Spherulitic Rhyolite is formed from magma rich in silica that cooled after volcanic eruptions over 100 million years ago. It is named Rhyolite due to the wavy patterns on the rock, resembling ocean waves. Many geologists refer to the numerous ‘stone spheres’ within it as ‘spherulitic structures’. These structures are formed by gas-laden magma that, after erupting onto the surface and flowing, leads to localized gas accumulation, creating cavities in the form of spherical bubbles. The site is open all year round, accessible 24/7, with specific operating conditions subject to daily opening status.
Spherulitic Rhyolite
Spherulitic Rhyolite is formed from magma rich in silica that cooled after volcanic eruptions over 1[...]
