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'Oh come now, Mr Buchanan. When one goes out into the world, one
always ends up smelling of something or other.' Fergus Buchanan has
led a charmed life: a doting family, a loving sweetheart and the
respect of his neighbours. All is as it should be and nothing
stands between him and the limitless happiness that is his destiny.
But then he is sent from his remote island to retrieve the cursing
stone, and his adventures in the wild world beyond cause him to
question everything he thought he knew. Succeed or fail, nothing
will be the same again. This modern quest is a story of courage,
duty and revenge, of family ties and loves lost and found, of
dragons and postcodes.
According to the accepted wisdom, in the 1860s the football games
created by public schoolboys were transplanted from these elite
foundations, rapidly becoming the sports of the masses. But has
this history ever been challenged or explored? Football, The First
Hundred Years, provides a revisionist history of the game,
challenging previously widely-accepted belief. The book argues that
established football histories do not correspond with the facts.
Football, as played by the 'masses' previous to the public school
codes is almost always portrayed as wild and quite barbaric but
Harvey shows evidence suggesting this view to be a serious
over-simplification. Football's First One Hundred Years provides a
very detailed picture of the football played outside the confines
of the public schools, revealing a culture that was every bit as
sophisticated as that found within their prestigious walls. Indeed,
the administrative body created by public schoolboys, the FA,
rapidly collapsed and by 1867, it was the intervention of working
class representatives from Sheffield who saved soccer. offering a
different perspective on almost every aspect of the established
history of the formative years of the game. The book will be of
great interest to sports historians and football enthusiasts alike.
The story of the creation of Britain's national game has often been
told. According to the accepted wisdom, the refined football games
created by English public schools in the 1860s subsequently became
the sports of the masses. Football, The First Hundred Years,
provides a revisionist history of the game, challenging previously
widely-accepted beliefs. Harvey argues that established football
history does not correspond with the facts. Football, as played by
the 'masses' prior to the adoption of the public school codes is
almost always portrayed as wild and barbaric. This view may require
considerable modification in the light of Harvey's research.
Football's First One Hundred Years provides a very detailed picture
of the football played outside the confines of the public schools,
revealing a culture that was every bit as sophisticated and
influential as that found within their prestigious walls. Football,
The First Hundred Years sets forth a completely revisionist thesis,
offering a different perspective on almost every aspect of the
established history of the formative years of the game. The book
will be of great interest to sports historians and football
enthusiasts alike.
The Howgill Fells in Cumbria, represent one of the most erosionally
active landscapes in Britain. The bedrock geology, folded Silurian
mudstones, is not especially well seen. The direct effects of
Pleistocene glaciation are limited and not as well developed as in
the neighbouring Lake District, although glacial meltwaters did
have an important impact. However, it is in its post-glacial
landscape that the Howgills are exceptional. The steep hillslopes
of the headwater valleys are riddled by networks of erosional
gullies, many active during the last few thousand years but now
stabilised, others actively erosional now. The gully systems feed
sediment downslope, locally forming large tributary-junction
alluvial fans, elsewhere creating braided reaches within the stream
channels.The Holocene sequence of hillslope gully erosion, alluvial
fan deposition, and stream terrace aggradation and dissection is
exceptionally well exhibited by numerous exposed sections through
the sedimentary sequences. The modern active gully systems have
been monitored for more than thirty years. The results of this
long-term study illustrate two fundamental aspects of process
geomorphology: first, the importance of coupling, i.e. linkages,
within the geomorphic system, and secondly, the significance of
magnitude/frequency relationships. Essentially, the Howgills form
an excellent field laboratory for the study of modern processes and
landforms as well as retaining the evidence for reconstructing the
erosion/deposition sequence of the last few thousand years.The book
is organised in two sections. A series of thematic chapters is
followed by chapters dealing with details of recommended field
excursions. The first excursion is a car-based excursion around the
margins of the Howgills but the other excursions are all hiking
excursions into the interior of the Howgills. One of the joys of
the interior of the Howgills is that they form an upland block,
within which there is no settlement, there are no roads and
virtually no walls. You have to hike in to see, study and learn!The
book is copiously illustrated by maps, diagrams and colour
photographs.
Inverness, known as the capital of the Highlands, was designated a
Millennium city in 2000. This Royal and Ancient Burgh is recorded
going back thousands of years, but it doesn't look like an old town
because it was sacked and burned so many times that little remains
of its long history. There are exceptions, including a house which
dates from 1592 and Dunbar's Hospital of 1688. Also nearby is the
site of the Battle of Culloden, the last battle fought on British
soil. Situated at the head of the Moray Firth and the mouth of the
Great Glen, Inverness is a terminus and starting point for travel
and traffic, living up to its other nickname as the Hub of the
Highlands. In the words of Neil M. Gunn: 'No one can say he has
seen Scotland who has not seen the Highlands, and no one can say he
has been to the Highlands who has not stopped to sample its spirit
in Inverness.'
Geomorphology is the study of the earth's landforms and the
processes that made the landscape look the way it does today. What
we see when we look at a scenic view is the result of the interplay
of the forces that shape the earth's surface. These operate on many
different timescales and involve geological as well as climatic
forces. Adrian Harvey introduces the varying geomorphological
forces and differing timescales which thus combine: from the
global, which shape continents and mountain ranges; through the
regional, producing hills and river basins; to the local, forming
beaches, glaciers and slopes; to those micro scale forces which
weather rock faces and produce sediment. Finally, he considers the
effect that humans have had on the world's topography.
Almeria exhibits superb structural geology (especially the fault
system), a complete Neogene sedimentary sequence (itself rare)
involving an enormous range of sedimentary environments, and
classic dryland geomorphology. Exposure of the sedimentary
sequences is excellent. The area is spectacular and the landform
assemblage includes a wide range of erosional and depositional
landscapes. Furthermore, the region enables linkages to be made
between the several disciplines of geodynamics. The Neogene
sequence cannot be interpreted without considering the evolving
tectonics nor the contemporaneous geomorphology. Neither may the
geomorphology be understood without considering the modern
landscape as a development from the Neogene tectonic and
sedimentary sequences. This guide is an essential companion to
geologists and physical geographers visiting this province in SE
Spain to view its range of unique features, made famous as a
spectacular location for a host of popular films. GPS coordinates
are provided for the locations discussed.
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