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The former Northern Coalfield, comprising much of the Newcastle–Maitland–Cessnock–Lake Macquarie region, has now been mined for two hundred years. Most of the twenty-odd seams in the Newcastle, Tomago and Greta Coal Measures have been worked, but the bulk of production has been drawn from just four coalbeds: the Borehole, Greta, Homeville and Great Northern Seams. Literally hundreds of mine names are on record for the coalfield, the great majority working these seams at depths of less than 30 m. This paper reviews regional subsidence problems in the context of mining history, past mining practices and coal measures geology. Subsidence over shallow bord-and-pillar workings may result in highly disturbed ground, open fissures, cratering, seam fires and ‘creeps’ (slow surface movements caused by gradual closure of mine cavities). This form of subsidence differs from that over modern longwall mines in being less predictable, affecting much smaller areas, and occurring sometimes decades after mine abandonment. The geological factors contributing to this subsidence hazard include the multiplicity of seams, the strong roof sandstones, stiff coal and relatively soft floors, and the presence of faults and dykes. The working of thick seams like the Borehole Coal in up to three phases, leaving high, slender pillars, also contributed to later ground instability. Contrary to expectation, the main problem areas are not over haphazardly laid-out convict-era pits, but rather above small hand-worked scavenger mines (‘ratholes’) which operated as late as the 1950s. Many of these short-lived collieries still contain large voids at shallow depth, sometimes only a few metres, which must eventually collapse or be backfilled. [ABSTRACT FROM AUTHOR]