Journal of the Transactions of the Victoria Institute, Or Philosophical Society of Great Britain, Том 21Victoria Institute., 1888 |
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Стр. xii
... Eastern Exploration continues to be at a standstill both in Babylonia and Palestine , by reason of the Porte still withholding the firmans once accorded to the English Government , and under which such important dis- coveries have ...
... Eastern Exploration continues to be at a standstill both in Babylonia and Palestine , by reason of the Porte still withholding the firmans once accorded to the English Government , and under which such important dis- coveries have ...
Стр. 11
... east . It includes the remarkable depression of the Jordan - Arabah valley , which , commencing on the north at the western base of Mount Lebanon , in Cole Syria , ranges south- ward along the line of the Jordan ; and , being continued ...
... east . It includes the remarkable depression of the Jordan - Arabah valley , which , commencing on the north at the western base of Mount Lebanon , in Cole Syria , ranges south- ward along the line of the Jordan ; and , being continued ...
Стр. 14
... east of the Bitter Lakes , ranges in a southerly direction for about 150 miles , and then , bending round towards the east at Jebel el Ejmeh , ultimately reaches the western margin of the Arabah valley near the head of the Gulf of ...
... east of the Bitter Lakes , ranges in a southerly direction for about 150 miles , and then , bending round towards the east at Jebel el Ejmeh , ultimately reaches the western margin of the Arabah valley near the head of the Gulf of ...
Стр. 15
... east of Safed . This terrace is as nearly as possible at a level with that of the Mediterranean . Hence Dr. Lortet has inferred that the waters of the Sea of Tiberias formerly stood at that level . This terrace near the northern margin ...
... east of Safed . This terrace is as nearly as possible at a level with that of the Mediterranean . Hence Dr. Lortet has inferred that the waters of the Sea of Tiberias formerly stood at that level . This terrace near the northern margin ...
Стр. 16
... east , to the extent of 1,000 feet and upwards . * On this account it is that the Nubian sandstone formation appears along the eastern side of the Ghor , but never on the western , that side being formed of Cretaceous limestone ; while ...
... east , to the extent of 1,000 feet and upwards . * On this account it is that the Nubian sandstone formation appears along the eastern side of the Ghor , but never on the western , that side being formed of Cretaceous limestone ; while ...
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