'Shaped valley' presentation slideshows

Rivers

Rivers. Learning Intention. How people use rivers? Why is water and rivers important? Why study rivers? What is the hydrological cycle?. Starter. Write down 5 words that come to mind when I say the next word Rivers. What good are rivers?. Why study rivers?. Water. Effect on man.

1.01k views • 57 slides

GLACIATION

GLACIATION. Glaciation. Learning Objectives Understand the term glaciation Understand the formation of glacier ice. Discover how glaciers move. Learn about the different types of glaciers Have a brief understanding of the formation of landforms of erosion and deposition.

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Rivers

10.0. Rivers. 10.1. The Journey of a River. The journey a river takes from its source to the sea. 10.2. The Stages of a River. The journey a river takes from its source to its mouth is called the course of the river. This course is broken up into three different stages. Lower Course.

534 views • 45 slides

Glaciation

Glaciation. Learning Intentions Be able to understand the processes which occurred during the last ice age. Be able to describe and explain the formation of features formed during glacial periods. Processes Of Weathering Freeze-Thaw. Water enters crack.

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541 views • 40 slides

Ch. 23.3 Water Shapes the Land

Ch. 23.3 Water Shapes the Land. Objectives: What is the most important factor influencing the ability of a stream to cause erosion? What features are formed by surface water erosion? What features are deposited by running water? What causes ground water erosion?.

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Change Over Time

636 views • 36 slides

Glaciation of Canada

Glaciation of Canada. Learning goals:. Further your knowledge and understanding of earth-shaping forces and processes Identify a evidence of earth-shaping forces and processes. WHAT IS A GLACIER?. WHAT IS A GLACIER?. WHAT IS A GLACIER?. WHAT IS A GLACIER?. - a large section of ice and

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Glaciers

Glaciers. Glaciers. V. Glacial Erosion Mechanisms Glacial Quarrying Masses of (fractured) bedrock are lifted from the bed and incorporated into the ice Melt water penetrates the cracks ? frost wedging 2. Glacial Abrasion

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Name Form Candidate Number

Name Form Candidate Number. Hypothesis. Blackwood has a higher Sphere of influence than Cefn Fforest. Introduction. A brief overview about what you intend to do and where you intend to do it. Aim.

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Think (20 secs) Pair (40 secs) Share (as a class)

1. Match up the aerial photo with the land photo. C. A. F. Think (20 secs) Pair (40 secs) Share (as a class). 2. Put them in the right order. D. B. E. Upper? Middle? Lower?. Upper? Middle? Lower?. Upper? Middle? Lower?. Upper? Middle? Lower?.

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Ice

Glacial Erosion. 1. Rocks frozen into glacier ice. Ice. 2. Glacier moves. Valley Floor. 3. Rocks scrape along the valley floor and erode it. This type of erosion is called abrasion. Glacial Erosion. 1. Ice freezes around bits of rock.

417 views • 16 slides

Changes to Land

Changes to Land . Grades 3-5 . Features . Features on the surface of Earth such as mountains, hills, dunes, oceans, and rivers . Delta. A triangle shaped landform at the mouth of a river as it empties into another body of water. Canyon .

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Cold Environments

Cold Environments. Distinct season below freezing with snow in winter. Can be defined by latitude and altitude ie.~ Polar Arctic and subarctic Periglacial Siberia Mountain Alps. Remember how would you describe a climate graph?. Processes in Glacial Environments :~ Weathering

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EXPEDITION TO GLACIER NATIONAL PARK

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River Landforms represented on O.S. Maps

River Landforms represented on O.S. Maps. V-Shaped Valley. Interlocking Spurs. Waterfall. Meander Examples. Lacustrine Delta. Exam Questions. Glacial Landforms represented on O.S. Maps. Truncated spurs

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Glaciation and O.S maps

Glaciation and O.S maps. Remember!. Corrie. Arete. Contour lines are very close together showing very steep land. The contour lines are curved showing a bowl-shape Sometimes a tarn is evident. U-Shaped Valley. Where two corries form back to back.

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V-Shaped Valleys

V-Shaped Valleys. &. Interlocking Spurs. V-Shaped Valleys. Weathering over time weakens the sides of the valley and continued vertical erosion at the base of the valley causing movement of materials down the valley sides. This creates the distinctive V shape.

443 views • 4 slides

A V valley is found up the top of a river. Here the river is fast and does not carry much stuff.

Describe how a V-shaped valley forms (4). The sides get washed in to the river by rain and this stuff is moved by the water down to the bottom. V Shaped Valley Vertical Erosion Weathering Slopes Erosion Material High Discharge Powerful Energy Interlocking spurs Load Steep River bed

160 views • 3 slides