The Vistula begins in the south from smaller rivers and tributaries in Belarus, Ukraine, and Slovakia and flows north until it empties into the Gdańsk Bay of the Baltic Sea. With a total length of approximately 650 miles and an average discharge of 38,140 cubic feet per second, the Vistula is easily Poland’s longest and largest river.
The Vistula is often thought of in terms of two different areas: the large delta where the river spreads out into several “fingers” before emptying into the Baltic; and the river and river basin heading upstream (i.e., south).
As far as we can tell, our family’s life in Poland/West Prussia was associated primarily with the upstream area, specifically along the Vistula in the Schwetz area. However, Mennonites first settled in Poland in the Danzig area (mid-1530s), at the northwest corner of the Delta, and shortly thereafter they spread eastward into the Delta itself (note the high density of Mennonite communities marked in that area).
The primary reason for their move east was to turn the swampy and water-logged delta ground into productive farmland. Earlier inhabitants had maintained dikes to hold back the river water as much as possible, but massive breaks in the dikes in 1540 and 1545 had reduced the Danzig Werder (German for “river peninsula, lowlands”) “to a watery waste which gradually became overgrown with reeds and rushes, since it lay below sea level” (Driedger 1957, 16).
The owners of this land—the king of Poland, the Catholic Church, and the cities of Danzig and Elbing—initiated a massive drainage project in 1547 whereby they leased various parcels of land to Mennonite associations who were then responsible to drain and maintain the land.
Johann Driedger, a twentieth-century farmer-minister in East Prussia, offers a detailed account of what was required to accomplish this feat:

This first and most difficult drainage work took three to four generations. The first fruit of the drainage was meadows and pastures with excellent grass. Since the drainage channels with their low dikes carried water which stood considerably higher than the surrounding land there was great danger in rainy seasons or snow thaws that the north wind would blow and drive the water of the Baltic back into the land and through the channels into the rear areas so high that the windmills would not dare to pump the water out of the polders, since in that case the dikes would have been immediately flooded. Consequently the polders were often flooded, and this was tolerable only for meadows and pastures. …
The Mennonites of the Vistula Delta settled not only in areas which lay below sea level but also in swampy areas which lay above sea level but had poor drainage because of lack of discharge channels. In such areas they also succeeded in draining considerable areas of land through development of controlled discharge channels. On such land wheat and rape could be planted, in addition to the raising of dairy cattle. This combination of grain raising and cattle raising gave the Mennonite farmers a considerable advantage above their other neighbors in the delta since they were able to use a considerable amount of animal manure at a time when artificial fertilizers were not yet available.
Source
Driedger, Johann. 1957. Farming among the Mennonites in West and East Prussia. Mennonite Quarterly Review 31:16–21.
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