Reading the bubbles in volcanic glass
Vesicles preserve traces of gas leaving magma, but growth, merger, flow and the cut of a specimen all change the pattern a reader sees.
A place for slower thoughts
Geology in stone, sediment and the ground beneath ordinary places.
Words by Ivo Calder
Vesicles preserve traces of gas leaving magma, but growth, merger, flow and the cut of a specimen all change the pattern a reader sees.
A limestone field can hide a connected drainage landscape. Dye traces, weathering experiments and sinkhole investigations show how water enters rock, travels through it and sometimes carries soil away.
Salt can leave a white bloom on stone or grow under its surface. The damaging difference lies in water, pore space and the pressure of a confined crystal.
An unconformity marks a break in the local rock record. At Siccar Point and Grand Canyon, angles, fossils, mineral ages and fragments of older stone reveal what a missing interval can still tell us.
A round pebble has met other surfaces, but its smoothness is no odometer. Rock type, broken edges, intermittent floods and recycled gravel complicate the journey it seems to show.