conglomeratic

In places the sandstone may be conglomeratic or ferruginous.

A conglomeratic member, called the Lost Run Member, exists in some locations.

It also contains beds of massive white, red or purple sandstone and conglomeratic sandstone.

First, the basal lower member consisting of purplish arkosic conglomeratic sandstone.

The raw material used for these anchors are hard basaltic, sedimentary and a few of conglomeratic material.

Tarkwa Mine mines several low-grade conglomeratic "reefs" of Tarkwaian type.

The group contains volcanogenic conglomeratic sandstone, fine-grained tuffite and tuffaceous sediment.

Confirmation is found in the increase of coarser sands and number of conglomeratic intervals towards the south within the alluvial fans.

Coarse-grained and conglomeratic sandstones which transressive overlain basalts, gently dipping to the south.

Lower Member: conglomeratic sandstone, present only in depressions formed in the underlying Devonian limestone.

The Qiseib Formation consists of sandstones, conglomeratic at the base with an overall fining upward trend.

The lower Oligocene is conglomeratic and pro-grades southward into evaporite and lacustrine deposits.

The site has two horizons of Landscape marble and outcrops of conglomeratic bone-beds (in the Westbury shales).

The formation is composed of conglomerate, conglomeratic sandstone, sandstone, coal and marine siltstone and shale.

Asymmetrically deformed quartz pebbles in conglomeratic layers of the Thiviers sandstone indicate dextral shearing.

Close to the border faults crop out the so-called sidérolithique (iron-rich, reddish, clayey sands) and solidified, conglomeratic alluvial deposits.

High tablelands are capped with tuffs, andesite, and basalt lavas, and volcanic-derived conglomeratic sandstones and mudstones.

Near its top, the limestone is conglomeratic and pelletoidal, in part, with pebbles and cobbles of limestone, chert, meta-arkose, and quartz.

The massif is formed mainly from Palaeogene limestone and, on its southern edge, an overlying coarse sandstone of Miocene age which is largely conglomeratic.

Quaternary glaciofluvial deposits, alluvial deposits, and Tertiary conglomeratic white quartz-breccia units have been mined in the Dutch Hills.

The clayey sediments of the Alemoa Member gradually give way to the more sandy, rarely conglomeratic, Caturrita Formation, which finishes with an unconformity.

The Viking Formation is composed of fine to coarse grained sandstone with interbeds of conglomerate and cherty conglomeratic sandstone.

The Shinumo Quartzite overlying this unconformity consists of arkosic conglomeratic sandstone that contains quartzite and granite pebbles.

It is a white to medium-gray or gray-green subgraywacke, sandstone, siltstone and shale, cross-stratified and conglomeratic conglomerate in parts, containing a few shale interbeds.

One conglomeratic sandstone layer that lies about 21 m (70 ft) above the base of the Shinumo Quartzite near the South Kaibab trail contains jasper pebbles.