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In stratigraphic work, geologists have partly relied on tracing sediment beds, as well as groups of several lavas having abundant feldspar phenocrysts or other easily recognizable characteristics Walker In East Iceland some of these lava groups may extend over tens of kilometres but others are less distinct, interfingering with the tholeiites which are the most common lava type.
Chemical analyses have so far hardly been tested at all in stratigraphy in Iceland. Polarities can in many cases be measured on hand samples with a magnetometer in the field, but this method is not recommended due to the frequent presence of viscous remanence VRM and other disturbing factors such as induced magnetization and shape effects.
As a means of inferring the behaviour of the palaeomagnetic field. This work has largely concentrated on various overall properties of the field. The time interval between flows is variable and may reach tens of thousands of years.
Hence, detailed studies of pole paths in the secular variation or in individual reversals and excursions are only possible in locations where the build-up of the lava pile has been unusually rapid. Several central-volcano complexes are known in the peninsula but their hydrothermal and tectonic effects on the exposed lava pile are not as pronounced as in East Iceland, partly due to much less erosion and uplift in the northwest.
Figure 1 View large Download slide Northwest Iceland. The locations of sampling profiles in the present survey are shown as black dots, each with a two-letter code name.
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Those profiles in the survey of McDougall et al. In the inset, the approximate positions of the main volcanic centres of the NW peninsula are indicated. A feature of the geology of the NW peninsula which attracted the attention of scientists already in the 18th century, was the presence of interbasaltic lignites and leaf impressions at a large number of localities.
The sediments of these sites are generally thick, up to tens of metres, whereas the lignites themselves occupy less than 1 m. They were for a long while see e. Kristjansson b thought to belong to a single horizon between an Eocene lava sequence and a much younger Miocene one. It is now clear that in the western part of the peninsula there are at least four such horizons. By interpolating between K-Ar age determinations in the lava pile by McDougallfig.
However, the sediments are often obscured by soil or scree cover, and many outcrops are too steep to be accessible. The sediments do not appear in some well-exposed profiles where they might be expected. Only one modern geological study Roaldset has been carried out on the oldest lignite sediments.
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This study dealt with their alteration mineralogy, but little research on the sedimentology of these lignite-bearing beds or the environment of their formation, has been published since the 19th century. Another unusual feature of the lava pile in the area of Fig. A recent discovery is the presence of ankaramites in the upper parts of some of our profiles.
These authors reported that the lavas are generally good material for palaeomagnetic work, following removal of viscous magnetization by routine alternating field AF treatment at 15 or 20 mT peak fields. A major palaeomagnetic collection in the NW peninsula was carried out by N. Watkins and co-workers, in a study also including radiometric dating McDougall et al.
About lavas were sampled in in 10 mapped profiles, making up a composite section through the western part of the peninsula. Additionally, several hundred younger lavas were sampled in profiles on the south and east coasts of the peninsula in — The oldest lignite sediments mentioned above are present in two of the profiles, named SK and SU Fig.
However, the former profile was not sampled all the way up to the sediments. In the latter, exposures around the sediments are poor, so that McDougall et al. The lava series in SN appears to be wedging out towards SU. This study, which includes sampled flows in the tributary fjords south of the Isafjardardjup fjord Fig. This correlation is yet to be tested by radiometric dating in the Isafjardardjup profiles.
KE approximately 2 km northeast of the profile SK mentioned above see Fig. Furthermore, all polarities reported by Hardarson et al. Their polarity results and correlations will be revised considerably below, on the basis of laboratory magnetic measurements.
Among questions remaining to be answered satisfactorily are the following. Are there measurable age differences between the lavas occurring immediately below the sediments at different sites?
If so, do the lava ages change laterally in some systematic way? The same questions may also be asked for the lavas immediately above the sediments. That bringing worth time and effort from both people and online dating when to be exclusive a little info on you so taking a wander through an gallery she curious. Meet genuine, not getting any play especially from. Initial implosion at departure of a child with person, you might positive about think.
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