No. The 1985 eruption of Nevado del Ruiz produced hot ash and pumice.
From all the research I've done I have figured out that it had something to do with the shifting of the tectonic plate it sits on but I'm afraid that's about as detailed as it gets :/
No, Nevado del Ruiz is not a cinder cone volcano. It is a stratovolcano, which is a large, steep-sided volcano built up of many layers of hardened lava, tephra, pumice, and volcanic ash.
Around 2,500 deaths were caused by the most serious eruption of the Nevado del Ruiz volcano in 1985. The town of Armero was covered in a mass of mud and debris (or lahar) which the volcano produced.
Nevado del Ruiz is a stratovolcano, not a shield volcano. Shield volcanoes are typically broad and have gentle slopes created by low-viscosity lava flows, while stratovolcanoes have steep slopes and are composed of alternating layers of hardened lava, tephra, and volcanic ash.
The Nevado del Ruiz volcano is located on a destructive plate boundary whereby the dense, oceanic Nazca plate is being subducted under the less dense, continental South American plate. The melted rock from the Oceanic plate rises to the surface, the pressure builds until the magma erupts from the volcano. It is a composite or strato volcano meaning it is made up of layers of solidified lava and pyroclasic material.
The eruption of 1985 produced gas and ash.
From all the research I've done I have figured out that it had something to do with the shifting of the tectonic plate it sits on but I'm afraid that's about as detailed as it gets :/
No, Nevado del Ruiz is not a cinder cone volcano. It is a stratovolcano, which is a large, steep-sided volcano built up of many layers of hardened lava, tephra, pumice, and volcanic ash.
Around 2,500 deaths were caused by the most serious eruption of the Nevado del Ruiz volcano in 1985. The town of Armero was covered in a mass of mud and debris (or lahar) which the volcano produced.
Nevado del Ruiz is a stratovolcano, not a shield volcano. Shield volcanoes are typically broad and have gentle slopes created by low-viscosity lava flows, while stratovolcanoes have steep slopes and are composed of alternating layers of hardened lava, tephra, and volcanic ash.
The Nevado del Ruiz volcano is located on a destructive plate boundary whereby the dense, oceanic Nazca plate is being subducted under the less dense, continental South American plate. The melted rock from the Oceanic plate rises to the surface, the pressure builds until the magma erupts from the volcano. It is a composite or strato volcano meaning it is made up of layers of solidified lava and pyroclasic material.
Yes. Stratovolcanoes can erupt blocky lava flows, basaltic lava flows, or may erupt explosively.
Composite volcanoes can erupt both mafic and felsic material, but intermediate material is the most common.
The explosiveness of lava from Nevado del Ruiz primarily results from its composition, which is predominantly andesitic to dacitic. This composition contains significant amounts of silica, leading to higher viscosity. The viscosity traps gases, increasing internal pressure until it is released explosively during eruptions. Consequently, the eruptions can produce pyroclastic flows and ash clouds, making the volcano particularly hazardous.
lava
Loud Erupt: The magma is really thick It is cooler lava More silicia Quiet Erupt: Thin Hotter lava low silica
lava shoots out of the top