Santorinikanava

Santorinikanava is a term that refers to the underwater channel or strait separating the island of Santorini from the nearby smaller islands of Thirasia and Aspronisi. This channel is part of the caldera, the geological formation created by the massive volcanic eruption that shaped Santorini millennia ago. The waters within the Santorinikanava are deep and can be subject to currents, making them a significant factor for maritime navigation in the region.

The geographical configuration of the Santorinikanava is a direct consequence of the volcanic activity that formed the caldera. The submerged parts of the ancient volcano and subsequent lava flows created the seafloor topography that defines this channel. The presence of the channel plays a role in the local marine ecosystem, influencing water circulation and the distribution of marine life.

Historically, the Santorinikanava has been a vital passage for boats and ships traversing the Aegean Sea. Its strategic location has meant it has witnessed centuries of maritime activity, from ancient trade routes to modern-day tourism. For the inhabitants of Santorini and Thirasia, the channel has always been a connection, facilitating travel and trade between the islands. Modern ferry services and private vessels regularly navigate these waters.