To use all functions of this page, please activate cookies in your browser.
With an accout for my.chemeurope.com you can always see everything at a glance – and you can configure your own website and individual newsletter.
- My watch list
- My saved searches
- My saved topics
- My newsletter
Volcanic blocks are fragments of rock which measure more than 64mm in size and are erupted in a solid condition.
Additional recommended knowledge
Blocks are formed from material from previous eruptions or from country rock and are therefore mostly accessory or accidental in origin. Blocks also occur due to the impact and breakage of volcanic bombs (a bomb is a block with streamlined appearance, often expelled in a molten state). Bombs can also occur due to the disruption of the crust of a lava dome that has formed up or over a vent during an eruption.
Blocks are nearly always angular to sub-angular and roughly equidimensional. If the parent rock is flow-foliated lava, sedimentary material or schistose metamorphic rocks, the blocks may have a plate-like or slab-like form. In other cases, blocks derived from great depths may resemble polished water-worn pebbles and are cobbled due to fluidisation and upwards transport.
Blocks can be enormous and may be transported great distances from the volcanic vent. The 1924 eruption of Kīlauea, Hawaii, expelled rocks weighing up to 14 tonnes; and Mount Vesuvius in Italy discharged blocks weighing 2-3 tonnes over distances of 100-200m.
|This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Volcanic_blocks". A list of authors is available in Wikipedia.|