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Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. Volcán de Flores is the most prominent stratovolcano in a volcanic field composed of several small volcanoes in southern Guatemala. It is located approximately 10 km west of the city of Jutiapa.A stratovolcano, sometimes called a composite volcano, is a tall, conical volcano with many layers (strata) of hardened lava, tephra, and volcanic ash. Stratovolcanoes are characterized by a steep profile and periodic, explosive eruptions. The lava that flows from…mehr

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Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. Volcán de Flores is the most prominent stratovolcano in a volcanic field composed of several small volcanoes in southern Guatemala. It is located approximately 10 km west of the city of Jutiapa.A stratovolcano, sometimes called a composite volcano, is a tall, conical volcano with many layers (strata) of hardened lava, tephra, and volcanic ash. Stratovolcanoes are characterized by a steep profile and periodic, explosive eruptions. The lava that flows from stratovolcanoes tends to be viscous; it cools and hardens before spreading far. The magma forming this lava is often felsic, having high-to-intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less-viscous mafic magma.