Open with QR Code
Scan this code to open the model on your device, then, tap on the AR icon
Or, open this link with your mobile:
Loading 3D model
3D viewer is not available.
Learn more here
You are seeing a 360° image instead.
Connection error. Please try again.
Sorry, the model can't be displayed.
Please check out our FAQ to learn how to fix this issue.
It looks like your browser or this site is blocking some scripts or cookies necessary to properly display the viewer.
Or visit the Help Center for more information:
Sample of 20 x 13 x 9cm olivine-rich basalt from the southeastern parking lot of the Fairmont Orchid Resort. This lava flow dates to 3000-5000yrs old, accroding to a USGS geologic map. The olivine crystals were the first minerals to crystalize in cooling magama chamber. The olivine sank to the bottom of the magma chamber over a period of many years enriching the magma at the bottom of the chamber. The olivine crytal-rich baslatic magma then erupted 3-5Ka years ago bringing the crystals to the surface in a gas-rich eruption. The baslat cooled relatively quickly to create the fine-grained vesicular basalt.