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Task 3: Compare your estimated speed of an Atlantic tsunamiwave from Part III to the calculated speed of the 1755 Atlantic tsunami from Part IV. BASED ON THIS COMPARISON, do you think that the method used in Part III to determine tsunami speed based on the average depth of the ocean is appropriate and accurate enough for making safe estimates for the arrival times of Atlantictsunamis? Explain/defend your answer.

Task 3: Compare your estimated speed of an Atlantic tsunamiwave from Part III to the calculated speed of the 1755 Atlantic tsunami from Part IV. BASED ON THIS COMPARISON, do you think that the method used in Part III to determine tsunami speed based on the average depth of the ocean is appropriate and accurate enough for making safe estimates for the arrival times of Atlantictsunamis? Explain/defend your answer.

Applications and Investigations in Earth Science (9th Edition)
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
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Part IV Task 3 Compare Question. Explain/defend answer.
PARTIV: TESTING YOUR ESTIMATE – LISBON QUAKE OF 1755 3500 miles Task 1: Distance from quake epicenter to San Juan, Puerto Rico: Task 2: Calculated speed of 1755 Tsunami: 438 miles/hr Task 3: Compare your estimated speed of an Atlantic tsunamiwave from Part III to the calculated speed of the 1755 Atlantic tsunami from Part IV. BASED ON THIS COMPARISON, do you think that the method used in Part III to determine tsunami speed based on the average depth of the ocean is appropriate and accurate enough for making safe estimates for the arrival times of Atlantic tsunamis? Explain/defend your answer.
Transcribed Image Text:PARTIV: TESTING YOUR ESTIMATE – LISBON QUAKE OF 1755 3500 miles Task 1: Distance from quake epicenter to San Juan, Puerto Rico: Task 2: Calculated speed of 1755 Tsunami: 438 miles/hr Task 3: Compare your estimated speed of an Atlantic tsunamiwave from Part III to the calculated speed of the 1755 Atlantic tsunami from Part IV. BASED ON THIS COMPARISON, do you think that the method used in Part III to determine tsunami speed based on the average depth of the ocean is appropriate and accurate enough for making safe estimates for the arrival times of Atlantic tsunamis? Explain/defend your answer.
PART I: 2004 INDIAN OCEAN TSUNAMI SPEED Tasks 1 Tasks 2 Tasks 3 Distance (miles) Travel time (hrs) Tsunami speed (mile/hr) Indian Ocean Epicenter to St. Denis, Reunion Is. _3200miles_ _7 hours_ 457miles/hour_ PART II: 2011 PACIFICOCEAN TSUNAMI SPEED Tasks 1 Tasks 2 Tasks 3 Distance (miles) travel time (hrs) Tsunami speed (mile/hr) Pacific Ocean Epicenter to Crescent City CA: 4645miles_ 9 hours _516mile/hr_ PART III: ESTIMATING SPEED OF ATLANTIC OCEAN TSUNAMI Graph A Indian Ocean Ave. Tsunami speed vs. Ocean depth Depth: 12,900 ft 600 Pacific Ocean Ave. Depth: 14,000 ft 550 Atlantic Ocean Ave. 500 Depth: 11,900 ft 450 400 350 300 11,000 1,442,000 13,000 14,000 15,000 10,000 Average depth of Ocean, feet 40mile Slnanl. Task 3: Estimated Atlantic tsunami speed (in miles/hour) from the graph: 1 Tsunami speed miles/hr
Transcribed Image Text:PART I: 2004 INDIAN OCEAN TSUNAMI SPEED Tasks 1 Tasks 2 Tasks 3 Distance (miles) Travel time (hrs) Tsunami speed (mile/hr) Indian Ocean Epicenter to St. Denis, Reunion Is. _3200miles_ _7 hours_ 457miles/hour_ PART II: 2011 PACIFICOCEAN TSUNAMI SPEED Tasks 1 Tasks 2 Tasks 3 Distance (miles) travel time (hrs) Tsunami speed (mile/hr) Pacific Ocean Epicenter to Crescent City CA: 4645miles_ 9 hours _516mile/hr_ PART III: ESTIMATING SPEED OF ATLANTIC OCEAN TSUNAMI Graph A Indian Ocean Ave. Tsunami speed vs. Ocean depth Depth: 12,900 ft 600 Pacific Ocean Ave. Depth: 14,000 ft 550 Atlantic Ocean Ave. 500 Depth: 11,900 ft 450 400 350 300 11,000 1,442,000 13,000 14,000 15,000 10,000 Average depth of Ocean, feet 40mile Slnanl. Task 3: Estimated Atlantic tsunami speed (in miles/hour) from the graph: 1 Tsunami speed miles/hr
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