SEARCH
0-9 A B C D E F G H I J K L M N O P Q R S T U V W X Y Z
Prev | Current Page 108 | Next

Kingsley, Charles, 1819-1875

"Town Geology"


Instead of which, the coal is usually pure vegetable, parted sharply
from the sandstone which lies on it. The only other explanation was,
that the coal vegetation had grown in the very places where it was
found. But that seemed too strange to be true, till that great
geologist, Sir W. Logan--who has since done such good work in Canada-
-showed that every bed of coal had a bed of clay under it, and that
that clay always contained fossils called Stigmaria. Then it came
out that the Stigmaria in the under clay had long filaments attached
to them, while when found in the sandstones or shales, they had lost
their filaments, and seemed more or less rolled--in fact, that the
natural place of the Stigmaria was in the under clay. Then Mr.
Binney discovered a tree--a Sigillaria, standing upright in the coal-
measures with its roots attached. Those roots penetrated into the
under clay of the coal; and those roots were Stigmarias. That seems
to have settled the question. The Sigillarias, at least, had grown
where they were found, and the clay beneath the coal-beds was the
original soil on which they had grown. Just so, if you will look at
any peat bog you will find it bottomed by clay, which clay is pierced
everywhere by the roots of the moss forming the peat, or of the
trees, birches, alders, poplars, and willows, which grow in the bog.


Pages:
96 97 98 99 100 101 102 103 104 105 106 107 108 109 110 111 112 113 114 115 116 117 118 119 120