78 EJNAR MIKKELSEN. 
easterly branch of Danmark’s Fjord, which had escaped the observation 
of the Myzrius-ERICHSEN party. 
A very accurate track-survey was made while travelling out through 
this fjord, and its direction was at first determined in the same manner 
as in Fyen’s Lake, i. e. by means of the sun, which at 2 a.m. was standing 
right over its northerly end. 
The breadth of the fjord off Cape Holbæk was determined by the 
walking distance across it. The fjord opened up immediately after pas- 
sing this cape, and it became at once evident that it was the Dan- 
mark’s Fjord, in which we travelled, and observations were taken in 
order to get the exact data, on which to base the direction of the 
fjord. 
Observations for latitude and longitude were made (Station VI), 
and azimuths were taken to three defined points north of the stations, 
and one to the south, to Cape Holbeek. 
The distance from the station VI to Cape Viborg is about 8 miles, 
and an error in judging this distance of more than one mile is absolutely 
out of the question. With the sight from station VI to Cape Viborg 
and the travelled distance we have the means to determine with a fair 
accuracy the breadth of Danmark’s Fjord off this cape. 
While off a jutting point just south of Hjærtefjældsdalen on 81°07’ 
we could as yet distinguish a sharply outlined and easily recognizable 
mountain at the southern end of Sjællandsfjældene just clear of Cape 
Holbæk, which can be seen from the shore itself on 81°15’ N. Lat. and 
this proves without the aid of track-survey and observations that the 
south-end of Danmark’s Fjord does not bend off to the west as shown 
on the map of HorGc-HAGeEn. 
The east coast of Danmark’s Fjord fell off to the east just north of 
Cape Viborg, and it seems as if a little further north the fjord may have 
the breadth shown on the map of HoEG-HAGEN. 
Foggy weather and our anxiety to get along towards the mouth of 
the fjord forced us to discontinue the track-surveying from Ulvebakkerne 
and northward, but the direction of the coast, as well as all indentations 
and capes, was apparently quite correct on this part of the coastline, 
and further along the coast, as often as we had a chance of checking 
the surveys of Horc-HaGen, we found them correct as well in their 
chief features as in details. 
On the map of the journey over the Inlandice, Pl. I, there will 
be found two ice-profiles, a longitudinal and a cross-section cut. 
The longitudinal profile is mainly a nearly north-south cut of the 
Inlandice from Brede Bre to Fyen’s Lake, and it represents all the material 
for determining the heights, which has been gathered and which has 
been deemed reliable. 
The actual rise or fall in the heights of the Inlandice as shown 
