Jökull


Jökull - 01.06.2000, Page 8

Jökull - 01.06.2000, Page 8
Eysteinn Tryggvason Figure 3. Observed ground tilt at two optical levelling tilt stations, Kötlukriki and Jökulkvísl, near the eastern extremities of the glacier Mýrdalsjökull. Error bars show one standard error of tilt computed for the period from íirst observation to each succeeding observation. Horizontal scale is time from beginning of the year 1965 to end of the year 1995. Vertical scale is either east- or north-component of ground tilt in microradians, positive if uplift is towards east or north. - Mœldar hallabreytingar við austurjaðar Mýrdalsjökuls, í Kötlukrika og við Jökulkvísl. Fyrsta mœling var gerð árið 1967. Lóðrétti ásinn sýnir hallabreytingu til austurs (efri hlutinn) og norðurs (neðri hlutinn) á árunum 1967-1995. field is about 15 cm, and that the thickness of the el- astic lithosphere is 5 to 10 km. Suggested tilt up towards west or north-west at the station Kötlukriki between 1967-1973 and 1986-1995 (Figure 3) is possibly the result of less average glacier load during the latter period. CONCLUSIONS Observations of ground tilt at the edge of the Mýr- dalsjökull glacier from 1967 to 1995 suggest that annual variations in the glacier load causes measura- ble ground tilt. There is no clear evidence that sub- surface magma movement at Katla has caused any ground deformation during this period. There is a vague indication of secular tilt, up towards west or north-west, at the station Kötluki'iki, and observati- ons at the station Jökulkvísl do not contradict such secular tilt. The suggested tilt rate is 0.1 /rrad per year at Kötlukriki, and less at Jökulkvísl. This tilt rate is too small to be observed with confidence and can be caused by less average glacier load during the observations of 1986-1994 than during the observati- ons of 1967-1973. Considering the rate of secular tilt of 0.1 /irad per year at Kötlukriki to be real, and assuming that this tilt is caused by increase of pressure in a magma cham- ber at 5 km depth below Katla, then a ground uplift of about 0.6 mm per year is suggested. To cause this much uplift, about one million cubic meters of magma 6 JÖKULL No. 48

x

Jökull

Direct Links

If you want to link to this newspaper/magazine, please use these links:

Link to this newspaper/magazine: Jökull
https://timarit.is/publication/1155

Link to this issue:

Link to this page:

Link to this article:

Please do not link directly to images or PDFs on Timarit.is as such URLs may change without warning. Please use the URLs provided above for linking to the website.