science - volcano

Cards (62)

  • The Philippines is home to several volcanoes due to its location in the Pacific Ring of Fire
  • Volcano refers to a mountain or hill
  • Crater or Vent is where lava, rock fragments, hot vapor, and gas are contained or have been erupted into the earth's surface
  • Lava originated from molten materials called magma
  • Magma is found beneath the surface of the Earth
  • Volcanism includes any activity that involves the movement of magma toward or onto the surface
  • Summit is the highest point or the apex of the volcano, with an opening called vent
  • Slopes are the sides or flanks of a volcano radiating from the main or central vent
  • Base is the lower outer part of the volcano
  • Magma Chamber is a region beneath the vent of a volcano where molten rock or magma is deposited or stored before eruption
  • Main Vent is the main opening or outlet on the surface of a volcano that emits lava, gases, ash, or other volcanic materials
  • Conduit is an underground central tube-like or pipe-like structure that connects the magma chamber to the crater through which the magma travels
  • Side Vent is a smaller outlet through which magma escapes
  • Crater is the mouth of the volcano, a funnel-shaped or bowl-shaped hollow at the top of the vent from where magma, ash, and gas come out
  • Lava is molten rock given off onto the surface of the Earth during a volcanic eruption
  • Ash and Gas Cloud is a mixture of rock, minerals, glass particles, and gases expelled or pushed out of the volcano during a volcanic eruption
  • Cinder Cone Volcano:
    • Simplest type of volcano
    • Built from particles and blobs of solidified lava ejected from a single vent
    • Most cinder cones have a steep slope and wide crater
    • Examples include Taal Volcano in Batangas and Mount Mayabobo in Quezon
  • Composite Volcanoes or Stratovolcanoes:
    • Large, steep-sided, symmetrical cones formed from alternating layers of lava flows, volcanic ash, cinders, blocks, and pyroclastic materials
    • Formed from viscous lava that does not flow easily
    • Examples include Mount Mayon in Albay and Mount Arayat in Pampanga
  • Shield Volcanoes:
    • Large, broad volcanoes built almost entirely of fluid lava flow
    • Easily identified by their tall and broad, flat, rounded shapes
    • Examples include Mauna Loa in Honolulu, Hawaii and Fernandina in Galapagos Island
  • Types of Volcanoes Based on Activity:
  • Active Volcanoes:
    • Volcanoes that have had at least one eruption during the past 10,000 years
    • Show regular activity like emission of gases, lava, and ash flows
  • Inactive Volcanoes:
    • Volcanoes that have not erupted for the last 10,000 years and are not expected to erupt again in the future
    • Show no signs of volcanic activity for a long period due to cut-off magma supply and intensive weathering and erosion
  • Potentially Active Volcanoes:
    • Volcanoes with no records of volcanic activity but are morphologically young-looking
  • Phreatic or Hydrothermal:
    • Steam-driven eruption as hot rocks come in contact with water
    • Short-lived and characterized by ash columns
  • Phreatomagmatic:
    • Violent eruption due to contact between water and magma, resulting in high-speed emission of pyroclastic materials
  • Strombolian:
    • Periodic weak to violent eruption characterized by a fountain of lava
  • Vulcanian:
    • Characterized by tall eruption columns with pyroclastic flow and ash fall tephra
  • Plinian:
    • Excessively explosive eruption of gas and pyroclastic materials
  • Signs of an Impending Volcanic Eruption:
  • Increased steaming activity
  • Crater Glow
  • Landslide from summit areas
  • Variation in the chemical content of springs and crater lakes
  • Development of new thermal areas
  • Increase in the temperature of wells and crater lakes near the volcano
  • Ground swells
  • Drying up of springs/wells around the volcano
  • Drying of vegetation around upper slope
  • Occurrence of volcanic tremors
  • Magma is the molten rock underneath volcanoes, formed at destructive plate boundaries and rich in silicate