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Concept
Hutterites
Summary
Hutterites (Hutterer), also called Hutterian Brethren (German: Hutterische Brüder), are a communal ethnoreligious branch of Anabaptists, who, like the Amish and Mennonites, trace their roots to the Radical Reformation of the early 16th century and have formed intentional communities.
The founder of the Hutterites, Jakob Hutter, "established the Hutterite colonies on the basis of the Schleitheim Confession, a classic Anabaptist statement of faith" of 1527, and the first communes were formed in 1528. Since the death of Hutter in 1536, the beliefs of the Hutterites, especially those espousing a community of goods and nonresistance, have resulted in hundreds of years of diaspora in many countries. The Hutterites embarked on a series of migrations through central and eastern Europe. Nearly extinct by the 18th century, they migrated to Russia in 1770 and about a hundred years later to North America. Over the course of 140 years, their population living in community of goods recovered from about 400 to around 50,000 at present. Today, almost all Hutterites live in Western Canada and the upper Great Plains of the United States.
Anabaptism
The Anabaptist movement, from which the Hutterites emerged, started in groups that formed after the early Reformation in Switzerland led by Huldrych Zwingli (1484–1531). These new groups were part of the Radical Reformation, which departed from the teachings of Zwingli and the Swiss Reformed Church. In Zurich on January 21, 1525, Conrad Grebel (c. 1498–1526) and Jörg Blaurock (c. 1491–1529) practiced adult baptism to each other and then to others. From Switzerland Anabaptism quickly spread northward and eastward in the timespan of one year. Balthasar Hubmaier (c. 1480–1528), a Bavarian from Friedberg, became an Anabaptist in Zurich in 1525 but fled to Nikolsburg in Moravia in May 1526. Other early Anabaptists who became important for the emerging Hutterites were Hans Denck (c. 1500–1527), Hans Hut (1490–1527), Hans Schlaffer († 1528), Leonhard Schiemer (c.
Official source
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