Sceal, J. S. C., & Weaver, S. D. (1971). Trace element data bearing on the origin of salic rocks from the Quaternary volcano Paka, Gregory Rift, Kenya. Earth and Planetary Science Letters, 12(3), 327-331. doi.org/10.1016/0012-821X(71)90218-4

Key, R. M. (1987). Geology of the Maralal area. Republic of Kenya Ministry of Environment and Natural Resources, Mines and Geological Department Report, 105.

Dunkley, P. N., Smith, M., Allen, D. J., & Darling, W. G. (1993). The geothermal activity and geology of the northern sector of the Kenya Rift Valley.

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	*Dunkley, P N, Smith, M, Allen, D J, Darling, W G (1993) The geothermal activity and geology of the northern sector of the Kenya Rift Valley. Research Report* SC/93/1. British Geological Survey**	Report (issue)
	activity and geology of the northern sector of the Kenya Rift Valley British Geological Survey Research...activity and geology of the northern sector of the Kenya Rift Valley P N Dunkley, M Smith, D J Allen and...activity and geology of the northern sector of the Kenya Rift Valley P N Dunkley, M Smith, D J Allen and...springs along its western shores. Geographic index Kenya Suf>jecr index Geothermal exploration, geology...activity and geology of the northern sector of the Kenya Rift Valley. British Geological Survey Research
	*Jones, W.B. (1979) Syenite boulders associated with Kenyan trachyte volcanoes. Lithos, 12 (2) 89-97 doi:10.1016/0024-4937(79)90040-9*	Journal (article/letter/editorial)
	trachy~ic liquid in mngmz chambers under each volcano, is proposed for these. Separ'ation of a small...Londiani at the ju~letion of the Kenya and Kavirondo Rift Valleys., Kenya (Fig. 1)(Jones 1975). On Kilombe...boulders are found on the outer slopes of the volcano and in sediments at its foot formed by erosion...katophorite, sometimes grading marginally tewards arfvedsonite. Some specimens also have large green-brown...2ookm J -. ~. ~o ~8oE ,, Fig. 1. Location o f Kenya Rift Valley. K - Kilombe; L l.or~diani. nepheline
	*Price, R. C., Chappell, B. W. (1975) Fractional crystallisation and the petrology of Dunedin volcano. Contributions to Mineralogy and Petrology, 53 (3) 157-182 doi:10.1007/bf00372602*	Journal (article/letter/editorial)
	Fractional Crystallisation and the Petrology of Dunedin Volcano R.C. Price Department of Geology, University of...the range in rock types making up the Dunedin volcano has developed by crystal fractionation processes...variants on these series. The phonolitic rocks of the volcano are low pressure differentiates derived by fractional...outlined above. Quartz normative trachytes of the volcano appear to be differentiates from a distinct saturated...Fig. 1. Distribution of volcanics of the Dunedin Volcano. Domes are indicated and flow directions are outlined
	*Girdler, R. W. (1972) East African Rifts* - Developments in Geotectonics No. 7. Elsevier. doi:10.1016/c2013-0-11826-0**	Book
	magnetic surveys in northern Tanzania and southern Kenya B.W. Darracott, J.D. Fairhead and R.W. Girdler (Newcastle...of two areas in the Kenya Rift Valley J. Wohlenberg and N.V. Bhatt (Nairobi, Kenya) Planning of the airmagnetic...results of a seismic refraction experiment in the Kenya Rift D.H. Griffiths (Birmingham, Great Britain)...southwestern Afar is there a tendency for an axial volcano-tectonic lineament (Wonji fault belt) to extend...calderas most probably represents a tensional volcano-tectonic structure affecting the Danakil horst

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Arfvedsonite from Paka Volcano, Baringo County, Kenya

Arfvedsonite from
Paka Volcano, Baringo County, Kenya