extensive basin occupying the northwestern part of Transdanubia in northwestern Hungary, and extending into Austria and Slovakia (where it is called Podunajská Lowland). It has an area of approximately 3,000 square miles (8,000 square km). It is bounded on the south and east by the highlands of Transdanubia (Bakony and Vértes), to the west by the foothills of the Austrian Alps, and to the north by the Carpathians in Slovakia. The major drainage direction is west-east via the Danube River. The Rába River and its tributaries drain the Hungarian section through Győr, and in Slovakia the Váh River system enters the Danube at Komárno (Komárom).

Some of the Little Alfold is exceptionally rich agricultural land that produces wheat, corn (maize), rye, barley, sugar beets, potatoes, fodder crops, table vegetables, and tobacco; the basin has orchards and vineyards. Livestock breeding—dairy cattle, pigs, horses, and poultry—is also important. The climate is relatively dry, but abundant water comes from the surrounding highlands.

Only in its middle and north-central parts is the Little Alfold properly a plain; on the margins are degraded alluvial fans and low hills. The major settlement in the area is Győr. Submergence and basin formation of the Little Alfold began several million years ago. Deposition and local submergence has continued on a smaller scale, and the Little Alfold is subsiding very slightly.