× Homepage Vesuvius 79 AD Laki Fissure 1783
Instructions The Plinys Observations (1) Interpretations (2) Processes Fallout (3) Flows (4-5) Field Work Deposits (6) Exploration (7-9) Hypotheses (10)
Homepage Vesuvius 79 AD Laki Fissure 1783

Haraldur Sigurdsson studies an outcrop at Herculaneum

Fieldwork

During fieldwork, a volcanologist searches for clues about volcanic processes by examining the deposits left by an explosive eruption in the field.

The deposits contain valuable information about how an enruption took place, what kinds of phenomena it produced, and the impact that the eruption had on the local environment.

This information is extracted by making careful observations about the details of the deposits, including the grain sizes of particles, sorting (range of particle sizes in a specific layer) and the thicknesses of different layers.

Volcanic Deposits

Deposits from explosive eruptions are commonly arranged in layers. Each layer represents a specific type of volcanic process.

It is important to remember that a single eruption may produce a number of different layers if the volcanic processes change during the course of the eruption. The lowermost layer typically represents the earliest phase of the eruption with subsequent layers stacked one on top of another.

The sequence of events is thus read from the bottom to the top.

Superposition

Steve and Haraldur explain how the layering of deposits relate to the timeline of a volcanic eruption. In geology, we call this principle of layering through time "superposition."