Jökull


Jökull - 01.12.1987, Side 64

Jökull - 01.12.1987, Side 64
Fig. 5. Major processes operating in a fjord/bay glacio- marine environment. Compiled and modified from Boulton and Deynoux (1981), Elverhöi (1984), Powell (1984), Eyles et al. (1985), Stevens (1985). 5. mynd. Setmyndun í sjó framan við jökulsporð. Fig. 6. Melabakkar-Ásbakkar glacio- marine lithofacies. (A) Ásbakkar diam- icton at 800 m. Broken line shows con- tact with the overlying Melar diamic- ton. Arrow points at en echelon patterned joints; (B) A body of inter- bedded stratified diamictons and sands, intrabedded in facies Dmu of the Ás- bakkar diamicton at 5000 m; (C) The Látrar beds at 2600 m: transition from planar cross stratified esker fan sedi- ments, over stratified diamicton to in- terbedded laminated silts and sands. The exposure cuts facies Sp parallel to foreset strike. Note the upwards trend towards planar parallel stratification; (D) The Melabakkar silts and sands at 500 m: a transition from glaciomarine silts to sublittoral sands. 6. mynd. Ásýnd jökulsjávarsets í bökk- unum. 62
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Jökull

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