The Geographical Journal, Volume 15Royal Geographical Society., 1900 - Geography Includes the Proceedings of the Royal geographical society, formerly pub. separately. |
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Page 17
... latter . The ridges are nearly bare of sand , and brown in colour . The general effect reminds one of snow clinging to the shady side of the valleys on the spurs of a mountain - side . Mr. Floyer's efforts are directed to reclaiming a ...
... latter . The ridges are nearly bare of sand , and brown in colour . The general effect reminds one of snow clinging to the shady side of the valleys on the spurs of a mountain - side . Mr. Floyer's efforts are directed to reclaiming a ...
Page 22
and from the right , the latter sweeping in swirls across the floor of the fulj . The compact floor was somewhat eroded by the wind , showing a sort of erosion - rippling . I stuck a reed cane in the sand at the summit of the cliff and ...
and from the right , the latter sweeping in swirls across the floor of the fulj . The compact floor was somewhat eroded by the wind , showing a sort of erosion - rippling . I stuck a reed cane in the sand at the summit of the cliff and ...
Page 22
... latter is formed by deposition of sand upon a hard floor . It is , however , not difficult to imagine that in some cases barchans may be residual forms . Thus , if the wind continued to blow away the sand from the spot shown in Fig . 24 ...
... latter is formed by deposition of sand upon a hard floor . It is , however , not difficult to imagine that in some cases barchans may be residual forms . Thus , if the wind continued to blow away the sand from the spot shown in Fig . 24 ...
Page 38
... latter high salinity is obtained from the liquid ice of the spongy part of the floe . Direct measurement of the ice - floes has shown that the ice - ridges have generally the height of 10 to 14 feet . It is not unusual to meet an ice ...
... latter high salinity is obtained from the liquid ice of the spongy part of the floe . Direct measurement of the ice - floes has shown that the ice - ridges have generally the height of 10 to 14 feet . It is not unusual to meet an ice ...
Page 51
... latter view is accepted in the maps which accompany the work . In order to reach the Omo near the lowest known point on its course , it was now necessary to strike west across a mountainous region in which constant rain was experienced ...
... latter view is accepted in the maps which accompany the work . In order to reach the Omo near the lowest known point on its course , it was now necessary to strike west across a mountainous region in which constant rain was experienced ...
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Common terms and phrases
Abyssinian Africa altitude Arun Arundel Asia basin Bhotiyas Bognor British Captain Central centre Chalk Chichester Chitambo coast coastal plain crossed depth district dunes east eastern elevation escarpment expedition exploration fathoms feet forest Fort Jameson Geographical Society geological glacial glacier gorge ground harbour height high-road hills inches India island Journal journey Kalonga lake Lake Kivu land large number Lavant valley Littlehampton Loanda Loch Loch Katrine Loch Lubnaig Loch Voil London Lukchun Map and Illustrations Meteorological Midhurst Milam miles mountains native Nile north-east north-west northern observations pass Petworth plateau Presented Price Prof published Pulborough railway rainfall reached region Report ridge river road rocks route runs sand sheet shows slope south-west southern Spitsbergen square miles Stane Street station stream sudd surface Survey temperature Tibet Tibetan travellers trees valley village White Nile whole wind
Popular passages
Page 238 - I am directed by the Lords Commissioners of Her Majesty's Treasury to acquaint you that my Lords are...
Page 74 - Rawson, at the advanced age of eightyeight years, the Society has lost one of its oldest and most valued members.
Page 510 - Tables relating to the Output of Coal and other Minerals and the number of persons employed at mines worked under the Coal and Metalliferous Mines Regulation Acts during the Year 1899.
Page 33 - I was engaged at that time with my service, and did not then see my way to disclose my ideas, but I made some preliminary preparations. I wrote to Dr. Nansen a letter, in which I stated that I was entirely of his opinion, that he would be carried by the currents somewhere in the direction he imagined, and advised him that help should be sent for him to Franz Josef Land. My letter to him and his answer were duly published in the Russian newspapers and in geographical publications.
Page 511 - Report of the Expeditions organized by the British Astronomical Association to observe the total Solar Eclipse of 1898, January 22.
Page 122 - Sound, as commentators generally assume. " Now, having the wind at north-north-east, we steered away south and by east, with purpose to fall with the southermost part of this land, which we saw ; hoping by this meane, either to defray the charge of the voyage [? by discovery], or else, if it pleased God in time to give us a faire wind to the north-east, to satisfie expectation.
Page 57 - Dickson a'so contributed a paper on the temperature and salinity of the surface water of the North Atlantic during 1896 and 1897.
Page 422 - SOUTH AMERICA AND PACIFIC OCEAN. South America Pilot, part 1. East coast of South America, from cape St. Roque to cape Virgins, with the Falkland, South Georgia, Sandwich, and South Shetland islands ; also the north coast from cape St. Roque to cape Orange, in...
Page 181 - Report on the geology of the area covered by the Seine River and Lake Shebandowan map sheets, comprising portions of Rainy River and Thunder Bay districts, Ontario.
Page 125 - On the norther side of the mouth of this inlet lie three ilands [really blocks of mountains divided by valleys, which would look like islands from the distance (10 leagues) they were from land], not farre the one from the other, being very high mountainous land. The farthest of the three to the north-west [ie the block of the sea-front just south of the entrance to Ice fiord] hath four very high mounts [Mount Starashchin], like heapes of corne.