
2.6 h
1 plate

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Description

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This model represents the Geoid, which is the theoretical surface that oceans would assume under the influence of the Earth's gravitational field and the planet's rotation.

Scientific Details

The Geoid provides crucial information about Earth's density: where density is higher, gravity is stronger and "attracts" water, creating a bulge (geoid high). In reality, these variations oscillate between ±100 meters; to make these differences visible to touch and sight, this model uses a vertical exaggeration of approximately 12,000 times.

A step of approximately 1 mm has been added along the coastline to facilitate visual interpretation of the continents. Similarities with real topography (such as mountain ranges) arise exclusively from the fact that mountains are much denser than the surrounding air, thus influencing the gravitational field.

Print Notes and Credits

  • Scalability: The model can be freely scaled in your slicer to suit any need.
  • Data: Based on the EIGEN-6C4 model (ICGEM at GFZ Potsdam).
  • Original Author: This file is a print-optimized adaptation for Bambu Studio derived from the project by Jeff Winterbourne (GitHub).

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License

This user content is licensed under a Standard Digital File License.

You shall not share, sub-license, sell, rent, host, transfer, or distribute in any way the digital or 3D printed versions of this object, nor any other derivative work of this object in its digital or physical format (including - but not limited to - remixes of this object, and hosting on other digital platforms). The objects may not be used without permission in any way whatsoever in which you charge money, or collect fees.