Learning about Learning in Ice Age France through Stone Tools

2018 ◽  
pp. 227-234
Author(s):  
Kathleen Sterling
Keyword(s):  
2021 ◽  
pp. 186-222
Author(s):  
Clive Gamble

By the end of the decade the time revolution was a done deal. Moulin-Quignon still reverberated, but in 1865 Lubbock produced the first guided tour of the Old Stone Age, in which he accused Lyell of plagiarism. In Pre-Historic Times he filled the new space of deep history with stone tools to show an evolutionary pathway from St Acheul to the Neolithic monuments of Avebury and Stonehenge. Tracing history back was matched by the anthropologist Edward Tylor, who traced it up. Both men were interested in the evolution of racial groups and accounting for the world’s hunters and gatherers. In a typically upbeat assessment, Lubbock saw the lesson of the past as providing hope for the future. Victorian ‘savages’ at the uttermost ends of the earth had not degenerated from a civilized state. They had the potential to evolve, as his ancestors in Europe had done. Unwritten history was making universal history possible. The decade saw deaths and career changes. Prestwich largely abandoned the time revolution, married Falconer’s niece, Grace McCall, and became an Oxford professor. Falconer and Boucher de Perthes died, while Lubbock entered Parliament in 1870. Prestwich’s fixed notion of a single ice age was challenged by James Croll, who painstakingly worked out the changes in the elliptical orbit of the Earth, and from these proposed multiple ice ages. As a bookend to the decade Evans published his fact-rich volume on ancient stone implements. The path of deep history was now set in stone.


Author(s):  
Frank F. Schambach

I am pleased and very honored that you have invited me here today to tell you something about the past of the Caddo people as it is known to archaeologists. This is a subject that has been both my occupation and my major preoccupation for more than 25 years. The story that I and other archaeologists have been piecing together over many years is long, complex, and endlessly fascinating. It is a heritage that anyone could be proud of. Let me give you some of the highlights. The story began over 11,500 years ago--or about 9,500 B.C.--when the first people arrived in the historic Caddo territory of Northwest Louisiana, Southwest Arkansas, East Texas, and Southeast Oklahoma. There were not many of them, perhaps only a hundred or so in this whole area at first. And the world they lived in was very different from the world today. It was cold, about like northern Maine or northern Michigan today, with forests of spruce and birch, because the Ice Age was still going on. They were probably dressed like Eskimos in carefully sewn parkas, trousers, and boots. We know this because many of the stone tools they left behind are tools for preparing hides and for making the bone needles necessary to sew them into clothing. They probably lived in skin tepees like those of the historic Plains Indians, but smaller, because they did not have horses to carry their gear from place to place. They did have dogs and they probably trained them to work as pack animals.


2021 ◽  
pp. 41-81
Author(s):  
Clive Gamble
Keyword(s):  
Ice Age ◽  

The narrative starts at breakfast in the northern French town of Abbeville on the River Somme. Prestwich and Evans are joined by the pioneering, but eccentric antiquary Jacques Boucher de Perthes. They are here to inspect his claims for stone tools found alongside the bones of extinct ice age animals. If they can verify his claim, then the time revolution has begun. The reasons why Boucher de Perthes has been ignored are touched on as the three visit the gravel pits of the town, looking at the evidence. Lunch allows them to study Boucher de Perthes’s huge collection of flints and antiquities, including his strange stone sculptures. They are interrupted by a telegram and leave for Amiens. The train journey from Abbeville to Amiens is used to reflect on how they built their scientific case from facts, not theories. Once in Amiens they are taken by Charles Pinsard to the gravel pits at St Acheul, where they find, and photograph, the evidence they came for. The circumstances of the discovery are described in their own words.


Author(s):  
Anne O'Connor

The acceptance of human antiquity in the mid-nineteenth century fed a desire to know more about the age of these chipped stone tools from the drift. In 1863, Canon William Greenwell (1820–1918), the antiquary, archaeologist, and collector from Durham, declared: ‘The great question which has yet to be settled is this—at what period was the drift in which the flints are found deposited? And side by side with this was another important query—down to what time did these now extinct animals occupy any part of our continent?’ This chapter seeks to untangle the web of time that was spun around the stone implements of Britain over the last four decades of the nineteenth century. Greenwell’s great question was a popular one, and ‘what period’ was often answered by connecting the implementiferous drifts to the Glacial epoch. The mid-glacial submergence, entertained by geologists like Ramsay and Phillips, provided a convenient division between pre-glacial and post-glacial times. On each side of this great division, detailed patterns were being drawn in stratigraphy and bones. As decisions were made about the pre-glacial or post-glacial date of sediments from river drifts and caves, rich in tools and bones, the glacial chronology was, meanwhile, being revised and subdivided too. During the latter decades of the nineteenth century there was great activity and little agreement about the order of events in these distant times. Researchers immersed in different material, gathered from different geographical areas, and asking different questions would not find it easy—or even desirable—to mesh their findings into a single coherent sequence. Attempts to date the stone tools of Britain entered a contentious arena. The chronological indicators scrutinised by these researchers—river drifts, glacial drifts, and bones—offered few clear answers to Greenwell’s question. The sands, gravels, clays, and brickearths of Quaternary times were so scattered, patchy, and variable that even Prestwich found it diffcult to understand their sequence.


Nature ◽  
2005 ◽  
Author(s):  
Mark Peplow
Keyword(s):  

Author(s):  
W.P. De Lange

The Greenhouse Effect acts to slow the escape of infrared radiation to space, and hence warms the atmosphere. The oceans derive almost all of their thermal energy from the sun, and none from infrared radiation in the atmosphere. The thermal energy stored by the oceans is transported globally and released after a range of different time periods. The release of thermal energy from the oceans modifies the behaviour of atmospheric circulation, and hence varies climate. Based on ocean behaviour, New Zealand can expect weather patterns similar to those from 1890-1922 and another Little Ice Age may develop this century.


Sign in / Sign up

Export Citation Format

Share Document