Get our newsletter!
Zu den weltweiten Vulkanreisen von Volcano-Adventures!
Volcanoes & Earthquakes - new app for Android
Volcanoes & Earthquakes - app for iPhone & iPad

Garantierte Reisen:
2.-18. Nov 2019: Volcanoes and Spices - N-Sulawesi + Halmahera (Indonesien)
17.-21. Nov 2019: Krakatau Vulkanspezialreise - Krakatau Vulkan (Indonesien)
17.-30. Nov 2019: Wüste, Salz und Vulkane - Danakilwüste (Äthiopien)
9.-17. Mai 2020: Feuerberge Siziliens - vom Stromboli zum Ätna - Äolische Inseln + Ätna
11.-29. Aug 2020: Kamchatka - Land of Colors - Kamchatka (Russia)
: Plätze frei / : garantiert / : Wenig freie Plätze / : Ausgebucht
Zufallsfotos
News aus Milos:
New photos from Milos, Greece, taken during our tour in spring 2013

Dienstag, Jul 09, 2013
[mehr]
 

Milos Vulkan

stratovolcanoes, phreatic craters, lava domes 748 m
Griechenland, 36.67°N / 24.48°E
Aktueller Status: normal / ruhend (1 von 5) | Berichte
Milos Vulkan-B cher | Tours
Last update: 26 Mär 2019
Typische Aktivität: Explosive, hydrothermal explosions
Ausbrüche des Milos: approx 2000 years ago: phreatic explosions
70.000 - 90.000 years ago (Tsingrado volcanic craters) Elevated submarine volcanic ash deposits of the spectacular Sarakiniko coast of Milos
UhrzeitMag. / TiefeDistanceOrt
Thu, 17 Oct 2019
Thu, 17 Oct 16:33 UTCM 2.6 / 29 km27 kmSouthern Greece
Milos is a volcanic island in the southern Aegean Sea and well known for its extensive mineral deposits and fine beaches. It is part of the Hellenic volcanic arc, that also comprises the volcanic islands of Santorini and Nisyros. Considered dormant, Milos presents strong hydrothermal activity, caused by subduction of the African under the Aegean plate.

Beschreibung:

Milos is a mainly volcanic island (like the neighbour islands of Kimolos, Polyaigis, Antimilos, Glaronisia and Akradia islands). Some older metamorphic rocks are exposed, that were formed many millions of years before the existence of the island (schists, prasinites, calc-schists, etc.). Later these layers were covered by sea-sediments. Volcanism on Milos started in upper Pliocene and continued until late Pleistocene. The last volcanic eruptions on Milos (90.000 B.C.) took place in the area of Tsingrado volcano. Volcanicm on Milos is similar to the other parts of the Hellenic Volcanic Arc comprising also Methana, Santorini and Nisyros.

It is caused by the geodynamic convergence of the African and Aegean plates. The collission and subduction of the African plate produces calcalkalines (andesitic, dacitic) magmas and rocks. The eruptive phases on Milos produced mainly acidic tuffs & pumice, pyroclastic flow and lahar deposits. During extrusive phases a number of andesitic volcanic domes were built and some lavaflows emplaced. Towards the "end" of the most recent volcanic activity many phreatic explosions produced small craters (like near Agia Kyriaki or Achivadolimni) visible still today. Most of the volcanic rocks on Milos were strongly hydrothermally altered, which makes Milos become an important supplier for mining minerals like baryte, silver, perlite, caolin, bentonite and in the future perhaps even gold (Hontrovouno). Studies show the presence of a high-temperature hydrothermal system (up to 310 deg. C) below the island, responsible for the abundance of active fumaroles (e.g. in the Kalamos area). This reservoir might be related to an active magma chamber and therefore, future volcanic activity on the island can not be excluded.

Milos Fotos:




Milos Vulkanresien
Silber der Ägäis (8-tägige geologische Wander- und Studienreise nach Athen, Laurion und Milos, Griechenland)
Santorini & Milos Kombination (Zwei der schönsten Vulkaninseln Griechenlands)

Letzte Satellitenbilder


See also: Sentinel hub | Landsat 8
 

Mehr auf VolcanoDiscovery:

Copyrights: VolcanoDiscovery und andere Quellen wie angegeben.
Verwendung von Bildern:Text und Fotos auf dieser Webseite sind urheberrechtlich geschützt. Weitere Verwendung und Kopieren ohne vorherige Genehmigung ist untersagt. Wenn Sie Fotos für private oder gewerbliche Zwecke nutzen wollen, kontaktieren Sie uns bitte.