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Aim: How are Landscapes (landforms) formed? Landforms are the results of interaction of tectonic forces, processes of weathering, erosion, deposition,

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Presentation on theme: "Aim: How are Landscapes (landforms) formed? Landforms are the results of interaction of tectonic forces, processes of weathering, erosion, deposition,"— Presentation transcript:

1 Aim: How are Landscapes (landforms) formed? Landforms are the results of interaction of tectonic forces, processes of weathering, erosion, deposition, and climate.

2 What are the characteristics of a landscape? 1.Elevation 2.Bedrock 3.Stream drainage pattern 4.Soil characteristics 5.Slope All these help to define the landscape pattern of a region

3 What factors influence landscape development? 1.Uplifting forces (tectonic forces)- originate beneath or within Earth’s lithosphere. 2.Leveling or destructional forces - lower and level out Earth’s surface by breaking the landmasses, transporting sediments along Earth’s surfaces, and depositing sediments. ForcesSource of Energy Uplifting- Volcanic actions, earthquakes and any other movement associated with plate interactions Earth’s interior due to radioactive decay materials and from residual heat from Earth’s formation Leveling- Weathering, erosion, deposition, and sinking Energy from the sun-insolation-and gravity.

4 Types of Landscape Destructive Forces (Leveling)Constructive Forces (Uplifting)

5 More on Landforms Leveling Forces

6 The topographic pattern streams take are not necessarily totally random. They are affected by rocks and their structures. Drainage Patterns

7 Factors affecting Landscape Features Wherever earthquakes and volcanic activities occurs, uplifting is usually the dominant force. Slopes rise up

8 Drainage Patterns drainage pattern: the arrangement of a river and its tributaries types: – dendritic: resembles the branches of a tree or veins in a leaf

9 Drainage Patterns (cont.) – rectangular: when tributaries have frequent 90 o bends and tend to join other streams at right angles; develops on regularly fractured rock

10 Drainage Patterns (cont.) – radial: when the streams diverge outward like spokes of a wheel; formed on high conical mountains

11 Stream Pattern and Geologic Structures


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