...ot India or the Himalayas. The Past History of Ceylon and South-India as indicated by its Fawna. — In our account of the Ethiopian region we have already...affinity with Malaya, require however some closer approxima-- tion to these islands, which probably occurred at a later period. When, still later, the...

...India consisting mainly of granite and old-metamorphic rocks, while the greater part of the peninsula is of tertiary formation, with a few isolated patches...Malaya, require, however, some closer approximation with these islands, which probably occurred at a later period. When, still later, the great plains...

...India consisting mainly of granite and old-metamorphic rocks, while the greater part of the peninsula is of tertiary formation, with a few isolated patches...Malaya, require, however, some closer approximation with these islands, which probably occurred at a later period. When, still later, the great plains...

...India consisting mainly of granite and old-metamorphic rocks, while the greater part of the peninsula is of tertiary formation, with a few isolated patches...evident, therefore, that during much of the tertiary period.f Ceylon and South India were bounded on the north by a considerable extent of sea, and probably...

...India consisting mainly of granite and old-metamorphic rocks, while the greater part of the peninsula is of tertiary formation, with a few isolated patches...Period, Ceylon and South India were bounded on the ftorth by » considerable extent of sea, and probably formed part of an extensive Southern Continent...

...connect their earliest origin with that people. But they have emerged H 'VuV !?• eviden* that> dur'°K much of the tertiary period, Ceylon and South India...very numerous and remarkable cases of affinity with Malava require however some closer approximation to these islands, which of >0C'°Ur " PetM" Wallaoe'...