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Foreign News May 21, 1867

The Tri Weekly Standard

Raleigh, Wake County, North Carolina

What is this article about?

At the Swedish Academy of Science's annual meeting, M. Nordenskiold announced a major geological find in Nullaberg, Sweden: a 33-meter-thick bituminous gneiss deposit embedded in gneiss and mica schist, containing organic remains implying early life in Scandinavia's crystalline rocks.

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Full Text

Important Geological Discovery.-At the annual meeting of the Swedish Academy of Science, M. Nordenskiold announced that a discovery of great importance to geological science had been made in the hill of Nullaberg, in Sweden. A large deposit of bituminous gneiss, thirty-three metres in thickness, has been found imbedded in layers of gneiss and mica schist. It is composed, in addition to feldspar, quartz and mica, of a black substance like coal, containing carbonated hydrogen-in fact, a real organic substance, formed of the remains of plants or animals coeval with the deposit. He added that there could be no doubt as to the antiquity and geological situation of the strata of Nullaberg; infiltration was impossible. The inference was that the crystalline stratified rocks of Scandinavia were formed when there existed animated creatures, but at a time long anterior to the period when life is supposed to have first existed on the earth.

What sub-type of article is it?

Scientific Discovery Geological Find

What keywords are associated?

Sweden Geological Discovery Bituminous Gneiss Nordenskiold Scandinavia Rocks Organic Remains

What entities or persons were involved?

M. Nordenskiold

Where did it happen?

Nullaberg, Sweden

Foreign News Details

Primary Location

Nullaberg, Sweden

Key Persons

M. Nordenskiold

Outcome

discovery of bituminous gneiss deposit implies crystalline stratified rocks of scandinavia formed with animated creatures earlier than previously supposed.

Event Details

M. Nordenskiold announced at the Swedish Academy of Science annual meeting a significant geological discovery in Nullaberg, Sweden: a 33-meter-thick deposit of bituminous gneiss embedded in gneiss and mica schist layers, composed of feldspar, quartz, mica, and an organic black substance like coal containing carbonated hydrogen from ancient plant or animal remains. The strata's antiquity rules out infiltration, suggesting early life in the region's rock formation.

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