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Prentice   Hall   EARTH SCIENCE Tarbuck   Lutgens  
Chapter   11 Mountain Building
11.1  Rock Deformation     Factors that influence the strength of a rock and how it will deform include temperature, confining pressure, rock type, and time. ,[object Object],[object Object],-  Most crustal deformation occurs along plate margins.  ,[object Object],Factors Affecting Deformation
11.1  Rock Deformation     Temperature and Pressure ,[object Object],-  Ductile deformation is a type of solid state flow that produces a change in the size and shape of an object without fracturing the object. -  Brittle deformation is the fracturing of an object once its strength is exceeded. Factors Affecting Deformation
11.1  Rock Deformation     Rock Type    Time ,[object Object],[object Object],Factors Affecting Deformation
11.1  Rock Deformation     The three types of stresses that rocks commonly undergo are tensional stress, compressional stress, and shear stress. Types of Stress
Types of Stress
11.1   Rock Deformation     Anticlines ,[object Object],   Synclines    Monoclines ,[object Object],[object Object],[object Object],Folds
Anticlines and Synclines
Monoclines
11.1  Rock Deformation     Normal   Faults ,[object Object],   Reverse   Faults and Thrust   Faults ,[object Object],[object Object],Faults
11.1  Rock Deformation     Joints ,[object Object],   Strike-Slip Fault ,[object Object],Folds
Four Types of Faults
Joints
11.2  Types of Mountains     Folded   Mountains ,[object Object],   Mountains are classified by the dominant processes that have formed them. ,[object Object],Folded Mountains
Folded Mountains
11.2   Types of Mountains     Large-scale normal faults are associated with structures called fault-block mountains. ,[object Object],[object Object],[object Object],Fault-Block Mountains
Fault-Block Mountains
11.2   Types of Mountains     When upwarping produces a circular or elongated structure, the feature is called a dome. ,[object Object],Domes and Basins
Domed Mountains
11.3  Mountain Formation     Most mountain building occurs at convergent plate boundaries. Colliding plates provide the compressional forces that fold, fault, and metamorphose the thick layers of sediments deposited at the edges of landmasses. Mountain Building at Convergent Boundaries
11.3   Mountain Formation     Ocean-Ocean Convergence ,[object Object],   Ocean-Continental Convergence ,[object Object],[object Object],Mountain Building at Convergent Boundaries
Ocean-Ocean Convergence
Ocean-Continental Convergence
11.3   Mountain Formation     Continental-Continental Convergence ,[object Object],Mountain Building at Convergent Boundaries
Continental-Continental Convergence
11.3   Mountain Formation     The mountains that form along ocean ridges at divergent plate boundaries are fault-block type mountains. Mountain Building at Divergent Boundaries
Mountain Building by  Continental Accretion
11.3  Mountain Formation     Not all mountains are formed by plate boundaries. Some are formed by hot spots or regional extension or stretching. Non-Boundary Mountains
11.3  Mountain Formation     Terranes ,[object Object],   Accretion  is a process that occurs when crustal fragments collide with and stay connected to a continental plate. ,[object Object],Continental Accretion
Accretion in Western North America
11.3   Mountain Formation  ,[object Object],   Isostatic Adjustment for Mountains ,[object Object],[object Object],Principles of Isostasy
Isostatic Adjustment
Isostatic Adjustment in Mountains

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Phes Ch11