oalib
Search Results: 1 - 10 of 100 matches for " "
All listed articles are free for downloading (OA Articles)
Page 1 /100
Display every page Item
Ants of the Kruger National Park
A. J. Prins
Koedoe : African Protected Area Conservation and Science , 1965, DOI: 10.4102/koedoe.v8i1.790
Abstract: Ants of the Kruger National Park
The freshwater molluscs of the Kruger National Park  [cached]
G. Oberholzer,J. A. Van Eeden
Koedoe : African Protected Area Conservation and Science , 1967, DOI: 10.4102/koedoe.v10i1.762
Abstract: The freshwater molluscs of the Kruger National Park
Scarabaeidae from the Kruger National Park  [cached]
M. C. Ferreira
Koedoe : African Protected Area Conservation and Science , 1967, DOI: 10.4102/koedoe.v10i1.770
Abstract: Scarabaeidae from the Kruger National Park
The freshwater fished of the Kruger National Park  [cached]
Ph.D, U. de V. Pienaar
Koedoe : African Protected Area Conservation and Science , 1968, DOI: 10.4102/koedoe.v11i1.761
Abstract: The freshwater fished of the Kruger National Park
Geological Guide to Selected Areas of the Kruger National Park
J.W. Bristow,R. Sweeney,F.J. Venter
Koedoe : African Protected Area Conservation and Science , 1986, DOI: 10.4102/koedoe.v29i1.530
Abstract: The Kruger National Park (KNP) contains a considerable variety of rock types, ranging from Archaean granitoids to Recent sedimentary deposits. Some 3 500 million years of geological history is represented in an approximately 85 km east-west section at the southern area of the Kruger National Park. Older rocks are typically found in the western half of the KNP and to the east rock units become progressively younger. Some of the more important rock types found in the KNP include greenstones of the Barberton Mountain Land (approximately 3 500 million years old), granitoid rocks of the Nelspruit Batholith (approximately 3 200 million years old), syenitic intrusions associated with the Phalaborwa Complex (approximately 2 050 million years old), Soutpansberg volcanics and sediments (approximately 1 750 million years old), Timbavati Gabbros (approximately 1 450 million years old?), Karoo sediments and Lebombo volcanics (approximately 200 - 170 million years old) and Cretaceous to Recent sedimentary deposits which are best developed in the eastern region of the park.
The influence of the African Elephant on the vegetation of the Kruger National Park  [cached]
P. Van Wyk,N. Fairall
Koedoe : African Protected Area Conservation and Science , 1969, DOI: 10.4102/koedoe.v12i1.747
Abstract: The influence of the African Elephant on the vegetation of the Kruger National Park
Animal behaviour with respect to tourists in the Kruger National Park
B.Sc. (Eng.), K. Babich
Koedoe : African Protected Area Conservation and Science , 1964, DOI: 10.4102/koedoe.v7i1.807
Abstract: Animal behaviour with respect to tourists in the Kruger National Park
The Zoogeography and systematic list of Amphibia in the Kruger National Park
Ph.D., U. De V. Pienaar
Koedoe : African Protected Area Conservation and Science , 1963, DOI: 10.4102/koedoe.v6i1.814
Abstract: The Zoogeography and systematic list of Amphibia in the Kruger National Park
The Solifugae, Scorpions and Pedipalpi of the Kruger National Park  [cached]
R. F. Lawrence
Koedoe : African Protected Area Conservation and Science , 1964, DOI: 10.4102/koedoe.v7i1.797
Abstract: The Solifugae, Scorpions and Pedipalpi of the Kruger National Park
The Pseudoscorpions (False-Scorpions) of the Kruger National Park  [cached]
R. F. Lawrence
Koedoe : African Protected Area Conservation and Science , 1967, DOI: 10.4102/koedoe.v10i1.766
Abstract: The Pseudoscorpions (False-Scorpions) of the Kruger National Park
Page 1 /100
Display every page Item


Home
Copyright © 2008-2017 Open Access Library. All rights reserved.