European Waterfalls: Here its course is broken by the Schaffhausen Falls (Ger. Rheinfall or Falls of the Rhine), some 60 feet high, reputed to be the most pic¬turesque of European waterfalls. Among nu¬merous other branches, the Rhine is joined by the Aar, bearing the surplus waters of Zurich, Neu-chatel, and several other Alpine lakes. At Basel (Basle) it turns northward to separate the province of Alsace from Baden. In its course of some 233 miles in Switzerland, it descends nearly 7,000 feet.
A tourist-fare development of great importance to planners for a; European vacation took place in the spring of 1954, when this type of: travel, and tariffs, was extended so as to cover direct flights via Lisbon to i southern European cities. Until that time the tourist fare applied only on 1 the northern European routes and thence southward throughout Europe, i also at tourist rates, to the desired destinations.See Also Numerous Waterfalls:Gudbrandsdal is narrow and steep-sided along most of its length, and the Lagen River, which rushes through it, is broken by numerous rapids and waterfalls. In a few places where the valley broadens out, relatively dense agricultural settlement is found. Otherwise, habitations are krgely restricted to the valley bottom beside the national highway and main-line railroad that run between Oslo and Trondheim.
RORAIMA, rro-rl'ma, mountain of South America, in the Serra Pacaraima, near the junc¬tion of the boundaries of Brazil, Venezuela, and British Guiana. It is 9 miles long and 3 miles wide, and is flat-topped; the highest point has an elevation of 8,620 feet. The sides of the mountain are steep and rocky; the numerous waterfalls are the source of several rivers of Guiana, of the Amazon system (southwards), and of the Orinoco system (westwards).
On The Other Hand See From Waterfalls And Large:Graded streams generally have smooth grad ents, free from waterfalls and large rapids. A important characteristic of such streams is th: they cut laterally to a greater extent than the cut downward. Thus, the presence of flood plain and flat valley floors indicates a graded condition Such quantitative information as is available in dicates that a stream is graded when the slop and the dimensions of the channel are adjusted t the amount of water and sediment passing througi the channel.
Make it a real point, however, to include these minor elements, unless the picture is a close-up portrait or a straight record. If the picture features a group of trees, a second group or other objects a little farther away will help toward balance. In picturing such subjects as waterfalls it is often a help, rather than a hindrance, to include people who may be in the field of view. They should, however, look at the scene—not at the camera—and they should be at least twenty-five feet from the camera.
|
