Presentation on theme: "Volcanoes. What is a volcano? A volcano is any place on the planet where some material from the inside of the planet (magma) makes its way through to."— Presentation transcript:
What are the properties of magma? 1. Viscosity – the ability of magma to resist flow; high viscosity is associated with explosive eruptions 2. Gas content – the amount of gas dissolved in magma; high gas levels are associated with explosive eruptions
What are the types of volcanic eruptions? 1. Plinian Magma is highly viscous and has high gas levels Explosive eruptions produce a towering plume of pyroclastic material and fast moving lava
Pyroclastic materials refer to hot ash, pumice, rock fragments, and volcanic gas. Once deposited, the ash, pumice, and rock fragments may deform (flatten) and weld together because of the intense heat and the weight of the overlying material.
What are the types of volcanic eruptions? 2. Hawaiian Magma is of low viscosity and has low gas levels Subdued eruptions may produce a fountain of fire or a slow, steady lava flow
What are the types of volcanic eruptions? 3. Strombolian Magma has a fairly high viscosity and low gas levels, taking time to build up a high gas pressure for an eruption to occur Small, explosive eruptions come in very short bursts, spewing small amounts of lava and ash into the air accompanied by booming sounds. They may have some lava flow.
What are the types of volcanic eruptions? 4. Vulcanian Magma is highly viscous and has high gas levels Several short, explosive bursts spew out lava, ash and pyroclastic bombs. No lava flow occurs.
What are the types of volcanic eruptions? 6. Fissure Occur where plate movement produce fractures in the crust or may also spring up around the base of a volcano Magma flows up through cracks in the ground as a curtain of slow moving lava
What are the parts of a volcano? 1. Summit crater – the mouth of the volcano 2. Magma chamber – a pool of magma beneath a volcano 3. Central vent – leads from the magma chamber to the crater 4. Edifice – the structure surrounding the central vent
Parts of a Volcano Summit crater Edifice Central vent Magma chamber
What are the parts of a volcano? 5. Other structures Caldera – a large crater-shaped basin produced from the collapse of the volcano edifice Lava dome – a plug of hardened lava at the summit crater
What are the types of volcanoes? 1. Stratovolcano Also known as composite volcanoes With a fairly symmetrical edifice with steep slopes and accessory vents Built up by alternating violent eruptions of pyroclastic material and quiet lava flows
What are the types of volcanoes? 2. Scoria cone volcanoes Also known as cinder cones Small cones with steep slopes and a wide crater Usually associated with eruptions of rock and ash and very few lava flows
Volcanoes on Other Planets 1. Venus – covered with hundreds of geologically young volcanoes 2. Mars – has several volcanic features, including the largest volcano in the solar system, Olympus Mons * Mercury and our moon appear to have ceased being volcanically active.
Volcanoes on Other Planets 4. Saturn’s moons Encaladus – may have ice volcanism Titan – volcanism may account for its dense atmosphere 5. Neptune’s moon Triton – its dense atmosphere may be due to volcanism
Plate Tectonics in the Philippines Several micro-plates are getting squeezed between two convergent plate margins. Black triangles = active subduction zones with "teeth" on the over-riding plate, white triangles = inactive subduction, arrows = transform or major strike-slip faults, red triangles = volcanoes active in the last 10,000 years
Volcanoes in the Philippines With 22 active volcanoes and around 330 potentially active and inactive volcanoes Mostly cinder (scoria) cones, stratovolcanoes and calderas Mudflows are common because of heavy rains. Tsunami are commonly associated with eruptions
Lahar is an Indonesian word for a rapidly flowing mixture of rock debris and water that originates on the slopes of a volcano. Lahars are also referred to as volcanic mudflows or debris flows.
Mayon LOCATION: Albay province Height: 2,460 m asl Type of Volcano: Stratovolcano No. of Recorded Eruptions: 47 since 1616 Latest Eruption: 24 June & 26 July 2001 Most Destructive Eruption: 01 February 1814; 1,200 people perished due to lahars Eruption Types: Strombolian, Vulcanian, Plinian
Kanlaon LOCATION: Negros Island, Central Visayas Height: 2,435 m asl Type of Volcano: Stratovolcano (summit caldera: 15 km² ) No. of Recorded Eruptions: 27 since 1866 Latest Eruption: 10 August 1996 Eruption Types: Hydrovolcanic, Strombolian
Taal LOCATION: Batangas Province Type of Volcano: small cones formed inside a large caldera Highest Point of the Volcano Island: 311 m asl No. of Recorded Eruptions: 33 since 1572 Latest Eruption: 03 September 1977 Destructive Eruptions: several, latest in 1965 as ashfall covered an area of 60 sq. km killed 200 people Eruption Types: Strombolian, Plinian, Hydrovolcanic
Pinatubo LOCATION: at the boundaries of Zambales, Pampanga and Tarlac Height Before the 1991 Eruption: 1,745 m asl Height After the 1991 Eruption: 1,445 m asl Type of Volcano: Stratovolcano with a summit caldera No. of Recorded Eruptions: 2 since 1380 First Observed Major Eruption: 12 June 1991 at 8:51 AM Eruption Type: Plinian
Bulusan LOCATION: Sorsogon Province Height: 1.559 m above sea level (asl) Type of Volcano: Stratovolcano formed inside a caldera No. of Recorded Eruptions: 18 eruptions since 1852 Latest Eruption: 27 November 1994 Type of Eruptions: Hydrovolcanic, Strombolian
Volcanoes and People Destructive effects 1. People may die or become injured 2. Property may be destroyed 3. People may lose their livelihood (farming) 4. Respiratory disease cases may increase 5. Jet planes may malfunction due to ash in engines
Volcanoes and People Beneficial effects 1. New land masses are formed 2. Soil becomes more fertile 3. Commercially important minerals, rocks and gemstones are produced 4. Locations for spas and resorts and as tourist spots 5. Geothermal energy may be harnessed from volcanic heat