The Mohawks lived farther east, in the Mohawk Valley, among the limestone and granitic formations of the Adirondacks and Eastern New York, and they were the Agmaque, meaning "the possessors of the flint." Within the league their name was Ganniagwari, or the "She-Bear," whence the Algonquins called them Mahaque, which the English gradually corrupted into Mohawk, the name being also adopted for their river. The early Dutch settlers at Albany made a treaty with them which was lasting, and the English also had their friendship. Their most noted chief was Thayendanega, better known as Joseph Brant, who espoused the English cause in the Revolution and held a post in the Canadian Indian Department, his tribe then extending throughout the whole region between the St. Lawrence and the Hudson. He visited England in 1786 and collected money to build a church for his people, and published the Prayer-Book and the Gospel of Mark in Mohawk and English. He steadily exerted himself after the Revolution to maintain peace between the frontier Indians and the United States, being zealously devoted to the welfare of his tribe. He had an estate on the shore of Lake Ontario, where he died in 1807. LITTLE FALLS AND UTICA. In ascending the Mohawk valley the distant view is circumscribed on the south by the Catskills and Helderbergs, and on the north by the Adirondack ranges. The outcrops of the latter compress upon the river in long protruding crags covered with firs and known as the "Noses." There are various villages, started in the eighteenth century as frontier posts among the Indians. There are also hop-fields in plenty and much pasture, and finally the hills become higher and the valley narrower as Little Falls is reached, where the Mohawk forces a passage through a spur of the Adirondacks, known as the Rollaway. The river, approaching the gorge, sharply bends from east to south, and plunges wildly down a series of rapids, the town being set among the rocky precipices right in the throat of the defile. The place is heaped with rocks, the stream falling forty-two feet within a thousand yards, the descent forming three separate cataracts, which give power to numerous mills on the banks and clustering upon an island in the rapids. They make cheese and paper, and on either hand precipitous crags rise five hundred feet above them. The pass is very narrow, compressing the Erie Canal and the New York Central and West Shore Railways closely upon the river; in fact, the canal passage has been blasted out of the solid granite on the southern river-bank. Here can be readily studied the crystalline rocks of the Laurentian formation, which are described as "part of the oldest dry land on the face of the globe." It is this pass through the mountains, made by the Mohawk, that gives the Erie Canal and the Vanderbilt railways their low-level route between the Atlantic seaboard and the West. All the other trunk railways climb the