'Synclines' diaporamas de présentation

Chapter 11

Chapter 11. Mountain Building. I) Where Mountains Form. Mountain Belts 1) Most Mountains are associated with convergent plate boundaries 2) Most mountains occur in long belts that follow convergent boundaries 3) Himalayas lie along a current convergent boundary

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Crustal Deformation

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WHAT IS OROGENY? Processes of mtn building

WHAT IS OROGENY? Processes of mtn building. Distinctive patterns of deposition eugeocline, miogeocline Deformation Folding and thrust-faulting Metamorphism Intrusions: batholiths, etc Volcanic Activity. TYPES OF MOUNTAINS. Volcanic: Shield and composite

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11.2A Folds, Faults, and Mountains

11.2A Folds, Faults, and Mountains. Folds and Faults. Folds. Over millions of years, stress forces can bend rock like a ribbon or soft dough. Steady pressures of stress over long periods of time affect sedimentary layers and can fold them into dramatic forms. Folds. F olds :

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11.30.2010

11.30.2010. 11.30.2010. Do Now:. Agenda:. Objective : I can describe and draw how anticlines and synclines are different. Question : How is relative age different from absolute age? Have your homework assignments out on your desks as you are working!. Do Now Check Homework

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