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Dividend Two Directory 04
Page 03
In so far as this is a process of growth, accompanied by the assumption of a definite form, it might be compared with the growth of a crystal of salt in brine: but, on closer examination, it turns out to be something very different. For the crystal of salt grows by taking to itself the salt contained in the brine, which is added to its exterior; whereas the plant grows by addition to its interior: and there is not a trace of the characteristic compounds of the plant's body, albumin, gluten, starch, or cellulose, or fat, in the soil, or in the water, or in the air.
The most important spoon in the Jamestown collection, and one of the most significant objects excavated, is an incomplete pewter spoon--a variant of the trifid, or split-end, type common during the 1650-90 period. Impressed on the handle (in the trefoil finial of the stem) is the mark of the maker, giving his name, the Virginia town where he worked, and the year he started business. This is the sole surviving "touch" or mark of an American pewterer of the 17th century. The complete legend, encircling a heart, reads: "IOSEPH COPELAND/1675/CHUCKATUCK." (Chuckatuck is a small Virginia village in Nansemond County, about 30 miles southeast of Jamestown.) Joseph Copeland later moved to Jamestown where he was caretaker of the statehouse from 1688-91. He may have made pewter in Virginia's first capital. His matchless spoon found in the old Jamestown soil is the oldest dated piece of American-made pewter in existence.
I left Tarma on January 29th, following a well-cultivated valley, fairly thickly inhabited. We were travelling over a good mule-track, swarming with Indians, donkeys, mules, and horses. The mud houses and land on either side were enclosed by hedges of cacti, or by walls. We were between barren mountains of a brownish colour, against which the quaint, brightly-coloured costumes of the many people on the road were thrown out in vivid contrast. Most of the houses were constructed of large mud bricks, sun-dried. The crops seemed to consist chiefly of Indian corn. As we went farther, among dark brown rocks and limestone, we came to grottoes and rock habitations. At some remote period there must have been a great upheaval in that country--at least, judging by the sedimentary foliated rock, the strata of which were from one to three feet thick, and which had originally been deposited horizontally by water. These accumulations or sediments now stood up at an angle of 45 deg.. We were now in a region where llamas were plentiful--most delightful animals, with their pointed ears pricked up, their luxuriant coats, and stumpy curled tails.
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