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Helsingin seudun taajamakartoitus - Arkisto.gsf.fi - Geologian ...

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GEOLOGICAL SURVEY OF FINLAND<br />

DOCUMENTATION PAGE<br />

Date / Rec. no.<br />

Authors<br />

Marit Wennerström, Meri-Liisa Airo, Tuija Elminen,<br />

Sari Grönholm, Matti Pajunen, Markus Vaarma, Pekka<br />

Wasenius<br />

Type of report<br />

Archival document, Final report<br />

Commessioned by<br />

Geological Survey of Finland<br />

Title of report<br />

<strong>Helsingin</strong> <strong>seudun</strong> taajamageologia (Urban geological mapping in the Helsinki Region)<br />

Abstract<br />

In the project rock types and tectonic and structural properties were mapped in the areas of Sipoo, Kerava, Järvenpää,<br />

Tuusula, Nurmijärvi, Hyvinkää and Kirkkonummi. Knowledge in the evolution of the Svecofennian bedrock<br />

is very important for the activities utilizing the bedrock. Tectonic, magmatic and metamorphic evolution has determined<br />

the recent distribution of the rock types, its structural anisotropy and the factors determining the distribution<br />

and characters of the brittle structures. These are important for all kind of bedrock applications. The principal<br />

characters of the evolution of the Svecofennian bedrock are presented for the analysis of applications.<br />

The regional geophysical data were used for de<strong>fi</strong>ning geophysically different sub-areas and in the interpretation of<br />

the structures of bedrock.<br />

The faults that pierce the bedrock in the area were classi<strong>fi</strong>ed according to their origin. Groups with different properties<br />

that also contribute the recent quality of the rock were distinguished. The fault structures were also divided<br />

into three different classes of zones of weakness, which give estimate on the rock quality for engineering purposes.<br />

Based on jointing properties bedrock has been fractured around zones of weakness, borders between major tectonic<br />

units and in the hinge areas of the reoriented gneisses. Generally bedrock is relatively unbroken all over the<br />

mapping area except along the zones of weakness.<br />

Volcanic rocks and quartzites in Hyvinkää are sources of high quality aggregates. Bedrock areas in the other<br />

places of the study area contain mainly raw materials for poor quality aggregate (quality classes II – III, TVH<br />

1988). Gabbros and quartzites from Hyvinkää and the Obbnäs rapakivi granite from Kirkkonummi have been used<br />

as natural stones. In this report 9 aggregate quarrys and 3 already closed natural stone quarrys are described.<br />

Different themes: lithology, tectonic structures, faults, zones of weakness and fracturing of sub-areas are presented<br />

at maps in the scale 1:250 000. Information on aggregates and natural stones are presented with relation to the<br />

Counties.<br />

Keywords<br />

bedrock, deformation, structural analysis, faults, shear zones, joints, rock aggregates, dimensional stones, geophysical<br />

methods, urban geology<br />

Geographical area<br />

Finland, Southern Finland Province, Uusimaa, Hyvinkää, Järvenpää, Kerava, Kirkkonummi, Nurmijärvi, Tuusula,<br />

Sipoo<br />

Map sheet<br />

2031, 2032, 2034, 2041, 2042, 2043, 2044<br />

Report serial<br />

Urban geology<br />

Total pages<br />

94<br />

Language<br />

Finnish<br />

Unit and section<br />

Southern Finland Unit, Bedrock & Mineral Resources<br />

Signature/name<br />

Archive code<br />

K 21.42/2006/6<br />

Price<br />

Project code<br />

2704000<br />

Signature/name<br />

Con<strong>fi</strong>dentiality<br />

Public

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