De ijstijden Guide to 1960 exhibition

THE ICE AGE IN EUROPE especially in the Netherlands In the entrance hall a map (fig. 4) shows the largest extent of the glaciation in Europe. A model of a glacier suggests how the stones and hills shown on the photographs were transported or modelled by the ice. A stone and a buffalo\xe2\x80\x99s sk...

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Main Author: NN
Format: Article in Journal/Newspaper
Language:unknown
Published: 1960
Subjects:
Eik
Online Access:https://repository.naturalis.nl/pub/505162
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record_format openpolar
spelling ftnaturalis:oai:repository.naturalis.nl:505162 2024-02-11T10:05:52+01:00 De ijstijden Guide to 1960 exhibition NN 1960-01-01 application/pdf https://repository.naturalis.nl/pub/505162 unknown https://repository.naturalis.nl/pub/505162 Beaufortia vol. 8 no. 90, pp. 93-107 info:eu-repo/semantics/article 1960 ftnaturalis 2024-01-17T23:25:45Z THE ICE AGE IN EUROPE especially in the Netherlands In the entrance hall a map (fig. 4) shows the largest extent of the glaciation in Europe. A model of a glacier suggests how the stones and hills shown on the photographs were transported or modelled by the ice. A stone and a buffalo\xe2\x80\x99s skull have even been found deep in the soil where Amsterdam now stands. An enormous bear tells us of the animals that once braved the cold.\nIn the first room (left of entrance hall) the tropical or subtropical life, before the Ice Age, is shown. Of the four glacial periods distinguished by the palaeontologists the first did not influence our climate. We see the animals then living here: the largest known elephant, Archidiscodon meridionalis, (fig. 2, shoulder 5 m. high), rhino, tapir, hippo, sabletoothtiger (fig. 3), hyaena, antelopes, porcupine, beavers, deer and a monkey. Many of their remains are disclosed by the water from the bottom of the Zeeland Sea-arms, others are found in the clay-pits at Tegelen, known for their pottery clay ever since Roman times. Both are sedimentations of the rivers of the first interglacial period. The plant remains are shown in a pollen diagram: the cork epidermis of the pollen is preserved in the layers deposited at a certain time (a picture shows some pollen grains highly enlarged). The diagram covering a depth of about 5 m shows the changing climate: willow (wilg) and birch (berk) belong to colder times, oak (eik) and hazel (hazelaar) point to a milder climate.\nThe room to the right of the hall shows the animals that survived here during the cold period. The last glacial period (fig. 4) saw reindeer, musk-ox, glutton, mammoth (fig. 5), woolly rhino, giant deer, bear. Many of them have been pictured by the human inhabitants in their caves, as the reproductions on the exhibition show. The wisent (fig. 6) survived, as probably did the Przewalski horses, and others (boar, elk, deer).\nThe next room shows the animals that inhabited our regions after the Ice age: as said some adapted ... Article in Journal/Newspaper musk ox Naturalis Institutional Repository Eik ENVELOPE(6.668,6.668,62.627,62.627)
institution Open Polar
collection Naturalis Institutional Repository
op_collection_id ftnaturalis
language unknown
description THE ICE AGE IN EUROPE especially in the Netherlands In the entrance hall a map (fig. 4) shows the largest extent of the glaciation in Europe. A model of a glacier suggests how the stones and hills shown on the photographs were transported or modelled by the ice. A stone and a buffalo\xe2\x80\x99s skull have even been found deep in the soil where Amsterdam now stands. An enormous bear tells us of the animals that once braved the cold.\nIn the first room (left of entrance hall) the tropical or subtropical life, before the Ice Age, is shown. Of the four glacial periods distinguished by the palaeontologists the first did not influence our climate. We see the animals then living here: the largest known elephant, Archidiscodon meridionalis, (fig. 2, shoulder 5 m. high), rhino, tapir, hippo, sabletoothtiger (fig. 3), hyaena, antelopes, porcupine, beavers, deer and a monkey. Many of their remains are disclosed by the water from the bottom of the Zeeland Sea-arms, others are found in the clay-pits at Tegelen, known for their pottery clay ever since Roman times. Both are sedimentations of the rivers of the first interglacial period. The plant remains are shown in a pollen diagram: the cork epidermis of the pollen is preserved in the layers deposited at a certain time (a picture shows some pollen grains highly enlarged). The diagram covering a depth of about 5 m shows the changing climate: willow (wilg) and birch (berk) belong to colder times, oak (eik) and hazel (hazelaar) point to a milder climate.\nThe room to the right of the hall shows the animals that survived here during the cold period. The last glacial period (fig. 4) saw reindeer, musk-ox, glutton, mammoth (fig. 5), woolly rhino, giant deer, bear. Many of them have been pictured by the human inhabitants in their caves, as the reproductions on the exhibition show. The wisent (fig. 6) survived, as probably did the Przewalski horses, and others (boar, elk, deer).\nThe next room shows the animals that inhabited our regions after the Ice age: as said some adapted ...
format Article in Journal/Newspaper
author NN
spellingShingle NN
De ijstijden Guide to 1960 exhibition
author_facet NN
author_sort NN
title De ijstijden Guide to 1960 exhibition
title_short De ijstijden Guide to 1960 exhibition
title_full De ijstijden Guide to 1960 exhibition
title_fullStr De ijstijden Guide to 1960 exhibition
title_full_unstemmed De ijstijden Guide to 1960 exhibition
title_sort de ijstijden guide to 1960 exhibition
publishDate 1960
url https://repository.naturalis.nl/pub/505162
long_lat ENVELOPE(6.668,6.668,62.627,62.627)
geographic Eik
geographic_facet Eik
genre musk ox
genre_facet musk ox
op_source Beaufortia vol. 8 no. 90, pp. 93-107
op_relation https://repository.naturalis.nl/pub/505162
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