From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #3952 Reply-To: ammf@fruvous.com Sender: owner-ammf-digest@smoe.org Errors-To: owner-ammf-digest@smoe.org Precedence: bulk alt.music.moxy-fruvous digest Saturday, April 11 2020 Volume 14 : Number 3952 Today's Subjects: ----------------- Stop the āpain chainā now. Hereās the 1 thing you should do! ["Nerve Heal] ---------------------------------------------------------------------- Date: Sat, 11 Apr 2020 08:17:44 -0400 From: "Nerve Health" Subject: Stop the āpain chainā now. Hereās the 1 thing you should do! Stop the bpain chainb now. Herebs the 1 thing you should do! http://ketocarr.buzz/B4kfYaajgppvJzVh4FDBHjUIVMqdBpoCTVFvZimh6jjqRgJq http://ketocarr.buzz/9VruvjaEaokI6kFesc2EwY1aUNoRjaKZ15v7REhSnvz5LQud rea is formed from a thick succession of sedimentary rocks, largely limestones but also including sandstones, mudstones and siltstones. All of the solid rocks exposed at the surface are of Carboniferous age though they are underlain at depth by Old Red Sandstone of Devonian age which in turn overlies rocks of Lower Palaeozoic age. None of the pre-Carboniferous rocks is seen at the surface in the area. The limestones, which date from the Visean stage of the early Carboniferous, formed as sediments in a tropical sea approximately 325 million years ago. The strata contain fossil corals, crinoids, sea urchins and ammonites. This bed of limestone is up to 800 metres thick. In the north and west it lies on a shelf of Galway granite which supported the upper layers, preventing shifts like those that created the "twisted" hills Knockanes and Mullaghmore. The limestone also extends below Galway Bay out to the Aran Islands and to the east into the Gort plain.:16,33 Later in the Carboniferous (c. 318 million years ago), the limestone was covered by darker sand and mud that later turned into shale (the lower "Clare Shales") and sandstone (the upper "Millstone Grit"). These layers reached a thickness of up to 330 metres (1,080 ft) in north Clare. These top layers protected the underlying limestone from erosion for millions of years before being largely stripped away by glaciers, except in the south west, where they still extend from Doolin to Slieve Elva, Lisdoonvarna, Kilfenora and to the western shore of Lake Inchiquin. One "island" of shale is the hill Poulacapple, southwest of Ballyvaughan, where an upland moor has formed on top of the impermeable shale layers.:16,33:17 The local geological succession comprises the following formations some of which are subdivided into various members. The youngest rocks are at the start of the list, the oldest at the bottom. The first three listed are of Namurian age and are a mix of mudstones, sandstones and siltstones, the remainder are Visean age limesto ------------------------------ End of alt.music.moxy-fruvous digest V14 #3952 **********************************************