The most easterly of the Kobuk-Selawik Lowland alkaline complexes (Fig. 121), the Ekiek Creek intrusion covers 13 km2 and cuts quartz monzonites along its southern boundary, but there are no contact effects; to the west, north and south it is surrounded by alluvium.
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The building of the Black Mountain volcano involved the eruption of a series of voluminous ash-flow tuffs, multiple caldera subsidence, and partial or complete filling of the caldera by lavas.
Figs 169 and 172 Geophysical work, later confirmed by drilling, has shown that the Granite Mountain and Saline County intrusions are continuous at depth, the whole complex being referred to as the Little Rock igneous complex by Gordon et al. (1958, p. 67).
In the northeastern corner of Rhode Island peralkaline granites occur which have been correlated with the Quincy granite lying some 40 km to the northeast. They comprise microperthite, quartz, up to 10% sodic amphibole and 7% aegirine; patches and veins of purple fluorite are common.
In the southeastern corner of the Deep River Quadrangle, a sequence of granite gneisses includes a layer of aegirine-augite granite gneiss, the Joshua Rock gneiss, which extends into the unmapped quadrangle to the east.
At the upper contact of a 500 m thick dolerite sill nepheline and analcime-bearing syenite occur, both cutting the sill rocks and hornfelsed argillite. Poor exposure precludes the accurate determination of field relationships.
A suite of northwest-trending dykes injected into Palaeozoic sedimentary rocks of the Shenandoah Valley includes teschenites, camptonites, aegirine, nepheline and quartz syenites, spinel-bearing basalts, mica peridotites and olivine dolerites.
The Mount Rogers magma series includes mafic to felsic plutonic and volcanic rocks in which silica-oversaturated units have peralkaline affinities. Barker (1974, p. 161) indicates the presence of aegirine and/or riebeckite granite and rhyolite.
A metamorphosed, peralkaline granite is exposed in a quarry 0.8 km southeast of the town of Fountain. Dykes of amphibolite, metarhyolite and basalt cut the granite, which is foliated.
These occurrences form part of the Diablo Plateau segment of the Trans-Pecos magmatic province. Marble Canyon is an oval-shaped intrusion of 0.6x1.5 km which cuts and metamorphoses Permian dolomitic limestones.