CĂRȚI ÎN ENGLEZĂ ÎN LEGĂTURĂ CU «STINKSTONE»
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It occurs in beds in the flostz or secondary limestone and gypsum formations,
along with stinkstone, in Thin-ingia and Manst'eld. Observations. 1. The grey
colours, dusty particles, meagre feel, and lightness, characterise this mineral. It
passes ...
2
The Edinburgh Philosophical Journal
and in some places met with rocks of that kind of limestone named Stinkstone,
from the peculiarly fetid odour it exhales when pounded. The middle and western
part of this inlet, named Prince Regenfs Inlet, was blocked up, with ice as far as ...
3
The Edinburgh encyclopaedia, conducted by D. Brewster
Stinkstein, »y. Werner. Stinkstone. External Characters. — Its colours are white,
grey, pitch-black, yellow, and brown. Sometimes dendritic on the surface, or
clouded with greyish-black. Occurs massive, disseminated, also in distinct
concretions ...
Edinburgh encyclopaedia, sir David Brewster, 1830
4
Transactions of the Geological Society of London
Stinkstone — a great development of a highly fetid, slaty, cream-coloured
marlstone, with many plants and some shells. It forms the roof of the lignite, and
usually splits into finely laminated slabs, like the lithographic slate of Solenhofen,
...
Geological Society of London, 1835
5
Transactions Of The Geological Society
Stinkstone-a great development of a highly fetid, slaty, cream-coloured marlstone
, with many plants and some shells. It forms the roof of the lignite, and usually
splits into finely laminated slabs, like the lithographic slate ofSolenhofen, offering
a ...
6
The Edinburgh New Philosophical Journal: Exhibiting a View ...
and in some places met with rocks of that kind of limestone nam~ ed Stinkstone,
from the peculiarly fetid odour it exhales when pounded. The middle and western
part of this inlet, named Prince Regent's Inlet, was blocked up with ice as far as ...
Geognostic and Geographic Situations. It occurs in beds in the first and second
floetz limestone and gypsum formations, along with stinkstone, in Thu- ringia and
Mansfeld. Observations. 1. It passes into Limestone, Stinkstone, and Black Clay.
8
Transactions of the geological society, established November ...
Stinkstone-a great development of a highly fetid, slaty, cream-coloured marlstone
, with many plants and some shells. It forms the roof of the lignite, and usually
splits into finely laminated slabs, like the lithographic slate of Solenhofen, oifering
a ...
9
Danmarks geologiske undersøgelse
also contains a number of small angular quartz grains and small grains of
glauconite. The Exsulans Limestone is overlain by a black stinkstone with the
same structure development as in Locality 2. Gronwall (1902) states that the
Exsulans ...
10
Acta palaeontologica Polonica
Modified from Henningsmoen (1957), following Nielsen and Schovsbo (1999).
zones there is a 1.50 m thick stinkstone bed referred to as “The Great Stinkstone
Bed". It comprises a lower part measuring 0.30 m and a upper part measuring
1.20 ...
