Plate Tectonics 10.3 08 09

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Types of Boundaries ,[object Object],[object Object],[object Object]

Tectonics – study of formation of crustal features ,[object Object],[object Object]

Divergent Boundary Common at Mid-Ocean Ridges (M-O-R)

Plates move like they are groceries on a conveyor belt

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Earth and Life Science Earth Materials and Processes: Deformation of the Crust The learners shall be able to: 1) explain how the seafloor spreads (S11/12ESId-23); 2) describe the structure and evolution of ocean basins (S11/12ES-Id-24); and 3) explain how the movement of plates leads to the formation of folds and faults (S11/12ES-Id-22). Specific Learning Outcomes At the end of the lesson, the learners will be able to: 1. Discuss the history behind the Theory of Continental Drift; 2. Describe the Continental Drift Theory; 3. Enumerate and explain the evidence used to support the idea of drifting continents; 4. Identify major physiographic features of ocean basins 5. Describe the process of seafloor spreading

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GOAL: To create a poster that explains the phenomena of blue sky using the concept of wavelength and frequency of visible light. SITUATION: As the creative head in the science club of Macasandig National High School, you are tasked to create a poster showcasing the phenomena of blue sky on Science Club bulletin board. PRODUCT: A creative poster explains the phenomena of blue sky. The poster should be in 1/8 illustration board. faults generate earthquakes. S8ES-IIa- 14 Objectives: 1. Describe what fault is and how these faults related to earthquakes. 2. Determine the extent of damage an earthquake can do in a particular location. Article Reading Earthquake wreaks havoc in the Philippines more than 1,000 people are killed when a 7.7-magnitude earthquake strikes Luzon Island in the Philippines on this day in 1990. The massive tremor wreaked havoc across a sizeable portion of Luzon, the country’s largest island, with Baguio City suffering the most devastating effects. The epicenter of the quake, which struck at 4:26 p.m., was north of Manila in the Nueva Ecija province. Reports indicate that the shaking went on for nearly a full minute. Collapsing buildings were the main cause of damage and death. Getting out of a multi-story building was a good safety precaution that afternoon, although many people were injured and a few even died in stampedes of others doing the same thing. At Christian College, a six-story building completely collapsed, trapping approximately 250 students and teachers inside. Heroic rescue efforts saved many, but some victims who did not die in the collapse were found dead later from dehydration because they were not pulled out in time. All types of buildings, including several resort hotels in Baguio, known as the Philippines’ Summer Capital, suffered tremendous damage. Most of the city’s 100,000 residents slept outdoors that evening and during the following week, afraid to return to their homes amid the frequent aftershocks. For days, workers pulled bodies from the demolished buildings in Baguio. The best estimate is that 1,000 bodies were eventually recovered. At least another 1,000 people suffered serious injuries. Rescue efforts were hampered severely because the three main roads into the city were blocked by landslides. Hundreds of motorists were stranded on the roads as well. A fault is a fracture or zone of fractures between two blocks of rock. Faults allow the blocks to move relative to each other. This movement may occur rapidly, in the form of an earthquake - or may occur slowly, in the form of creep. Faults may range in length from a few millimeters to thousands of kilometers. Most faults produce repeated displacements over geologic time. The ground in the area of fault tends to remain not moving because of frictional force between the two opposing plates (boxes). As stronger forces (rubber band) shakes up the fault, the friction (tape) can no longer hold up the plates (box) thus resulting to a slip in the plates t

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Oceanography is an interesting subject. Geological oceanography deals with a lot of unique aspects of the oceans including the ocean morphology and relief, continental margins, tectonic processes acting on the ocean bottoms, marine mineral resources, and the deep sea deposits. The subject also focuses on the never ending dynamic processes like ocean waters, ocean currents and their impacts with reference to space and time. Understanding the tectonic disposition and movement of crustal plates are an important part while studying the earth and atmospheric sciences, in general and oceanography, in particular. The continental margins and the deep ocean basins are the two major aspects to be understood in this subject. This lesson is on the characteristics of continental margins.

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