Cape Granite Suite

At cape granite we take pride in offering our clients a quality product backed by our unsurpassed service and attention to detail.

Cape granite suite.

The three main rock formations are the late precambrian malmesbury group metamorphic rock the peninsula granite a huge batholith that was intruded into the malmesbury group about. At its tip is the cape of good hope the peninsula forms the west side of false bay. The cape granite suite cgs is composed of several late precambrian granitoids located in the south west part of western province. The george pluton is part of the late ediacaran to early cambrian cape granite suite and was named after the city of george in the western cape province of south africa.

Garnet is an accessory mineral in the cape granite suite and garnet δ 18 o values in the peninsula granite range in from 10 0 to 11 4 mean 10 6 0 6 n 15. The maximum age of the cape granite suite is therefore about 552 ma significantly younger than previous age determinations for the oldest cape granite the hoedjiespunt granite. The cape peninsula is a peninsula that juts out into the atlantic ocean at the south western extremity of the african continent. Londolozi s private granite suites are a celebration of elegance and elephants in a remarkable river setting and offer an extraordinary experience for the exclusive use of six guests.

The cape granites formed during the saldanian orogeny part of the panafrican orogenic system. These values are consistent with the garnet being produced during incongruent melting of a metapelitic source that has a similar o isotope composition to the malmesbury group. Those plutons intrude the precambrian malmesbury supergroup and are covered by the table mountain group. The geology of the west coast peninsula forms part of the larger cape granite suite e g.

The field trip will visit key localities. The pan african cape granite suite cgs in the western cape province of south africa comprises mainly s type 560 ma to 530 ma and i type 540 to 520 ma plutons in association with rare a type intrusions 515 to 510 ma. These rocks are not only extremely picturesque but they also contain a wealth of information about the recycling of the continental crust during the saldanian orogeny how large granitic plutons and volcanic complexes are constructed and the source processes that spawned the magmas. The lodge is flanked by an extrusion of granite rocks an effect echoed by the décor s bold materials and silver charcoal and elephant grey palette.