Reading the Irish LandscapeThis is the third revision of this seminal work. Co-authored by original author Frank Mitchell and now Michael Ryan, the result is a stunning collaboration between masters giving all the elements of the original book, modified, updated and further enhanced by the inclusion of a new narrative of Irish archaeology from the Stone Age to the Norman Invasion. Together they have successfully undertaken the daunting task of giving in one book the story of the shaping of the land from the beginning of time until now, by all tbe varying forces of nature, sea, climate, man and machine. The story takes in the shaping of the crust, the movement of glaciers, the first men and their primitive agriculture, their buildings and their effect on the forests, the growth of bogs, new migrations, the rise of the monasteries of the Early Christians and the castles of conquest, the devastation of war, urban growth, modern agriculture and afforestation, all set against the backdrop of the landscape, arguably one Ireland's most precious resources. |
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Page 37
... cold / warm Marine Oxygen Isotope Stages ( here abbreviated to MS ) have been recognised in the oceanic record ; these have been numbered , counting downwards from the top . In each stage , a short cold phase is followed by a longer ...
... cold / warm Marine Oxygen Isotope Stages ( here abbreviated to MS ) have been recognised in the oceanic record ; these have been numbered , counting downwards from the top . In each stage , a short cold phase is followed by a longer ...
Page 71
... cold conditions . Cold is clearly indicated by the presence of leaves of the least willow ( Salix herbacea ) , abundant in northern latitudes but surviving only on mountain tops in Ireland , and the dwarf birch ( Betula nana ) , also a ...
... cold conditions . Cold is clearly indicated by the presence of leaves of the least willow ( Salix herbacea ) , abundant in northern latitudes but surviving only on mountain tops in Ireland , and the dwarf birch ( Betula nana ) , also a ...
Page 93
... cold . Radiocarbon dating has shown that the cold spell began about 10,600 years ago and that it ended about 10,000 years ago ; it therefore had a duration of not more than 600 years . The North Atlantic Ocean , which by about 13,000 ...
... cold . Radiocarbon dating has shown that the cold spell began about 10,600 years ago and that it ended about 10,000 years ago ; it therefore had a duration of not more than 600 years . The North Atlantic Ocean , which by about 13,000 ...
Contents
The Ice Age 1700000 to 13000 years ago 335 | 35 |
The End of the Ice Age | 81 |
Response to Warm Conditions 98 886 | 98 |
Copyright | |
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agricultural animals Antrim basin blanket bog bones Britain Bronze Age built burial cattle centre century clay clearance climate coast Cork court tombs crannog debris deposits ditch Donegal drumlins Dublin Earlier Bronze Age Early Medieval enclosure Europe evidence excavated farmers farming flint forest fossils giant deer glacial grassland gravel ground hazel houses Illus important Ireland Irish Sea Iron Age Island Kerry Knowth lake land landscape Later Bronze Age layer limestone Littletonian Lough material Mayo Meath megalithic megalithic tombs Mesolithic Midlandian million years ago monasteries monuments mound Mount Sandel Mountains Neolithic Newgrange passage tomb peat period phase plants pollen portal tomb pottery probably produced Radiocarbon dating raised bog rath record ridge river rock sea level settlement Shannon slope soil stone suggests surface survived temperature trees uplands valley vegetation warm stage wedge tombs Wicklow wood woodland