Submit an Article
Become a reviewer
Vol 1 Iss. 4
Pages:
318
Download volume:
RUS
Article

On the formation of telluric iron from bog ores

Authors:
A. E. Kupffer
Date submitted:
1908-06-10
Date accepted:
1908-08-20
Date published:
1908-12-01

Abstract

In 1891, 20 versts northeast of Vologda, near the Church of St. Nicholas of Vozimsky (near Lake Kubinskoe), a piece of iron was found under a peat mass within a bed of bog ore, shallow from the surface. It was originally covered with a loose coating of ocher and immersed in the bog ore; its weight together with the ocher was 1100 grams. In some places it was permeated with rust to a certain depth. Freed from the ocherous shell, it took the shape of a spherical sector measuring about 10 centimeters wide and about 5 centimeters thick; it was veined and, in places, contained fine-grained inclusions of ocherous magnetic ironstone.

Область исследования:
(Archived) Without section
Funding:

None

Go to volume 1

References

  1. Dr. E. Zikendrat, note in Bulletin de la Société Impériale des Naturalistes de Moscou, 1892, new series, Vol. VI, p. 444.

Similar articles

Hypoparallel aragonite intergrowth from Bilin
1908 Ye. S. Fedorov
On the formation of well-crystallizing and water-soluble salts of alkali and alkaline earth metals in so-called colloid-amorphous formations
1908 P. P. von-Weymarn
Several specimens of graphite deposits belonging to the mineralogical collection of the Mining Museum
1908 A. N. Zavaritsky
Representation of crystal structure by vector circles
1908 Ye. S. Fedorov
Construction of second-order curved surfaces (conosecunds) and the complete hexahedron
1908 Ye. S. Fedorov
Construction of a second-order curved surface (a conosecund) from imaginary pairs of points or an imaginary conic section.
1908 Ye. S. Fedorov