Contact metamorphic zone at the foot of Mt. Watamuki

The contact metamorphic zone at the foot of Mount Watamuki displays rocks that have been transformed by intense heat from ancient magmatic intrusions beneath the mountain. The site reveals multiple layers where original rock and altered material sit side by side, showing the effects of underground heat over time.

The metamorphic zone developed over millions of years as tectonic activity pushed magma into surrounding rock layers, transforming their structure. These geological changes occurred during a period of significant earth movement in the region.

The metamorphic zone functions as an educational site where students and researchers examine geological processes and rock transformations in natural settings.

Wear sturdy hiking boots and dress for changing mountain weather to navigate the uneven ground safely. The terrain can be wet or slippery after rain, so timing your visit on stable weather days makes the exploration easier.

The site displays sharp boundaries between metamorphosed and unaltered rocks, with noticeable color and texture differences that reveal the geological transformation. These clear transitions allow visitors to see firsthand how magmatic heat reshaped the stone without needing technical equipment.