Explain the geographical factors which have attracted refugees to settle in different parts of Uttar Pradesh.

Physical geography as pull

• The Ganga–Yamuna Doab and the wider Ganga plain offer deep alluvium, a long kharif–rabi window, and canal or tubewell irrigation, which promised a farm restart to agrarian refugees from West Punjab and Sindh after 1947.
• A sub-humid monsoon climate, without the extreme aridity of western Rajasthan or the high-altitude cold of the Himalaya, lowered the ecological shock of relocation for plains people.
• The Terai–Bhabar belt, once malaria-blocked, opened after DDT and colonisation schemes in the 1950s; empty moist grassland became a settlement frontier for Partition families, hill migrants, and later land-hungry peasants.
• Riverine tracts and oxbows also absorbed fishing and labour households, including some streams from the 1971 Bangladesh crisis into eastern districts, though that wave was smaller than Punjab’s.

Situation, towns, and corridors

• Western UP sits on the Delhi–Amritsar road and rail corridor; Meerut, Saharanpur, Muzaffarnagar, Moradabad, and Ghaziabad offered mandis, workshops, and later industry, so refugees clustered where accessibility, not only soil, was high.
• Shared Indo-Aryan speech, wheat–sugarcane diets, and existing Muslim–Hindu mixed towns reduced cultural distance compared with a move to the deep South or the far North-East.
• State capital Lucknow, mill town Kanpur, and pilgrimage-commercial Varanasi pulled educated and trading refugee groups toward urban niches rather than only toward canal villages.
• Geography therefore selected western Doab and Terai first, then industrial and administrative cities; flood-prone east and dry Bundelkhand received fewer Partition farmers because the resource package was weaker.