Home About Us Contact Us Site Map Links Library
 
 
 
Gardener Tips
Home Garden And Gardening
Flowers
Roses
Garden Accesories
Decorative Plants
Garden Design
Garden Planning
The Water Garden
Garden Topography
Sculpture
Containers For Garden
Designing Your Garden
Garden Construction
Drawing Up Your Plan
Cement Garden
Materials Of Garden
Patio Ornaments
Garden Path
Boundaries
Trees
Japanese Style Garden
Outdoor
Plants
Garden Walls
Garden Fences
Rhododendrons
Clematis
Garden Screens
Annuals
Biennials
Bulbs
Lilies
Water Garden
Garden Basket
Season
Techniques
Garden Tools
Cultivation
Protection
Home
New York
Country
Town Flowers
Garden Blocks
Herbs
Blue Roses
Red Roses
Scent Gardens
Large Gardens
Garden Fall
 
 

Unique Home Furniture, Home Decorating and Home Decoration Store

Drowned Topography:

Drowned Topography The Scottish islands vary too much to be regarded as a physiographic unit, but they are grouped together here because many of them, particularly the Shetlands, show obvious evidence of a drowned topography. This effect, due to late-and post-Pleistocene rises in sea level, also affected the sea lochs of the mainland. Off northwestern Scotland there are two chains of islands —the Outer Hebrides, from Lewis to Barra, and, somewhat less well defined, the inner Hebrides, including Skye, Rhum, Muck' Eigg, and Mull. In this province the highest mountains are in Mull—Ben More, the tallest, reaching 3,169 feet (955 meters).

In one of the most famous eruptions in I tory, a major engulfment of one of the peal Krakatau (Krakatoa) in the straits between} and Sumatra reduced it to a height below | level and caused a tidal wave 120 feet 1 which drowned more than 36,000 people. 1 followed a terrific explosion on Aug.


A fjord is a U-shaped valley that has been deepened by a glacier and afterwards invaded by the sea. Fjords are common in Scandinavia, Canada, Greenland and Chile. A ria coast is a system of river valleys that has been drowned when the coast sinks or the sea level rises. An example is the Sydney area, Australia.
 
 
  Home | About Us | Contact Us | Site Map | Links | Library