Characters	Kaman-Shilotter	Sativli 194 hill	Saphale	Nandgaon Murba
Clast/fragment size	Average size 2 to 64 mm 10% to 15% > 64 mm, maximum lm	2 to 64 mm	Upto 64 mm	Murba, mainly lapilli size max. 64 mm
Composition of clast	Basalt, dolerite gabbro, subordinate cherty, siliceous.	Basalt, dolerite, gabbro, diorite, cherty, pumice	Basalt, GPB, gabbro, diorite, dolerite.	Tuffaceous lapilli, basalt, subordinate gabbro,
Shape of Pyroclasts	Sub-angular to angular, bigger ones are more angular, chilled margms	Bombs of various shapes, fragments of bombs, smaller fragments angular.	Subangular to blocky, basaltic blocks	Various shaped bombs, ribbon, spherical and spindle.
Matrix	Basaltic, gray with angular clasts of cherty and soot material, size gradation at places	Tuffaceous glassy, small lapilli of siliceous material with chilled margins	Basaltic, occasional radish clayey muddy.	Basaltic, occasionally muddy.
Welding, compaction, cohesiveness	Cohesive with magmatic character, finer flows have tuffaceous matrix.	Very well welded glassy nature, coarser parts are magmatic and cohesive.	Well consolidated, open framework.	Vitreous nature, magmatic with patches of muddy matrix, less welded
Depositional structures	Massive with occasional gravity bedded, basalt boulders aligned parallel to beds, vitreous tuff beds	Massive, small sectors contain compositionally banded tuffs with planar bedding, bedding sags	Non bedded massive	Massive non bedded
Geometry of the deposit	Sheet, with localized circular to semicircular out crop.	Sheet, inter-layered with tuffs	Wedge shaped with circular out crops	Lenticular, lensoid.
Associated facies	Basalticflows, pumiceous layer on top, pockets of tuff present, interlayered with basic vitric tuff bands, acidic dykes	Thinly bedded compositionally banded tuffs, basalt flows, acidic dykes.	Basaltic flows, gabbro intrusives.	Basaltic flows, plugs of basaltic nature dyke swarm.
Vesicularity of clasts	Scoraceous	Vesicular basalt fragments., small pumice fragments, vesiculated acidic tuff fragments with non vesicular blocks and smaller fragments of all.	Scoraceous fragments of basalt and soot material occasional pumice fragments along with non vesicular fragments.	Scoraceous basalt fragments and scoraceous lava soot material, occasional pumice fragments Besides non vesicular fragments of all.
Vesicularity of clasts	basalt, pumice, vesiculated tuffaceous clasts, non-vesicular blocks of dolerite, gabbro, and acidic rocks and vein quartz.
Relation with the associated facies.	Gradational, conformable and interfingering relation with the associated rocks	Conformable but not gradational, interlayerd with compositionally banded and felsic/flows	Gradational with basalt. Housed within the basaltic pile.	Gradational with the basalt flows, encompassed within the flows itself.