Linn Park et alia loca
Sponsored by the Linn Park Gentlemen's Walking Club

Introduction

Many things have come and gone in Linn Park, but the most remarkable, yet most elusive, were the mills. The mills harnessed the river to drive their water wheels, and were the main source of employment in the area. If we stand today by the remains of their dams, we can almost hear the plash-plash of their water wheels. From the advent of rotary steam power in the 1790s, water power was in decline. Yet, in the search for renewable energy, water power is now experiencing a renaissance. In recent years, most of the former mill sites in the area have been seriously considered by consultants for small-scale power generation.

Linn FallsBy some accounts, the stretch of the White Cart Water flowing through the park only supported one mill, a snuff mill. However mills did much more than grind snuff. Basically they were sources of power for almost any industrial process. Snuff milling was one of many mills in the park area, including paper, meal, flour, barley, pease, waulk, saw mills, bleachfields and printfields.

There were so many mills in Linn Park, that it is easiest to locate and understand them by their dams or falls. Each fall powered one or more individual mills, or several mill types. As each type of mill needed specific skills, the millers moved around between similar mills in the wider area, so we need to consider them too.

Erosion at Millholm WeirStarting just above Linn Park, the first waterfall was at Netherlee. The second was the natural fall at Linn. The third dam was at Millholm, now breached at the east end. The fourth was at Cartside, now gone. The fifth was at Cathcart Meal mill, many of its great sandstone blocks carried away by the force of the river. To understand the mills fully we need to carry on briefly downstream below the park to two other dams. The sixth dam was behind Weirs works, now lost. The seventh and final dam was at the end of Dundrennan Road for Millbrae Mill.

The river is always changing. A century ago, for most of the year, the river was a series of long tranquil stretches, separate by dramatic dams or waterfalls. This was still the situation through much of the park from Linn Falls down to Millholm until 1984, when Millholm dam burst. Since then, the river has gradually worn its way down through 300 years of deposits.

Further reading: What follows was mostly provided by Stuart Nisbet from his articles: ‘Netherlee and Linn Mills’ (The Eastwoodian Vol.1, 1989); ‘Renfrewshire Snuff Mills’ (RLHF Journal Vol.6 1994); The Four Paper Mills of Cathcart (Scottish Local History Vol.49, 2001).

Other material is accredited within its section.

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