119 



like, with /> {oio} and f[\Ol] about equally developed. The 

 crystals are semi-trans[iarent and of a greyish colour. 

 Gaa se fjord in Scoresby Sund. 



1) The south coast. A few small amygdaloids were found here 

 isolated from their surrounding rock. The interior was al- 

 most completely filled with stilbite, so that crystals faces 

 (б(010}, f{00l}, Ш {ito}) were only found in a few places. 

 The length of the crystals was about I cm. ; they were 

 cloudy and of a greyish colour. 



A few loose fragments of basalt were also found here, 

 which contained almost exclusively chabazite. One fragment, 

 however, had a few stilbite crystals developed on the cha- 

 bazite crystals. The stilbite crystals are of the same form 

 and size as those mentioned above and are also very irre- 

 gularly developed. 



In addition to these, a pale grey dolerlte rock had some 

 of its cavities filled with levynite, but others contained both 

 levynite and small (1 — 2^^) stilbite crystals, or, in some 

 cases, stilbite crystals only. The form of the crystals differs 

 from the ordinary one, as è{010}, c'{00l} and /"{loij pre- 

 dominate and m{llo} is only seen as small faces at the 

 corners. The crystals are clear and transparent, with 

 irregular curved faces. 



2) Gaaseland. In a single block obtained from a moraine and 

 perhaps of identical origin with the specimens mentioned 

 above, a few cavities were found containing, in addition to 

 chabazite, small stilbite crystals of the ordinary form. The 

 crystals are small, semi-transparent and colourless. Most 

 of the cavities in the rock were filled exclusively with 

 chabazite. 



Sabine Ö. Stilbite was found here only as a single 

 small fragment. It seems to be partly columnar and partly in 

 the form of small sheaf-like crystals (1—3"™). of the combi- 



