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Road log

By
F. Molnár
F. Molnár
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J. Lexa
J. Lexa
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I. Gatter
I. Gatter
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Published:
January 01, 1999

Abstract

km 0 The first Shell gas station on the M3 motorway after the end of Budapest sign. From here, the M3 motorway crosses the Gödöllő Hills during the next 35–40 kilometers. This area consists of a 2 km thick Tertiary-Quaternary sedimentary sequence underlain by Mesosoic carbonate rocks. On the present surface, loess from the Pleistocene glaciation and drift sand deposits are the most common sediments.

60 On the left side ahead the first view of the Western Mátra Mtns. appears. They are the highest mountains of Hungary with 1014 m elevation at the Kékes summit. The visible part of the Western Mátra Mts. is composed of Miocene andesitic-rhyolitic rocks forming a caldera structure with approximately 15 km diameter. The Mátra Mtns. is the object of the field programme on the fourth day and details of regional geology can be found in the guidebook. In front of the mountains the town of Gyöngyős can also be seen.

69 The M3 motorway crosses one of the traditional wine-producing area of Hungary. The vineyards covering 28 000 acres on the southern foreland of the Mátra Mts. are famous for various white vines. The center of the wine region is Gyöngyős.

Behind the vineyards to the left (north) the Eastern Mátra Mtns. can be seen. This part of the Matra Mtns. is built up by andesitic rocks of Miocene age. In contrast to the Western Matra Mts., large caldera structures cannot be found here and the area is very poor in hydrothermal mineralisation.

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Contents

Society of Economic Geologists Guidebook Series

Epithermal Mineralization of the Western Carpathians

Ferenc Molnár
Ferenc Molnár
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Jaroslav Lexa
Jaroslav Lexa
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Jeffrey W. Hedenquist
Jeffrey W. Hedenquist
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Society of Economic Geologists
Volume
31
ISBN electronic:
9781934969847
Publication date:
January 01, 1999

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