Outstanding feature	High energy radial ooids & quartz - in with thin isopachus and equant cement
Folk Classification	Well sorted quartzose oosparite
Dunham Classification	Well sorted quartzose oograinstone
Common Grains	Ooids, &quartz
Sorting	Well sorted
Rounding	Well rounded
Micritization & envelopes	A few coated grains
Cement & diagenetic fabric	Isopachus cement, interpenetration of ooids before final passive equant spar
Porosity	None
Depositional Setting	High energy shoal
Diagenetic history	Freshwater isopachus cement

Striking high energy ooid grains within spar cement matrix. Radial calcitic ooid cortex is concentricly layered about nucleae of both quartz and micritic pelloids. Darkened spots within ooid layers and micrite envelopes are cyanobacteria colonies that caused local micritization when high energy grains came to rest in this setting. In some parts of thin section common points of contact between ooids show some interpenetration and disolution at ooid grain boundaries.