The last eruption of the volcano took place here in the last thousand years times. Volcanic heat still is felt here – there still are several geothermal areas. Especially active springs are located in the northeastern peninsula of the island, here are located boiling springs, mud pools, and fumaroles, some are depositing sulfur.
Deeper the temperature of the water reaches 180°C, but at the surface, it the temperature of the water is 81 – 96°C. There is found opaline silica which formed when these hot springs were still inundated by the lake water.
In 1902 here (above the lake level) existed springs which on a regular basis erupted – geysers. Over the last decades, geysers have not been observed here anymore.
Soro Hot Springs, Ol Kokwe Island are included in the following list:
- T. Scott Bryan, The Geysers of Yellowstone, fourth edition. 2008. Boulder.
Soro Hot Springs on the map
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|Location, GPS coordinates:||0.6251 N 36.0835 E (possible mistake up to 900 m)|
|Categories:||Thermal springs, Geysers (extinct?)|
|Where is located?||Africa, Kenya, Rift Valley Province, Lake Baringo, north-eastern peninsula of Ol Kokwe Island near Soro|
|Alternate names:||Ol Kokwe Hot Springs|
The aim was simple: to assimilate basic geological facts for each African country, in order to give the regional geologist a digestible starting point for future research. The book, which is printed in full colour on high quality, glossy paper, is in A4 format and organized into four chapters. … the book is very attractive to a wider audience and shouldn’t miss the office table community. The Geological Atlas of Africa is a worthwhile addition to the regional literature on African geology.
This book describes the interrelationship between the spectacular geology of an area of East Africa that includes a branch of the rift valley, as well as giant freestanding ice-capped mountains and extraordinarily toxic, alkaline lakes, and some of the greatest concentrations of wildlife on Earth. It suggests that geological processes that have shaped the iconic landforms, including active volcanoes, may also be responsible for the unusually diverse speciation which characterises the region.