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Updated: June 19, 2025


So they sailed past the Isle of Sciathos, with the Cape of Sepius on their left, and turned to the northward toward Pelion, up the long Magnesian shore. On their right hand was the open sea, and on their left old Pelion rose, while the clouds crawled round his dark pine forests, and his caps of summer snow.

He gave his cook the house of a Magnesian citizen, as a reward for a single highly successful supper, and, at last, when he was proceeding to lay a second whole tribute on Asia, Hybreas, speaking on behalf of the cities, took courage, and told him broadly, but aptly enough for Antony's taste, "If you can take two yearly tributes, you can doubtless give us a couple of summers, and a double harvest time;" and put it to him in the plainest and boldest way, that Asia had raised two hundred thousand talents for his service: "If this has not been paid to you, ask your collectors for it; if it has, and is all gone, we are ruined men."

"You must remember that the calcium will be supplied in the limestone;" cautioned Percy. "And, if you use magnesian limestone, you will thus supply both calcium and magnesium. Keep in mind that magnesian only means that the limestone contains some magnesium. and that it is not a pure calcium carbonate.

Methone and Pydna are on the Macedonian coast approaching Thessaly. Pagasae is a Thessalian town in the Magnesian district. It was the sea-port of Pherae, capital of the tyrant Lycophron, against whom Philip was invited to assist the Thessalians.

The "Empress Spring" would be a hard spot to find. What landmarks there are I will now describe. The entrance is in a low outcrop of magnesian limestone, surrounded by buckbush, a few low quondongs and a low, broom-like shrub; beyond this, mulga scrub. Immediately to the North of the outcrop runs a high sand-ridge, covered sparsely with acacia and spinifex.

"The Fourth" Magnesian Limestone, or lowest number of the Ozark series recognized, has its typical exposures along the Niangua and Osage rivers in Morgan and Camden counties. Professor Swallow, in his Missouri Geological Survey Reports I. and II., 1853 and 1854, says: "Caves, natural bridges and subterranean streams occur in the valley of the Osage and its tributaries."

Professor Sedgwick in 1832 described what is now recognised as the central member of this group, the Magnesian limestone, showing that it attained a thickness of 600 feet along the north-east of England, in the counties of Durham, Yorkshire, and Nottinghamshire, its lower part often passing into a fossiliferous marl-slate and resting on an inferior Red Sandstone, the equivalent of the Rothliegendes of Germany.

Among the most remarkable examples of concretionary structure are those described by Professor Sedgwick as abounding in the magnesian limestone of the north of England.

Though magnesian, it is of a different quality from that employed in building our Houses of Parliament. As this was carefully selected, the latter was carelessly unselected. It was quarried at random, in the most ignorant way; some of it proved little better than chalk; and though all sorts of nostrums have been tried, nothing will cure the radical defect.

They have been classed with the Magnesian Limestone by Professor Sedgwick, as being nearly co-extensive with it in geographical range, though their relations are very obscure. But the principal development of Lower Permian is, as we have seen by Mr. Organic remains are generally wanting, but the leaves and wood of coniferous plants, and in one case a cone, have been found.

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