- Captain John Smith’s Map of New England
The Pilgrims were familiar with Capt. John Smith’s account of a voyage in which he had surveyed the coast from Cape Cod to Penobscot Bay in 1614. He had even offered his services as guide and military captain, but Myles Standish got the job. Undoubtedly they did bring with them his Description of New England (London, 1616), in which the following map was published. Capt. Smith, who had already gained some fame and fortune in Virginia, dedicated to Prince Charles this effort in which the term “New England” first appeared: “... it being my chance to range some other parts of America, whereof I here present your highness the description in a map, my humble suit [in original, “sure”] is you would please to change their barbarous names for such English, as posterity may say Prince Charles was their godfather.” Several English place-names were incorporated in the map, but posterity disregarded most of them, a noteworthy exception being “Plimouth.” Smith notes that the Indians called the site “... Accomack, an excellent good harbor, good land, and no want of any thing but industrious people,” recalling that “After much kindness, upon a small occasion we fought also with 40 or 50 of those [Indians]; though some were hurt and some slain, yet within an hour after, they became friends.” - Samuel de Champlain’s Map of Plymouth Harbor
Although the Pilgrims were the first Europeans to establish a permanent colony in northeastern North America, they did not come to an unknown land. As early as 1605, Samuel de Champlain had mapped Plymouth Harbor, in the course of a three-year expedition during which he explored the coast from Nova Scotia to Martha’s Vineyard. The quality of his detailed and accurate observations on the land and people appears in this map, and in his notes on the visit: “There came to us two or three canoes, which had just been fishing for cod and other fish which are found there in large numbers. These they catch with hooks made of a piece of wood, to which they attach a bone in the shape of a spear and fasten it very securely. The whole has a fang-shape, and the line attached to it is made out of the bark of a tree. They gave me one of their hooks, which I took out of curiosity. In it the bone was fastened on by hemp, like that in France, as it seemed to me, and they told me that they gathered this plant without being obliged to cultivate it, and indicated that it grew to the height of four or five feet. This canoe went back on shore to give notice to their fellow inhabitants, who caused columns of smoke to arise on our account. We saw eighteen or twenty savages, who came to the shore and began to dance. Our canoe landed in order to give them some bagatelles, at which they were greatly pleased. Some of them came to us and begged us to go to their river. We weighed anchor to do so, but were unable to enter on account of the small amount of water, it being low tide, and were accordingly obliged to anchor at the mouth. I went ashore, where I saw many others, who received us very cordially. I made also an examination of the river, but saw only an arm of water extending a short distance inland, where the land is only in part cleared. Running into this is merely a brook not deep enough for boats except at full tide. The circuit of the bay is about a league. On one side of the entrance to this bay there is a point which is almost an island, covered with wood, principally pines, and adjoins sandbanks, which are very extensive. On the other side, the land is high. There are two islets in this bay, which are not seen until one has entered, and around which it is almost entirely dry at low tide. This place is very conspicuous from the sea, for the coast is very low, excepting the cape at the entrance to the bay. We named it the Port du Cap. St. Louis...”. - Reconstruction of coal-forming swamp
Coal is a combustible rock that was formed by the accumulation and partial decay of vegetation. When coal was forming millions of years ago, most of the state was a low coastal plain bordered on the west and southwest by a shallow sea. A large variety of plants grew in great swamps which covered this coastal plain. When the plants died, they accumulated in the swamps to form thick masses of peat that were eventually covered by shallow seas and buried beneath mud and sand. Periodically, the region was above sea level, new swamps developed, new peat deposits accumulated, and more sediments were laid down. This process occurred repeatedly until over 3,000 feet of sediments had been deposited. Then the sediments were slowly compacted and hardened so that sandstones, shales, limestones, and coals were formed. - Extent of the main glacial advances
Extent of the main glacial advances which began with the Nebraskan (a—the oldest) and ended with the late Wisconsinan (f—the youngest). Diagram “d” shows the major stream development during the time between the Illinoian and the earliest Wisconsinan glaciers. The heavy lines on the diagrams indicate major stream valleys that were present during these times. a. Inferred limit of NEBRASKAN glaciation b. Inferred limit of KANSAN glaciation c. ILLINOIAN glacial advance d. SANGAMONIAN major drainage e. Maximum WISCONSINAN glacial advance f. Late WISCONSINAN Valparaiso front and Kankakee Flood - Physiographic provinces of Illinois
Physiography is the study of the creation and gradual change of land surface forms (the landscape). Thus, the land surface as we see it today in each of the physiographic provinces has had a particular history of development. Driftless Area Wisconsinan Moraines Illinoian Till Plain Mississippi River Wabash River Shawnee Hills Ohio River - Austin, Nevada, six thousand feet above the sea
Austin, Nevada, six thousand feet above the sea. The metropolis of the Reese river district. Silver first discovered at this point in July, 1862. - The Typist
Lynde Pyne watched the graceful movements of Leonie's fingers over the key board - Choice of fabric
Here a small all-over pattern minimizes size, the plaits and tassels lengthen, the necklace adds a slenderizing touch. The appearance as a whole is graceful and youthful. - Two looks - same pattern
Would you believe that the pattern of these two dresses is exactly the same? This illustrates how you can vary a dress once you find the foundation lines that are becoming to you. One pattern can suffice for both a tailored and an afternoon dress, as you see both effects are pleasing in their slenderness. - Hats 1
These two examples show how even a hat with drooping brim, if not too wide, can be worn by the stout person if trimming is adeptly used to direct the vision upward and lend an illusion of height. - Hats 2
Here trimming is used on two entirely different types of hats to give in each case added height to the figure and help in attaining a slenderizing appearance. Left—Hats with medium brims and high trimming are often becoming, especially if wide enough to avoid the pyramid effect. Right—High built trimming and delicate veils are advantageous where a double chin is the handicap. - Optical Illusion in dress
Note the diagonal line in the small diagram of the figure below. It is actually straight, but the vertical lines which break it give it a “going-down-steps” appearance. This principle is used in the dress below—the two vertical panels of trimming break the line of the tunic and give the whole figure a more slender appearance than in the figure above.