Geology in the landscape and buildings of LONDON

 


VOLCANIC ASH & TUFF

 

Volcanic ash is a pyroclastic rock, composed of fine grains less than 2mm in diameter. Pyroclastic means ‘fire-broken’, a name for rocks that have been blown apart by exploding gases. Ash exploded out of a volcano, may fall through the air and settle in beds, called ash-falls when unconsolidated, or tuffs when consolidated. The ash can vary in composition, for example it may be made up entirely of rock fragments.



Colour: white or grey powder when newly fallen.

Composition: ash-fall tuffs composed of a mixture of rock fragments, crystals and glass shards.

Classification: pyroclastic igneous rock.

Occurrence: associated with explosive volcanic activity, particle size decreases away from the vent because lighter ash is carried further by the wind.

Texture: fine-grained, less than 2mm.

Structure: ash-fall tuffs are often well-bedded.

 

 

Obsidian     Return to the igneous rocks menu