Results 231 to 240 of about 25,047 (266)
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Palaeoproterozoic accretionary processes in Fennoscandia
Geological Society, London, Special Publications, 2009Abstract Accretionary processes contributed to major continental growth in Fennoscandia during the Palaeoproterozoic, mainly from 2.1 to 1.8 Ga. The composite Svecofennian orogen covers c . 1×10 6 km 2 and comprises the Lapland–Savo, Fennia, Svecobaltic and ...
Raimo Lahtinen +3 more
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Event detectability of seismograph stations in Fennoscandia
Physics of the Earth and Planetary Interiors, 1976Abstract The event detection probability as a function of ISC magnitude shows significant variations between seismic stations in Fennoscandia. In the teleseismic range, the 50% incremental detection thresholds extend from m b = 4.5 to 5.5 among those stations that reported to the ISC during 1964–1969; the best stations being located in Finland ...
Pirhonen, S. +2 more
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Applied Vegetation Science, 2019
Aims: Present-day large-scale and plot-based vegetation analyses contribute to the transnational characterization and interpretation of biodiversity patterns and to habitat typologies, which are important for planning, monitoring and decision making in ...
Ricarda Pätsch +6 more
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Aims: Present-day large-scale and plot-based vegetation analyses contribute to the transnational characterization and interpretation of biodiversity patterns and to habitat typologies, which are important for planning, monitoring and decision making in ...
Ricarda Pätsch +6 more
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Diet overlap among ruminants in Fennoscandia
Oecologia, 2000Information on overlap in resource use is central to understanding of interspecific exploitation competition and resource partitioning. Despite this, measures of diet overlap among northern ruminants in Fennoscandia is limited to one earlier study (reindeer and sheep).
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The Autumnal Moth in Fennoscandia
1988Mountain birch, Betula pubescens Ehrhart ssp. tortuosa (Ledebour) Nyman, forests form the tree line in northwestern Europe and are periodically defoliated by the autumnal moth, Epirrita = Oporinia autumnata (Borkhausen). This chapter analyzes the population dynamics of Epirrita, but many of our conclusions may apply to other defoliators, such as ...
Erkki Haukioja +3 more
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Crustal structures of Eastern Fennoscandia
Tectonophysics, 1991The area of the Eastern Fennoscandian Shield is quite well covered by deep seismic sounding profiles, most of which were shot in the last ten years. In general the velocities of the seismic waves in the crust increase continuously with depth, but intense reflections also indicate the presence of distinct velocity boundaries.
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Surface urban heat islands in 57 cities across different climates in northern Fennoscandia
, 2020V. Miles, I. Esau
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