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Books > Earth & environment > Earth sciences > Geology & the lithosphere > General
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United States Circuit Court of Appeals for the Ninth Circuit, Vol. 1 of 3
- Sterling Carr, a Corporation, Bankrupt, and Fidelity and Deposit Company of Maryland, a Corporation, Appellants, vs. Hermosa Amusement Corporation, Ltd., a Corporation, and J. M. a
(Hardcover)
U S Court of Appeals Ninth Circuit
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R938
Discovery Miles 9 380
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Ships in 12 - 17 working days
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The geology of the Cairngorms was created on a timeline that
stretches back hundreds of millions of years. Much of the land is
underlain by granite that formed deep within the Earth's crust and
'surfaced' as the overlying layers of rock were stripped away by
ice, wind and water. The bedrock is hard, and although the area has
been heavily glaciated, still boasts 18 Munros, the highest of
Scotland's peaks. The area attracts climbers, walkers and assorted
adventurers who want to pit themselves against some of the most
challenging conditions to be found anywhere in the UK. The plants
and animals of the Cairngorms need to be hardy to survive the
severe winter conditions. The higher reaches of the mountains are
rich in montane vegetation such as lichen-rich heath and other
habitats support many rare species.
West Somerset is an area of great geological diversity, straddling
the Tees-Exe Line between highland and lowland Britain. The story
of the last 400 million years of Earth history can be gleaned from
its rocks: the opening and closing of oceans, the collision of
continents and a journey across the Equator. The area may also
provide the key to settle the controversy about the origin of
South-West England, whose ancient geology is so different from the
rest of the country. This unique and diverse geology is also the
reason why it is one of the most beautiful and varied stretches of
landscape in England. With nearly 170 illustrations, including
maps, charts, diagrams and colour photographs, this book describes
and explains the evidence for the geological history of the area,
from the Palaeozoic, through the Mesozoic to the Pleistocene and
Holocene. Regional guides, which discuss the factors that led to
the landscape we see today and offer places of interest to visit,
cover: the Northern Brendon Hills and Minehead; the Southern
Brendon Hills; Wellington and the Blackdown Hills; Wiveliscombe and
the Vale of Stogumber; the Quantock Hills; West Somerset coast and
the Cannington and Bridgwater Lowlands.
This book is one of a popular and exciting series that seeks to
tell the story of some of Britain's most beautiful landscapes.
Written with the general reader - the walker, the lover of the
countryside - firmly in mind, these pages open the door to a
fascinating story of ancient oceans, deltas, mineralization and
tundra landscapes. Over millions of years the rocks that now form
the spectacular terrains of the White Peak and the Dark Peak were
laid down on the floors of tropical seas and deformed by plate
tectonics before being shaped by streams and rivers. The white
limestone was fretted into its own distinctive landscape above
hidden cave systems; then generations of miners and farmers
modified and contributed to the landscapes we see today. With the
help of photographs that are largely his own, geologist Tony
Waltham tells the remarkable story of the Peak District, explaining
just how the landscapes of limestone plateau, grit moors and river
valleys came to look as they do. Including suggestions for walks
and places to visit in order to appreciate the best of the National
Park's landforms, this accessible and readable book opens up an
amazing new perspective for anyone who enjoys this varied and
beautiful area.
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