A Popular Account of Dr. Livingstone's Expedition to the Zambesi and its tributaries - And of the Discovery of Lakes Shirwa and Nyassa, 1858-1864 by David Livingstone
page 6 of 394 (01%)
page 6 of 394 (01%)
|
to be thereby accomplished, formed a noble contrast to some of the
earlier expeditions to Eastern Africa. I believe that the information it will give, respecting the people visited and the countries traversed, will not be materially gainsaid by any future commonplace traveller like myself, who may be blest with fair health and a gleam of sunshine in his breast. This account is written in the earnest hope that it may contribute to that information which will yet cause the great and fertile continent of Africa to be no longer kept wantonly sealed, but made available as the scene of European enterprise, and will enable its people to take a place among the nations of the earth, thus securing the happiness and prosperity of tribes now sunk in barbarism or debased by slavery; and, above all, I cherish the hope that it may lead to the introduction of the blessings of the Gospel. In order that the following narrative may be clearly understood, it is necessary to call to mind some things which took place previous to the Zambesi Expedition being sent out. Most geographers are aware that, before the discovery of Lake Ngami and the well-watered country in which the Makololo dwell, the idea prevailed that a large part of the interior of Africa consisted of sandy deserts, into which rivers ran and were lost. During my journey in 1852-6, from sea to sea, across the south intertropical part of the continent, it was found to be a well-watered country, with large tracts of fine fertile soil covered with forest, and beautiful grassy valleys, occupied by a considerable population; and one of the most wonderful waterfalls in the world was brought to light. The peculiar form of the continent was then ascertained to be an elevated plateau, somewhat depressed in the centre, and with fissures in the sides by which the rivers escaped to the sea; and this great fact in physical geography can never be referred to without calling to mind the remarkable hypothesis by which the distinguished President of the Royal Geographical |
|