Studies in the Palaeolithic Succession in England, No. III: Palaeoliths from St. Neots, Huntingdonshire
Palaeolithic artifacts were recorded from a terrace on the Great Ouse, near St. Neots, Huntingdonshire, in 1927, the chief source being a group of pits dug in what was formerly part of Paxton Park, on the left bank of the river in the parish of Little Paxton. Mr Tebbutt has since recovered many more...
Published in: | Proceedings of the Prehistoric Society |
---|---|
Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
1947
|
Subjects: | |
Online Access: | http://dx.doi.org/10.1017/s0079497x00019617 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0079497X00019617 |
id |
crcambridgeupr:10.1017/s0079497x00019617 |
---|---|
record_format |
openpolar |
spelling |
crcambridgeupr:10.1017/s0079497x00019617 2024-03-03T08:48:24+00:00 Studies in the Palaeolithic Succession in England, No. III: Palaeoliths from St. Neots, Huntingdonshire Paterson, T. T. Tebbutt, C. F. 1947 http://dx.doi.org/10.1017/s0079497x00019617 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0079497X00019617 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Proceedings of the Prehistoric Society volume 13, page 37-46 ISSN 0079-497X 2050-2729 General Medicine journal-article 1947 crcambridgeupr https://doi.org/10.1017/s0079497x00019617 2024-02-08T08:42:58Z Palaeolithic artifacts were recorded from a terrace on the Great Ouse, near St. Neots, Huntingdonshire, in 1927, the chief source being a group of pits dug in what was formerly part of Paxton Park, on the left bank of the river in the parish of Little Paxton. Mr Tebbutt has since recovered many more artifacts from this site. Taken together, the material constitutes a working industry, which will be described in this paper. A twelve-foot section, fig. 1, shows a basal layer (1) of boulders and large pebbles resting upon undisturbed Oxford Clay. One boulder of limestone measured two feet in length, and many other erratics showed the derivation of this layer from drift deposits of a preceding glacial stage. Bones and teeth of Elephas primigenius, Rhinoceros antiquitatis, Rangifer tarandus , and Equus caballus were found here. This basal bed is not a solifluxion level in place, though it may represent a solifluxion layer which has been re-washed and sorted. Certainly the Oxford Clay has not been caught up into it, and the elements are uniformly water-laid, passing up, without break, into nine feet of compact, well-bedded, fluviatile gravels. Article in Journal/Newspaper Rangifer tarandus Cambridge University Press Proceedings of the Prehistoric Society 13 37 46 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
General Medicine |
spellingShingle |
General Medicine Paterson, T. T. Tebbutt, C. F. Studies in the Palaeolithic Succession in England, No. III: Palaeoliths from St. Neots, Huntingdonshire |
topic_facet |
General Medicine |
description |
Palaeolithic artifacts were recorded from a terrace on the Great Ouse, near St. Neots, Huntingdonshire, in 1927, the chief source being a group of pits dug in what was formerly part of Paxton Park, on the left bank of the river in the parish of Little Paxton. Mr Tebbutt has since recovered many more artifacts from this site. Taken together, the material constitutes a working industry, which will be described in this paper. A twelve-foot section, fig. 1, shows a basal layer (1) of boulders and large pebbles resting upon undisturbed Oxford Clay. One boulder of limestone measured two feet in length, and many other erratics showed the derivation of this layer from drift deposits of a preceding glacial stage. Bones and teeth of Elephas primigenius, Rhinoceros antiquitatis, Rangifer tarandus , and Equus caballus were found here. This basal bed is not a solifluxion level in place, though it may represent a solifluxion layer which has been re-washed and sorted. Certainly the Oxford Clay has not been caught up into it, and the elements are uniformly water-laid, passing up, without break, into nine feet of compact, well-bedded, fluviatile gravels. |
format |
Article in Journal/Newspaper |
author |
Paterson, T. T. Tebbutt, C. F. |
author_facet |
Paterson, T. T. Tebbutt, C. F. |
author_sort |
Paterson, T. T. |
title |
Studies in the Palaeolithic Succession in England, No. III: Palaeoliths from St. Neots, Huntingdonshire |
title_short |
Studies in the Palaeolithic Succession in England, No. III: Palaeoliths from St. Neots, Huntingdonshire |
title_full |
Studies in the Palaeolithic Succession in England, No. III: Palaeoliths from St. Neots, Huntingdonshire |
title_fullStr |
Studies in the Palaeolithic Succession in England, No. III: Palaeoliths from St. Neots, Huntingdonshire |
title_full_unstemmed |
Studies in the Palaeolithic Succession in England, No. III: Palaeoliths from St. Neots, Huntingdonshire |
title_sort |
studies in the palaeolithic succession in england, no. iii: palaeoliths from st. neots, huntingdonshire |
publisher |
Cambridge University Press (CUP) |
publishDate |
1947 |
url |
http://dx.doi.org/10.1017/s0079497x00019617 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0079497X00019617 |
genre |
Rangifer tarandus |
genre_facet |
Rangifer tarandus |
op_source |
Proceedings of the Prehistoric Society volume 13, page 37-46 ISSN 0079-497X 2050-2729 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0079497x00019617 |
container_title |
Proceedings of the Prehistoric Society |
container_volume |
13 |
container_start_page |
37 |
op_container_end_page |
46 |
_version_ |
1792505275407663104 |