The Physical Features And Geology of Borneo
The Physical Features And Geology of Borneo
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Since they have broken through the highest beds of the limestone stage, they are probably of Miocene age. Above the andesites lies a series of shales and sandstones, which Verbeek describes as Late Tertiary (Miocene). The lower beds consist of soft shales and harder marls. The greenish sandstones which lie above them have, in great measure, derived their material from the andesites and tuff. These Miocene beds contain occasional seams of brown coal, which is very inferior^ as fuel to the black ...coal of the Eocene beds.
* An admirable summary, with full reference to the literature, will be found in Posewitz's "Borneo. " • "The vegetation of the Sunda Islands has retained its Indian character, from the Eocene period down to the present time, although the Tertiary floras of Europe have been considerably modified. " Geyler, Jaarb. V. H. Mynwezen in Ncderl. -Ind. 1879. II.
"5 The diluvium (drift) of the plains occurs chiefly as a zone round the Tertiary hill-land, though it also covers the flanks of the mountains.
What to read after The Physical Features And Geology of Borneo?
You can find similar books in the "Read Also" column, or choose other free books by F H Frederick Henry Hatch to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Since they have broken through the highest beds of the limestone stage, they are probably of Miocene age. Above the andesites lies a series of shales and sandstones, which Verbeek describes as Late Tertiary (Miocene). The lower beds consist of soft shales and harder marls. The greenish sandstones which lie above them have, in great measure, derived their material from the andesites and tuff. These Miocene beds contain occasional seams of brown coal, which is very inferior^ as fuel to the black ...coal of the Eocene beds.
* An admirable summary, with full reference to the literature, will be found in Posewitz's "Borneo. " • "The vegetation of the Sunda Islands has retained its Indian character, from the Eocene period down to the present time, although the Tertiary floras of Europe have been considerably modified. " Geyler, Jaarb. V. H. Mynwezen in Ncderl. -Ind. 1879. II.
"5 The diluvium (drift) of the plains occurs chiefly as a zone round the Tertiary hill-land, though it also covers the flanks of the mountains.
What to read after The Physical Features And Geology of Borneo?
You can find similar books in the "Read Also" column, or choose other free books by F H Frederick Henry Hatch to read onlineMoreLess
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