1. DEEP COVE CAMP 2013 2. 1.TRAVEL OVER THE LAKEAfter arriving in Manapouri we headed to Pearl Harbour to load the Real Journeys boat to travel across Lake Manapouri. We…
Slide 1EARTH SCIENCE CHAPTER 15 GLACIERS Slide 2 Chapter 15 GLACIERS I. What is a Glacier? Mass of moving ice responsible for the most powerful agents of erosion Types of…
Slide 1 Slide 2 Corrie, cirque, cwm – hollow where a glacier formed Armchair shaped hollow – usually northerly aspect in UK and N. Hemisphere. Steep back wall e.g. Llyn…
Slide 1http://suratiundhiyu.wordpress.com/ VIPUL M DESAI PRESENTS WATERFALLS OF INDIA http://suratiundhiyu.wordpress.com/ SPEAKERS ONCLICK FOR NEXT Slide 2 DUDHSAGAR FALLS-GOA…
Slide 1 Slide 2 Land Use Conflicts Slide 3 Click on the locations marked on the following map with a This will open up a page with information about the land use conflicts…
Slide 1 The landscape around Loch Skene registers the impact of the severe climate of the Loch Lomond Stadial. Small valley and corrie glaciers developed in the higher hills…
1. Glacial environments 2. Sweden after the last ice agearound 10,000 years agoAbove sea-levelUnder sea-level 3. A glacier is a system• Inputs: accumulation of snow and…
1. 1 2 3 4 5 6 7 8 9 2. 1 Red tarn is an example of what glacial erosion feature? 3. 2 What glacial erosion feature is arrow A and arrow B pointing to? A B 4. 3 Explain how…
Slide 1 By the end of today's lessons you will be able to recognize Arêtes and explain the formation of glacial troughs and hanging valleys. Key Words; Glaciated trough…