Adirondack Marble Geology

Calcsilicate and granite south of tupper lake.

Adirondack marble geology.

Marble is an example of a metamorphic rock that was created when a chunk of limestone underwent extreme heat. Algonquin peak seen from the south meadows lake plain in north elba 4 october 2015. They mainly consist of metasedimentary rocks chiefly marbles and gneisses. Although the reason s for this doming remain to be fully elucidated.

Marble is a metamorphic rock that forms when limestone is subjected to the heat and pressure of metamorphism. Brief regional geology in the adirondack mountains of new york the adirondack lowlands domain contains sequences of shallow water carbonates evaporites and talc schists upper marble formation sitting on the popple hill gneiss that includes metamorphosed slates mudstones sandstones and volcanogenic sequences. Other adirondack rocks were formed from emerging magma molten rock squeezed up through existing sedimentary and metamorphic rock by the friction of sliding rocks up down and sideways. South meadows lake was a temporary meltwater lake formed during the closing stages of wisconsin glaciation the last of the four main glaciations of the pleistocene ice age epoch.

Grenville marble forms the bedrock under rich lake here in newcomb. The molten rock cooled and crystallized to form igneous rocks such as granite and anorthosite. Because of its limestone origin it has provided a natural buffering agent to the lake protecting it from the effects of acid deposition. The protoliths of these metamorphic rocks were more or less impure limestone and dolostone deposited as shelf sediments in the trans adirondack basin.

Amphibolite with porphyroblasts of k feldspar locally prominent in northwest adirondacks. Bedrock geology of the adirondack region the current topography of the adirondacks is related to doming which began about 180 million years ago when the atlantic ocean opened. Geology of the adirondack park the adirondack dome the adirondack mountains are very different in shape and content from other mountain systems. Biotite and or hornblende granite gneiss middle proterozoic at surface covers 0 3 of this area locally pyroxenic.

It is composed primarily of the mineral calcite caco 3 and usually contains other minerals such as clay minerals micas quartz pyrite iron oxides and graphite. Folded marble and calcsilicate east of speculator.