Geography
The topography of Trafford Park is either flat or gently undulating, about 144 feet (44 m) above sea level at its highest point. The local bedrock is Triassic Bunter Sandstone, overlaid by sand and gravel deposited during the last ice age, around 10,000 years ago. There are some areas of peat bog in the west of the park, in the area formerly known as Trafford Moss. In 1793, William Roscoe began work on reclaiming the bog, and by 1798 that work was sufficiently advanced for him to turn his attention to the task of reclaiming the much larger Chat Moss in nearby Salford, also owned by the Trafford family.
The park occupies an area of 4.7 square miles (12 km2), and is almost entirely surrounded by water. The Bridgewater Canal forms its southeastern and southwestern boundaries, and the Manchester Ship Canal forms its northeastern and northwestern boundaries. Trafford Park is the most northerly area of Trafford, and faces Salford across the Manchester Ship Canal. Stretford lies to the south and east, and Urmston to the west.
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