Reference Edition
Field Reference for Natural PlacesGeography Atlas
Volcano Record

Santorini Caldera

Santorini Caldera is a flooded Aegean volcanic collapse structure, with island-ring cliffs, pumice deposits, central volcanic islands, and arc-related terrain.

Why This Record Matters

A flooded caldera and island-ring landform

Santorini adds a caldera record where eruption, collapse, marine flooding, and island remnants create one visible volcanic basin.

TypeFlooded caldera

A volcanic collapse basin filled by the sea.

SettingAegean arc

The caldera belongs to a volcanic island arc.

LandformIsland ring

Cliffs and islands outline the collapsed structure.

MaterialsPumice and ash

Explosive deposits record caldera-forming eruptions.

Overview

What Santorini Caldera is

Santorini Caldera is a volcanic basin in the Aegean Sea. Its rim islands and steep cliffs mark the outline of a collapsed volcanic center.

The record is useful because it connects explosive volcanism, caldera collapse, marine flooding, and island landform structure.

Caldera Form

Collapse basin, cliffs, and island remnants

The caldera rim exposes volcanic layers and collapse geometry. Central islands and deposits show that volcanic activity continued after the main collapse.

Rim

Caldera cliffs

Steep walls reveal layered volcanic deposits.

Basin

Marine flooding

Sea water fills the collapse structure.

Arc

Aegean setting

The caldera belongs to a regional volcanic arc.