Abiyata diatomite is situated in Central Main Ethiopian Rift (CMER) on the narrow strip of land dividing the two lakes Abiyata and Shala in the lakes district of the Ethiopian Rift Valley which is about 210 km from Addis Ababa. Geology of the deposit area is composed of Miocene to Quaternary age acidic igneous rocks consisting of pyroclastic tuff, ignimbrite and pumice and lacustrine sediments in which diatomite is hosted. rnDiatomite's geological, geochemical, and mineralogical features, as well as its formation, are discussed in this research. To characterize diatomite from Abiyata, chemical, mineralogical, technological, and micro paleontological examinations were conducted on samples collected from outcrops and stream sections. rnThe XRD characteristic peaks of diatomite demonstrate that it is primarily made up of Opal-A silica, however certain crystalline phases were discovered in adequate amounts. Quartz and feldspar were the predominant crystalline phases, with lesser amounts of calcite, cristobalite, illite, mordinite, wairakite, halloysite, clinoaptilolite, adularia, and tridymite. rnFrom SEM photomicrographs diatomites are primarily formed of benthic freshwater diatom species such as Staurosirella pinnata, Staurosira construens, Pseudostaurosira brevistriata, Epithemia Sorex and surirella pinnata. Diatom species, sedimentary profile sections and mineralogical data suggest that diatomite was deposited in lacustrine-type freshwater shallow lake environment. rnChemical data obtained from 10 diatomite samples show that while silica is the bodybuilding material for diatomite. i.e., Silica (SiO2), 76.9%; Alumina (Al2O3), 3.49%; Sodium Oxide (Na2O), 1.52%; Potassium Oxide (K2O), 1.107%; Iron Oxide (Fe2O3), 1.1%; Loss on ignition (LOI) 13.7 and other oxides are below 1%. rnStudies from technological properties like physical tests, chemistry, and mineralogy and micropaleontology of Abiyata diatomite suggest that calcined diatomite can be used for waste treatment processes in the filter aid industry and as filler material.