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Extra resources for Anleitung zur Kenntnis und Behandlung der Pistole 1900/06
6 billion years has left the remaining highland areas fragmented. Notable among these outlying peaks and massifs is the Makari Mountain above Canister Falls in Guyana, the Tafelberg and Emma Range in east-central Suriname, the Urupi Massif in the northeastern corner of Amazonas state, Brazil, Serra Araca (Jauri), Padre and Pico de Neblina (transnational) near the Venezuelan frontier, and Uneuxi between the Negro and Japurá Rivers. In Venezuela, a series of outlying massifs extend in a north–south alignment near the Casiquiare Biophysical Features of the Guiana Shield rift valley in Amazonas state.
Most of this supports dry forest, scrub and desert, with a much smaller fraction covered by tropical moist forests in comparison to South America, where the Guiana Shield accounts for the largest amount (see Chapter 1). The difference in amount of exposed Precambrian basement provides another useful means of contrasting the geology of the Guiana Shield from other tropical regions. The implications of this to tropical forest dynamics at the cratonic level are discussed further in Chapter 7. EXTENT OF EXPOSURE PHANEROZOIC COVER Across the South American craton, only the Guiana, Central Brazilian and Atlantic Shields exhibit sig- Biophysical Features of the Guiana Shield 19 Global tropical forestlands Mainly volcanic Mainly Plutonic SE Asia Central America Caribbean South America Africa Australia India Less Precambrian More Precambrian Australia India South America Africa More exposed More Buried Africa South America Mostly Phanerozoic cover Mostly Proterozoic cover Sub-Andean Foredeep Amazon Downwarp Guiana Shield Central Brazilian Shield Atlantic Shield Greenstone belts rare Central Brazilian Shield Atlantic Shield Greenstone belts common Guiana Shield Fig.
4E). They consist mainly of metamorphosed tuffaceous lavas, pumice and ignimbrites (lithiﬁed volcanic ash and breccia). Highland centres forming the Sierra Maigualida, Sierra de Guampi and Sierra Guanay ranges are granitic intrusives formed from the Santa Rosalia and San Pedro batholiths. g. 1). Signiﬁcant sedimentary formations can be found in three provinces delimited by Gibbs and Barron (1993). Localized and often not insigniﬁcant formations can be found, however, throughout the Guiana Shield interspersed with metamorphosed volcanic, subvolcanic and plutonic groups.