Volcanoes PART 1
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This document discusses different types of volcanoes. It provides descriptions of cinder cones, shield volcanoes, composite volcanoes, and lava domes. Cinder cones are symmetrical cones up to 1,200 feet tall formed from a single vent. Shield volcanoes are very broad with shallow slopes and can be over 30,000 feet tall. Composite volcanoes are also known as stratovolcanoes, ranging from 1-10 km wide and up to 10,000 feet tall with steep slopes. They have explosive, dangerous eruptions. Lava domes are much smaller formations that occur when lava is too viscous to flow, piling up in a dome shape around 100 feet tall. Examples of each type
Volcanoes PART 1
- 1. JANET BRIGIDA A. CATIPON Grade 9 Science Teacher, MHS MAE-Chemistry, BSU Malolos V O L C A N O E S UNIT III - EARTH & SPACE
- 2. Choose the letter of the best answer. Pre-Assessment
- 3. 1. Which characteristic of magma mainly determines its explosiveness? a. color b. amount c. temperature d. silica content
- 4. 2. Which of the following characteristics of a volcano depends on its magma emission? a. age b. size c. shape d. location
- 5. 3. Which of the following factors associated with huge volcanic eruptions may cause the decrease in the Earth’s average temperature for a few years? a. heat b. light c. acid rain d. volcanic ash
- 6. 4. A thick layer of volcanic ash can be heavy enough to collapse the roofs of buildings because ash is ________. a. is solid. b. cannot be blown by winds. c. becomes heavier as it cools. d. consists of tiny fragments of rocks that becomes heavy as they file up.
- 7. 5. Which of the following is an active volcano in the Philippines? a. Apo in Davao b.Bud Datu in Sulu c.Isarog in Camarines Sur d.Kanlaon in Negros Oriental
- 8. LEARNING OBJECTIVES • Define what is a Volcano • Explain how volcanoes are formed • Identify the types of volcanoes • Characterize a volcano
- 10. ACTIVITY 1 (Work in Groups) Based on the presented pictures of Mayon Volcano, give at least five descriptions of a volcano. Use a volcano concept map.
- 11. WHAT IS A VOLCANO?
- 12. A VOLCANO is a vent from which the material from a magma chamber escapes. Volcanic eruptions can come from peaky volcanic cones, fractured domes, a vent in the ground, or many other types of structures. VOLCANOES are a vibrant manifestation of plate tectonics processes. Volcanoes are common along convergent and divergent plate boundaries. Volcanoes are also found within lithospheric plates away from plate boundaries. Wherever mantle is able to melt, volcanoes may be the result. WHAT IS A VOLCANO?
- 13. WHAT IS A VOLCANO? VOLCANOES erupt because mantle rock melts. This is the first stage in creating a volcano. Remember from the chapter Materials of Earth's Crust that mantle may melt if temperature rises, pressure lowers, or water is added.
- 14. A. According to their structure B. According to their activity C. According to their eruption CHARACTERISTICS OF A VOLCANO
- 15. TYPES AND CHARACTERISTICS OF A VOLCANO
- 16. CHARACTERISTICS OF A VOLCANO Cinder Cones • Less dangerous compared to other types, cinder cones only grow to about 1,000-1,200 feet tall. • cinder cones are usually created from a single opening. • the opening of a cinder cone is a cone-shaped structure, while the steeps are formed of the erupted, fragmented cinders that fall close to the chimney/vent. • The manner of eruption for cinder cones is relatively simple. When the lava erupts, cinders of it are blown into the air. These fragmented cinders fall a short distance from the opening, thus creating the cone. Examples: Paricutín in Mexico, Lava Butte, Sunset Crater
- 17. CINDER CONE
- 18. CHARACTERISTICS OF A VOLCANO
- 19. CHARACTERISTICS OF A VOLCANO Shield Volcano • Shield volcanoes can be very, very big in size. However, they are not as dangerous as that size might make it seem. This is because the eruption of lava out of shield volcanoes is not accompanied by pyroclastic material (bursts of gas and particles). • Shield volcanoes may be tall but tend to be very broad, with less steep slopes than other volcanoes. • Shield volcanoes can be huge because of their ample supply of magma. For example, Mauna Loa is a shield volcano that rises more than 30,000 feet above its base on the bottom of the ocean. Examples: Hualalai, Mauna Loa, Kohala Volcano
- 20. Shield Volcano
- 21. CHARACTERISTICS OF A VOLCANO
- 22. CHARACTERISTICS OF A VOLCANO Composite Volcano • Composite volcanoes are also known as strato volcanoes. Composite volcanoes are reasonably big and can rise up 8,000- 10,000 feet. • They can range anywhere from 1-10 km in diameter. Their eruptions are dangerous and explosive in nature, with many layers of lava and pyroclastic materials, the current of rock and gas that can reach 1,800°F and 450 mph, killing any living organism in its path immediately. Example is the Pompeii Volcano • The general structure of composite volcanoes is tall and symmetrical and with steep sides. • Commonly, composite volcanoes erupt hot gases, ash, lava, and pumice as well as stiff, slow-moving lava. Moreover, deadly mudflows—also commonly known as ‘lahars’—can also accompany the eruption.
- 23. CHARACTERISTICS OF A VOLCANO Composite Volcano • Composite volcanoes are believed to kill the most people because of their deadly nature and high numbers. Apart from their dangerous side, composite volcanoes are also famous because they comprise some of the most beautiful mountains on planet Earth. For example, Mount Fuji of Japan and Mount Shasta in California are two famous composite volcanoes. Examples: Mount Fuji, Mount Shasta Mount St. Helens, Mount Rainier
- 25. CHARACTERISTICS OF A VOLCANO
- 26. CHARACTERISTICS OF A VOLCANO Lava Domes • Unlike composite and shield volcanoes, lava domes are of significantly smaller stature. They are formed when the lava is too viscous to flow to a great distance. As the lava dome slowly grows, the outer surface cools and hardens as the lava continues to pile within. Eventually, the internal pressure can shatter the outer surface, causing loose fragments to spill down its sides. • Generally, such lava domes are found on the flanks of larger composite volcanoes. Examples: There are lava domes within the crater of Mount St. Helens, Chaitén lava dome, Lassen Peak
- 27. Lava Domes
- 28. Different Types of Volcanoes SUMMARY Type of Volcano Shape Height Slope Cinder Cone, AKA Scoria Cone Symmetrical cone Up to 1,200 feet (370 meters) 30-40 degrees Shield Tall and broad Up to over 30,000 feet (9,000 meters) Roughly 10 degrees near the base and 5 degrees near the top Composite, AKA Strato Tall, steep, and symmetrical Up to 8,000 feet (2,400 meters) Roughly 6 degrees near the base and roughly 30 degrees near the top Lava Dome Dome Up to 330 feet (100 meters) 25-30 degrees
- 29. LET’S TRY THIS…. Mount Pinatubo Caldera
- 30. LET’S TRY THIS…. Mount Krakatoa Composite
- 31. LET’S TRY THIS…. Kilauea Volcano Shield Volcano
- 32. LET’S TRY THIS…. Crater of Mount St. Helens Lava Domes
- 33. TRY IT ON YOUR OWN…. Chaiten Volcano
- 34. TRY IT ON YOUR OWN…. Lassen Peak
- 35. TRY IT ON YOUR OWN…. Mount Kanlaon
- 36. TRY IT ON YOUR OWN…. Mount Etna
- 37. TRY IT ON YOUR OWN…. Mount Piracutin in Mexico
- 38. The End… Nature is BEAUTFUL especially when WELL-TAKEN CARED OF, But Nature can be DANGEROUS when DISTURBED… JUST LIKE US.