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Updated: May 7, 2025
Ashman, and he said if you ever do i will lick you. the babys name is Edward Ashton Shute and not Ashman. i woodent name him for enny cornet player. it is pretty tuff luck. if i cood have got that cornet i woodent have minded a licking. went in swiming today. July 31.
But it has been suggested in explanation that such serpentine may have been originally regularly-bedded trap tuff, and volcanic breccia, with much olivine, which would still retain a stratified appearance after their conversion into a metamorphic rock.
"Next to Bostock and the doctor, father, my best friend," said Carey, eagerly. "Then he is mine," said Mr Cranford. "Here's a canoe of savages off from the island," shouted the captain of the Chusan from the deck. "Does this mean a fight?" "Jackum boy come back," cried the black. "No shoot; all good boy. Jackum take you Big Dan island. Plenty shell, plenty copra, plenty old ship 'tuff.
The chief part consists of red decomposing scoriae, associated with various kinds of tuff and yellow argillaceous beds, full of broken crystals, those of augite being particularly large. Here and there masses of highly cellular and amygdaloidal lavas protrude.
The base of the volcanic series is seen at Carsaig and Gribon to rest on Cretaceous and Jurassic rocks, like those of Antrim; hence the Tertiary age is fully established by the evidence of superposition. This was further confirmed by the discovery by the Duke of Argyll, some years ago , of bands of flint-gravel and tuff, with dicotyledonous leaves amongst the basalts of Ardtun Head.
The tuff consists of white felspathic mud, with fragments of slate and lava, reaching a depth in some places of 150 feet. After it has been quarried it is ground in mills, and used for cement stone under the name of trass.
This tract was converted by subsequent movements into a fresh-water lake, and contemporaneously volcanic operations commenced over the whole region, and beds of tuff, often containing blocks of rock ejected from neighbouring craters, were deposited over those of marine origin.
The terrain consisted mostly of thick slime mixed with petrified branches, but it changed little by little near four o'clock in the afternoon; it grew rockier and seemed to be strewn with pudding stones and a basaltic gravel called "tuff," together with bits of lava and sulfurous obsidian.
The Reformers about him accepted this as the signal of retreat, and they fled precipitately through the door at the rear of the stage. Of them all only four tarried in the wings, Ruse, Sneekins, Divvy, and Hacker; and as they grasped each other's hands in sorrow and sympathy, they saw the stalwart figure of Major Tuff mount the stage. Immediately the hall was quiet. "Gents!" said Tuff.
The lava is vesicular, but the vesicles never reach the surface of the branches, which are smooth and glossy. About a mile southward of Banks' Cove, there is a fine elliptic crater, about five hundred feet in depth, and three-quarters of a mile in diameter. Its bottom is occupied by a lake of brine, out of which some little crateriform hills of tuff rise.
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