■15 



Station 125. N. B. 67° 52', 0. L. 5° 12'. 700 

 Fvn. (12.su M.). -1.1°. Brunt Overgangsler. Nogle 

 Stene. 



Station 126. X. B. 67° 49', 0. L. 5» 33'. 730 

 Fvn. (1335 M.). — 1.1". Brunt Overgangsler uden Bilo- 

 culiner og < rlobigeriner. 



Station 127. N. B. 67° 47', 0. L. 5° 54'. Tlf» 

 Fvn. (1308 M.). 1.1". Brunt Overgangsler. IngeD 



Biloculiner eller Globigerineri Ingen Stene. 



Station 125. - Lat. 67° 52' \.. long. 5° 12' E.; d. 

 700 fms. (1280 m.); b.-t. -- 1.1". A brown transition clay 

 containing a few pebbles. 



Station 126. - Lat. (37" 49' X., long. 5° 33' E.; d. 

 730 fms. (1335 m.); b.-t. — 1.1". A brown transition clay 

 without either Biloculinæ or Globigerinæ. 



Station 127. - Lat, 67" 47' X., long, 5" 54' E.; d. 

 715 fms. (1308 m.); b.-t. 1.1". A brown transi- 



tion clay without either Biloculinæ or Globigerinæ. No 

 pebbles. 



Station 128. N. B. 67° 43', 0. L. (i" 21'. 688 

 Fvn. (1258 Ml 1.2°. Biloculinler, noget uensartet i 



Farven, limen Stene. 



Station 129. N. B. 67° 40', 0. L. 6° 42'. 709 

 Fvn. (1296 M.). -1.2". Blanding af Biloculinler og 

 niere graaligt Ler. I Leivt opdagedes blot Globigeriner, 

 ingen Biloculiner 1 . Nogle Stene (veiende indtil 0.2 Gr.), 

 bestaaende af Kvarts. Kvartsit, Glimmerskifer, Sandsten (?). 



Station 128. -- Lat. 67° 43' X., long. 6° 21' E.; d. 

 688 fms. (1258 m.); b.-t. —1.2". Biloculina clay, differ- 

 ing sligbtly in colour. No pebbles. 



Station 129. - Lat. 67" 40' X., long. ti" 42' E.: d. 

 709 fms. (1296 ni.); b.-t. -- 12". A mixture of Biloculina 

 clay and a clay of a greyer tint containing Gldbigerinæ (no 

 Biloculinæ could be detected 1 ) and a few pebbles (the 

 lårgest weighing 0.2"") of quartz, quartzite, mica schist, 

 sandstone (?). 



Station 130. N. B. 67" 38". 0. L. 7" 3'. 689 Fvn. 

 (1260 M.). -1.1°. Bundproven mangler; i Loddejour- 



nalen er blot noteret: Ler. 



Station 131. N. B. 67" 35', 0. L. 7" 26'. 795 Fvn. 

 (1454 M.). — 1.2". Blanding af brunt, lysgraat og mørk- 

 graat Ler. Ingen Biloculiner eller Globigeriner. Ingen 

 Stene. 



Station 132. X. B. 67" 33'. 0. L. 7" 48'. 954 Fvn. 

 (1745 M.). — 1.2". To Lag i Bundproven. Øverst "brunt 

 Overgangsler, underst graat Ler. 



Station 133. N.B. 67" 30', 0. L. 8° 10'. 890 Fvn. 

 ( ! 628 M.). — 1.3". Brunt Overgangsler med noget mørk- 

 brunt Ler. En liden Sten: Kvarts. 



Station 134. N. B. 67° 29', 0. L. 8° 20'. 878 Fvn. 

 (1606 M ). — 1.2". Uensartet, graat, grovkornigt Ler. 

 Mange Stene (veiende indtil 6.5 Or.), bestaaende af Kvarts. 

 Feldspath (?). krystallinske' Skifere. Granit. 



Station 130. - Lat. 67" 38' N., long. 7" 3' E.: d. 

 689 fms. (1260 m.): b.-t. --1.1°. No sample from this 

 Station. The entry in the sounding-journal is simply "clay." 



Station 131. -- Lat, 67" 35' X., long. 7" 26' E.; d 

 795 fms. (1454 in.); b-t. --1.2°. A mixture of brown, 

 light-grey, and dark-grey clay. No Biloculinæ or Gldbige- 

 rinæ; and no pebbles. 



Station 132. — Lat. 67" 33' X., long. 7" 48' E.: d. 

 954 fms. (1745 in.): b.-t. — 1.2". Two lavers in this sam- 

 ple: the upper a brown transition. the under a grey clay. 



Station 133. -- Lat. 67" 30' X., long. 8" 10' E. ; 

 d. 890 fms. (1628 m.); b.-t. -- 1.3". A brown transition 

 clay. along with a little dark-brown clay. containing a small 

 fragment of quartz. 



Station 134. - Lat, 67 1 ' 29' X., long. 8" 20' E.: d. 

 878 fms. (16(16 m.); b.-t. -1.2». A grey, coarse clay 

 containing many pebbles (the largest weighing 0.5"') of 

 quartz. feldspat (?). crystalline schists, granite. 



Station 135. X.B. 67" 27'. 0. L. 8" 31'. 860 Fvn. 

 (1573 M.). -1.2". Brunt Overgangsler. Nogle Globige- 

 riner kunde opdages. Ingen Stene. 



Station 136. X.B. 67" 25', 0. L. 8° 47'. 610Fvn. 



Station 135. - Lat, 67" 27' N., long. 8" 31' E.; d. 

 860 fins. (1573 ni.): b.-t. — 1.2". A brown transitiou 

 clay in which a few Globigerinæ could be detected. No 

 pebbles. 



Station 136. 



Lat. 67° 25' N., lon- 8" 47' E.; 



Sml. Stat. 96. 



Sr,. Stat. !)H 



