Download e-book for kindle: Africa by Gemma Pitcher

By Gemma Pitcher

ISBN-10: 0311839800

ISBN-13: 9780311839803

ISBN-10: 0411827707

ISBN-13: 9780411827700

ISBN-10: 0611823020

ISBN-13: 9780611823021

ISBN-10: 0631822119

ISBN-13: 9780631822110

ISBN-10: 0912352477

ISBN-13: 9780912352473

ISBN-10: 0922815860

ISBN-13: 9780922815869

Discover Africa

Watch the sunlight set over the Niger at Mopti, the place Malians exchange fish for salt with the wilderness Tuareg.
Wake as much as the tug of a trunk as elephants wander via your campsite within the Serengeti nationwide Park.
Dip your oar quietly into the Okavango Delta as you flow in the direction of a satisfaction of lions lounging at the water's edge.

In This Guide:

24 authors, forty nine nations, 1 scrumptious tremendous rat.
Covering extra international locations than the other Africa go back and forth guide.
Feature bankruptcy on Africa's improvement by way of veteran Africa journalist and best-selling writer Michela Wrong.
Visit lonelyplanet.com for up to date studies, updates, and traveller suggestions.

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Extra resources for Africa

Example text

J T Karar a ^ "V ^PJebel Bou Gobrine °S/, •>', *5>t *-\ / " " - ^ *-c Namib Taung A . , Springbok o a T • • • + Mid Pleistocene Early Pleistocene Pliocene Later Miocene EarlierMiocene Oligocene Eocene •sterktontein area o 7 Cornell Principal fossil mammal localities in Africa. The inset shows the East African area at an enlarged scale. used in the past by vertebrate palaeontologists. Thus Fort Ternan, described as late Miocene in the literature, is technically middle Miocene, as also is the 'early Pliocene' site of Ngorora.

Depositional breaks, mainly coincident with thickening of the soil outside the caves, alternated repeatedly with Cambridge Histories Online © Cambridge University Press, 2008 THE PALAEO-ECOLOGY OF THE AFRICAN CONTINENT episodes of soil attrition at the surface and gradual infilling of the caves below. In other words, the stratigraphy is more complex than was originally thought, the time-spans represented by each cave are considerably longer, and the external climates represented were somewhat more variable.

In East Africa, the bedrock beneath the volcanics consists largely of Precambrian granitic and metamorphic rocks and most of the volcanics lie on the sub-Miocene erosion surface. Some warping and faulting took place, followed by extensive volcanic activity. Although largely fissure eruptions, there were also many central volcanoes that built substantial cones. A number of these Miocene volcanoes now expose thin lenses of fossil-bearing sediment that had been deposited in localized basins or traps on the flanks of the cones and have now been re-exposed as a result of fairly extensive dissection.

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Africa by Gemma Pitcher


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