Under 100 Fayne er Temperaturen i samme Vertical 
constant (No. 8) eller svagt aftagende med Dybden. Fra 
Sydvest mod Nordost, fra Havet mod Land, er den gjen- 
nemsnitlige Dyb-Temperatur aftagende. 
Udenfor Folden-Fjorden ligger en Banke, der grunder 
op til 60 Favne Vand. Mellem denne og Kysten strækker 
sig en Dybrende, adskilt fra Foldenfjordens ved en grun- 
dere Ryg. I den første har man fra *Hansteen” taget føl- 
gende Temperaturrækker. 
Jal, No, Ni, 
Juli 9. 
Tel, INO i, 
1880. Juli 21. 1880. 
64° 34’ N. Br. 9° 21’ B. Led. 64° 40’ N. Br. 9° 20’ B. Led. 
Payne. Meter. Temp. Fayne. Meter. Temp. 
(Fins). (Fins). 
(0) fo) 1204 fo) fo) 11°.8 
5 9 12 2 IO 18 IEW gil 
IO 18 IO .2 20 37 10.4 
20 37 8.0 30 55 8.4 
30 55 75 40 73 79 
40 73 75 50 gt 7-4 
61 112 7 4. 61 112 7 oG 
82 150 7) 2 82 150 FB 
124 227 7.0 103 188 7.6 
B. 144 263 6.9 155 283 7 2 
B. 206 377 6.9 
Temperaturen er synkende fra 100 Fayne til Bunden, 
Observationerne stemme vel overens med de paa Nordhays- 
Expeditionen i det samme Strøg i 1876 maalte (No. 55 til 
No. 61) Bundtemperaturer, der gaa fra 79.2 til 60.9. 
Paa Vestsiden af den ovennævnte Banke har *Han- 
steen” to Temperaturrækker. 
ENNO 
1880. Juli 21. 
64° 36’ N. Br. 8° 15” BF. Led. 
Favne. Meter. Temp. 
(ims). 
0) (0) Tee 
5 9 II .5 
10 18 II .4 
20 37 10.8 
30 55 9.8 
40 73 8.7 
61 I 12 7.8 
82 150 7 2 
103 188 6.9 
1B, NÄR 210 6.9 
Temperaturen aftager med Dybden i de dybere Lag. 
Paa Nordhavs-Expeditionen fandtes midt imellem disse 
Punkter (Station No. 67) i 119 Favnes Dyb 699. Altsaa 
en meget nær Overensstemmelse. | 
84 
Below 100 fathoms, the temperature in the same 
vertical is constant (No. 8), or diminishes slightly with the 
depth. From the south-west to the north-east, or from the 
sea towards the land, the average deep-temperature is found 
to decrease. 
Off the Foldenfjord, lies a bank on which the water 
shoals up to 60 fathoms. Between this bank and the coast, 
extends a deep-channel, cut of from that of the Foldenfjord 
by a shallower ridge. In the former, the following serial 
temperatures were taken from the “Hansteen.” 
No. 13, 
Juli 29. 
Tal, NG, 19 lal, 
Juli 29. 
1880. 1880. 
64° 50’ N. Br. 9° 26! E. Led. 64°48’ N. Br. 10° 5’ E. Led. 
Favne. Meter. Temp. Fayne. Meter. — Temp. 
(Ems). (Ems). 
O fo) 12°.1 (0) (0) LOD 
5 9 12.0 5 9 Ik 43 
IO 18 i o& LO 18 UR o2 
20 37 9.4 20 37 10.0 
30 Re 8 .6 30 55 op 
40 73 td 2 40 73 8.4 
61 112 WH 61 112 8.0 
82 150 7B 82 150 7-9 
103 188 7.0 103 188 Wf 
13}, 127 232 6.9 12¢ 236 7 A 
155 283 7.0 
Bi 221 404 6.8 
| The temperature continues sinking from a depth of 100 
fathoms to the bottom. The observations exhibit excellent 
agreement with the bottom-temperatures — from 7°.2 to 6°.9 ; 
Nos. 55—61 — registered on the North-Atlantic Expedi- 
tion in 1876 throughout the same tract. 
On the west side of the aforesaid bank, we have two 
serial temperatures from the “Hansteen.” 
Jel, INO, 155 
1880. Juli 28. 
649 50’ N. Br. 8° 22” FE. Led. 
Fayne. Meter. Temp. 
(Fms). 
0) 0) 1202 
5 9 12.0 
10 18 II .6 
20 37 9.0 
30 55 8.4 
40 73 8.6 
61 112 7) df 
82 150 Tee) 
Bk ii 203 6.8 
| The temperature diminishes with the depth in the 
deeper strata. On the North-Atlantic Expedition, a tem- 
perature of 6°.9 was measured midway between these points 
(Station No. 67), at a depth of 119 fathoms. Accordingly, 
a very close agreement. 
