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Engineering Active faults of pakistan

1. Azhar Mahmood Roll # 225 EVENING B BS APPLIED GEOLOGY 2. ACTIVE FAULTS OF PAKISTAN PRESENTING TO: SIR MIRZA SHAHID BAIG 3. Active Fault • An active fault is a fault…

Documents Hazard and Disaster Situationer.ppt

SCHOOL DISASTER RISK REDUCTION AND MANAGEMENT TRAINING (SDRRMT) Provincial Disaster Risk Reduction and Management Office Camarines Norte edc1925 edc1925 The Philippines is…

Documents 10.pdf

Geothermics 34 (2005) 99–118 Interpretation of a well interference test at the Chingshui geothermal field, Taiwan Kai C. Fan, M.C. Tom Kuo∗, Kan F. Liang, C. Shu Lee,…

Education GPS Slip Rates

1. GPS constraints on continental deformation in the Africa-Arabia- Eurasia continental collision zone and implications for the dynamics of plate interactions Robert Reilinger,1…

Documents Unit 6 – Chapter 17 The Physical Geography of North Africa, Southwest Asia, and Central Asia.

Slide 1Unit 6 – Chapter 17 The Physical Geography of North Africa, Southwest Asia, and Central Asia Slide 2 I. Section I The Land Slide 3 A. Seas & Peninsulas Seas…

Documents Objective: Identify the types of plate boundaries and the land features and geologic events that...

Slide 1 Objective: Identify the types of plate boundaries and the land features and geologic events that each feature makes. Slide 2 Transform boundaries exist where two…

Documents 1 - Earth’s Layers The Earth's rocky outer crust solidified billions of years ago, soon after the....

Slide 1 1 - Earth’s Layers The Earth's rocky outer crust solidified billions of years ago, soon after the Earth formed. This crust is not a solid shell; it is broken…

Documents Plate tectonics Yes, the continents do move! (SC.7.E.6.5)

Slide 1 Plate tectonics Yes, the continents do move! (SC.7.E.6.5) Slide 2 Pre-assessment 1. Earth’s mantle plays an important role in plate tectonics. Why is the mantle…

Documents Litoshpere..Crust & Rigid upper mantle Astenosphere – weak and capable of flow Oceanic and...

Slide 1 Litoshpere..Crust & Rigid upper mantle Astenosphere – weak and capable of flow Oceanic and Continental crust Oceanic – 6-12 km thick, dense heavy, basalt,…