Jökull

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Jökull - 01.12.1977, Qupperneq 69

Jökull - 01.12.1977, Qupperneq 69
h1976 ' h1S75 ícr[l' ip =65ö40' Fig. 3. Height and gravity variations 1976— 1975 along the main gravity profile. Mynd 3. Hœðar- og þyngdarbreytingar eftir aðalmœlilinu 1976—1975. variations, an accumulation of systematic level- ling errors is to be assumed. The gravity increase and height decrease at Námaskard is the effect ot the subsidence at the Krafla area, being very strongly reduced already at a 8 km distance. Frorn the gravity and height change at Námaskard we obtain an average gravity-height factor of —0.1 ... —0.2 mgal/m. This could correspond to the combin- ed effect of the removal of a Bouguer plate and a superposed gravity decrease. 7’he gravity variations 1976—1975/70 found in the regional gravity field between Mývatn and Axarfjördur, are listed in Table 3, figure 4 shows the regional distribution of the varia- tions. These stations are not monumented like those in the main profile and had to be re- stored by point sketches. So the accuracy of the variations is influenced not only by the r.m.s.e. of the gravity measurements at the first (± 0.02 . .. ± 0.03 mgal) and the second (± 0.02 mgal) epoch, but also by remaining identification errors. Taking also local mass displacements in- to account, we estimate the r.m.s.e. of the deter- mined variations at ± 0.05 mgal. At some stat- ions, especially along the road from Námafjall to Krafla, the uncertainty might be greater, of the order of 0.1 mgal or more. Only the ten- dency of remarkable gravity increase should be recognized here. At the monumented Gjástykki- NW-SE-profile, accuracy is higher (± 0.03 . .. 0.04 mgal). From Fig. 4 we see, that gravity variations have a rather local character and occur only in á few areas. There is a strong gravity increase (up to a few tenths of a mgal) from Námafjall to Krafla, confirming the large subsidence of Fig. 4. Gravity stations between Mývatn and Axarfjördur and gravity variations 1976—1965/ 70 (t/ioo mgal). Mynd 4. Þyngdarmœlistöðvar milli Mývatns og Axarfjarðar og þyngdarbreytingar 1976—1965/70 /Vioo mgal). JÖKULL 27. ÁR 67
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