Hostname: page-component-848d4c4894-ttngx Total loading time: 0 Render date: 2024-06-05T06:44:44.680Z Has data issue: false hasContentIssue false

V.—Account of an Expedition to Greenland in the year 1870

Published online by Cambridge University Press:  01 May 2009

A. E. Nordenskiöld
Affiliation:
Foreign Correspondent Geol. Soc. Lond., etc., etc., etc.

Extract

Somewhat further to the west of Karsok, and about 50 feet higher up, occurs another similar stratum, containing a mass of graphite, so soft that it may be cut with a knife. This spot was not, however, accurately examined. A similar stratum of graphite imbedded in sand and clay occurs also at a very great height above the sea at Niakornet, but time did not admit of our visiting that spot.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1872

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

page 452 note 1 Heer's Flora Fossilis Arctica.

page 452 note 2 The upper strata in the neighbourhood of Kudliset are Miocene.

page 454 note 1 See further on, Figs. 12 and 13.

page 455 note 1 Rink mentions paths still remaining in districts uninhabited since the time of the old Northmen colonists, and we ourselves could clearly distinguish at Kaja the paths round the long deserted house-sites there.

page 455 note 2 The remarkably slight effect which the eruptive rock has produced on the surrounding layers of sand astonished Mr. Brown.

page 455 note 3 1084 Inglefield; 1175 mean of six measurements with the aneroid by Whymper; 1203 by the aneroid used by the Expedition of 1870.

page 456 note 1 Mean of several observations made in the ravine along the side of which I ascended this slope. Brown gives E. and W. as the direction. The difference probably arises from the circumstance that the magnetic perturbations at Atanekerdluk are of a local nature, and thus different in diiferent ravines.

page 457 note 1 Dr. Nauckhoff's and Dr. Pfaff's discovery of Sigillaria makes it possible that the Coal strata of the Coal formation occur at Ujarasusuk.

page 460 note 1 In this neighbourhood we even meet with sand layers lying beneath the basalt.

page 461 note 1 This Plate was inserted at p. 355, Geol. Mag. for August last, with Part II. of Prof. Nordenskiöld's paper.—Edit. Geol. Mag.

page 462 note 1 Brought to Europe by the Swedish Greenland Expedition of 1872, under command of Capt. Baron von Ober.

page 462 note 2 Of the parts of the stones that lay above ground.