Abdul Jabbar th Semester 8 UAJK STRUCTURE AND STRATIGRAPHY OF SANDAL, SADIQABAD, PIPLI, GHANAIR AND SANDI AREAS OF DADYAL, DISTRICT MIRPUR, AZAD JAMMU AND KASHMIR, PAKISTAN…
Dobras, Falhas e Montanhas DOBRAS, FALHAS E MONTANHAS DOBRAS E EMPURRÕES Enormes cadeias de montanhas se formam quando placas convergem. Rochas Contorcidas mostram a…
1. Fieldwork StudyRogador, Jacob IV E.Sarael, Jenes Mae 2. INTRO Structural Geology is the science that deals with the study of the structures of rocks insofar as it is resulted…
Slide 1 Slide 2 Earths Crust Slide 3 Convection currents Slide 4 Continental drift – idea that continents have moved slowly to their current positions due to convection…
Slide 1Geologic Time, Unconformities and Relative Dating Uniformitarianism Appendix A Slide 2 Law of Original Horizontality, Law of Superposition All sedimentary rocks are…
Slide 1 Slide 2 1.Tension – stretches rock, they become thin in the middle 2. Compression – pushes rock together, squeezes rock until it folds or breaks 3. Shearing –…
Slide 1Discussion Questions Chapter 16 Slide 2 Part I Slide 3 Question 1 n Before Hutton, it was widely assumed that the features of the Earth's surface were: n A. always…
1.S6E5e2. • What are earthquakes?• What conditions cause earthquakes?• What are some vocabulary wordsassociated with earthquakes?• How are earthquakes measured?•…
1.A normal fault drops rock on one side of the fault down relative to the other side.A normal fault is caused by tension.2. A thrust fault raises rock on one side of the…
1.A normal fault drops rock on one side of the fault down relative to the other side.A normal fault is caused by tension.2. A thrust fault raises rock on one side of the…