🪨 Geodes & Nodules

A geode is a rock with a hollow, crystal-lined cavity. A nodule is the same kind of structure filled solid, often with agate. A thunderegg is a nodule that grew inside volcanic rhyolite.

1 · A cavity forms

Gas bubbles in cooling lava, dissolved pockets in limestone, or hollows left by roots, shells or concretions in sediment make an empty space.

2 · A rind hardens

Silica-rich fluids coat the cavity wall with a tough skin of chalcedony. This is why geodes weather out of softer rock as round "rocks".

3 · Crystals grow inward

Over thousands to millions of years, mineral-rich groundwater seeps in. Quartz, amethyst, calcite, celestite or other minerals crystallize from the wall toward the centre.

Geode, nodule or thunderegg?

If the space stays partly open, it is a geode. If it fills completely, often with banded agate, it is a nodule. A thunderegg forms in rhyolite and usually has a star-shaped agate core.

See also Stalactites: drip-grown columns from the same cavities, including amethyst 'flower' slices.

Agate Geode
Agate GeodeGeode / noduleOften Cretaceous to Tertiary volcanic rocks (about 130–25 million years)
Amethyst Geode
Amethyst GeodeGeode / noduleBrazilian and Uruguayan amethyst geodes formed in Paraná basalt flows about 130–135 million years ago (Early Cretaceous)
Calcite Geode
Calcite GeodeGeode / noduleCommonly Mississippian (about 340 million years) in the US Midwest
Celestite Geode
Celestite GeodeGeode / noduleMadagascar celestite geodes are Cretaceous, about 100 million years old
Geode
GeodeGeode / noduleVaries widely. Many collector geodes are Mississippian (about 340 million years) or Cretaceous to Tertiary volcanic (about 130–25 million years).
Keokuk Geode
Keokuk GeodeGeode / noduleMississippian, about 340 million years old (Warsaw Formation)
Las Choyas Geode
Las Choyas GeodeGeode / noduleTertiary volcanic, about 35–40 million years old
Moroccan Geode
Moroccan GeodeGeode / noduleVaries; many come from Devonian to Cretaceous sediments
Quartz Geode
Quartz GeodeGeode / noduleVaries; Midwestern US quartz geodes are Mississippian, about 340 million years
Thunderegg
ThundereggGeode / noduleCommonly Eocene to Miocene, about 50–15 million years ago. Oregon material is about 30–40 million years old.
Uruguayan Amethyst Geode
Uruguayan Amethyst GeodeGeode / noduleEarly Cretaceous, about 130–135 million years old (Paraná–Etendeka basalts)