Sprinkler drop Y Sprinkler/other piping Y Electrical distribution Equipment Y Diesel generator Y RCMF: reinforced concrete moment frame; CHB: concrete hollow block; RC: reinforced concrete; Y: flag for component assignment; X: “Remove

of the mudstone block. B ) Close-up of a patch of subvertical tentaculitids in mudstone block from the south clay quarry, Hungry Hollow, Ontario, showing grid-like spacing pattern of upward-projecting apertural ends (University of Michigan Museum of Paleontology specimen UMMP 73818 collected by John and Michael

Figure 13. Recent topples of large undercut blocks along southeastern shore of Lake McConaughy. A) Large blocks of soft Ash Hollow Formation strata and soil, with intact turf cover, on cliff face at landward terminus of large erosional platform in S½, SW¼ NE¼ NW¼, section 8, T.14N., R.38W

Figure 2 ( Upper ) Hollowed out sandstone blocks (1 m diameter) from the Cedar Mountain Formation, Moab, Utah (USA). These blocks experience both case hardening of the outer shell and core softening (white arrows) of the block interior. ( Lower ) Backscatter electron (BSE) image of the Mn–Fe-rich

FIG. 7. —View eastward at B ( Fig. 1c ) of gastropod limestone at top of riser of Sandy Hollow step. Middle and upper parts of gastropod limestone crumpled and slid over its lower layers as overriding block of Sandy Hollow thrust surmounted top of riser.

Fig. 5.— Microbial mat in Unit 2. A ) Upper surface of Block A showing wrinkle marks and two intersecting trackways of Diplichnites cuithensis . B ) Close-up of wrinkle marks on Block A. C ) Upper surface of Block C illustrating concentric wrinkles around a hollow on the sediment surface. D

Formation. Arapien Shale is exposed beneath these extremely thinned Eocene rocks, and all are separated from light gray, east-dipping pebbly sandstone of the Miocene formation of Black Cap Mountain by a narrow horse block of sandstone and siltstone of the Eocene Crazy Hollow Formation. These Green River

Fig. 4. The Upper Chalk/Base Palaeogene (Reading Formation) contact at Alum Bay on the Isle of Wight [SZ 200 930] showing: (A) an irregular erosional contact lined with flint blocks and (B) solution hollow infilled with sediment.

Figure 1. Outline of mine showing haulage levels and undercut (at bottom) for new block cave, event (hollow black circles) and station (filled red squares) locations, and previously mined volume (at top). Event locations for March 2010 are shown.

Figure 7. (A) All measured slickenline sets on C-planes (solid circles) and S-planes (hollow circles). (B) All slip vectors calculated from S-C fabrics (see text for method). (C) Rose diagram of graywacke and greenstone block long-axis trends.