The fort, as described by Kregier in his "Journal of the Second Esopus War," was a palisaded village and the largest settlement of the Esopus Indians. He made no reference to a stream or to a ravine, but did note that he was obliged to pass over swamps, frequent kills, and "divers mountains" that were so steep that it was necessary to "haul the wagons and cannon up and down with ropes." His course was "mostly southwest" from Wildwijk, and the fort "about ten miles" (Dutch), or from thirty to thirty-five miles English. It was not so far southwest from Wildwijk (Kingston) as the New Fort by "about four hours," a time measure equal to nine or ten English miles. The Indians did not defend the fort; they abandoned it "two days before" the Dutch troops arrived. No particular description of it has been handed down. Under date of July 31, 1663, Kregier wrote: "In the morning at dawn of day set fire to the fort and all the houses, and while they were in full blaze marched out in good order." And so disappeared forever the historic Indian settlement, not even the name by which it was known certainly translatable in the absence of knowledge of the topography of its precise location. [FN]
[FN] The name has the appearance of derivation from _Gahan_ (Del.), "Shallow, low water"'; spoken with the guttural aspirate _-gks_ (Gahaks), and indefinite formative _-an._ As a generic it would be applicable to the headwaters of any small stream, or place of low water, and may be met in several places.
Magowasinghinck, so written in its earliest form in treaty deed of 1677 (Col. Hist. N. Y., xiii) as the name of an Indian family, and also as the name of a certain kill, or river--"Land lying on both sides of Rondout Kill, or river, and known by the name of Moggewarsinck," in survey for Henry Beekman, 1685--"Land on this side of Rondout Kill named _Ragowasinck,_ from the limits of Frederick Hussay, to a kill that runs in the Ronduyt Kill, or where a large rock lies in the kill," grant to George Davis, 1677. The Beekman grant was on both sides of Rondout Creek west and immediately above Honk Falls, where a large rock lying in the kill was the boundmark to which the name referred and from which it was extended to the stream and place. The George Davis grant has not been located, and may never have been taken up. Beekman sold to Peter Lowe in 1708, and the survey of the latter, in 1722, described his boundary as running west from "the great fall called Heneck." In Mr. Lindsay's History of Ulster County it is said that the grant was half a mile wide on the southeast side of the stream and a mile wide on the northwest side. Hon. Th. E. Benedict writes me: "The Rondout is eminently a river of rocks. It rises on the east side of Peekamoose, Table, and Lone mountains, and west side of Hanover Mountain of the Catskills, and flows through chasms of giant rocks. All the way down there are notable rocks reared in midstream. The rock above Honk Falls is hogback shape, a hundred or more feet long. It lies entirely in the stream and divides it into two swift channels which join together just above the falls. Here, amid the roar, the swirl and dash of waters breaking through rocky barriers, with the rapids at the falls, the Great Rock was an object to be remembered as a boundmark."