Pyroclastic Flow Deposits close to Volcan de Fuego, Guatemala.
The scale of these deposits, formed in 2012, can be seen against the scale of the person standing in the background [dark line, just above the red shrub]. Pyroclastic flows, alongside lahars, are two of the most significant and destructive volcanic hazards associated with Volcan de Fuego.
You can read more about Fuego and its secondary hazards online here.
(Credit: Geology for Global Development, 2014)
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Christopher Barry
How many eruptions formed that section? And why is it so colourful?
Matt watson
The colours are from oxidation of the rock (mostly iron bearing) and the flat bit in the foreground is the deposit. The valley walls are a sequence of flows and ash fall and probably represent a few thousand years of activity. Note the new flow almost fills the valley….