liquid crystal, colloid, SAXS Suspensions of three different clays in K15, a thermotropic liquid crystal have been studied by optical microscopy and small angle X -ray scattering. The three clays were Claytone AF, a surface treated natural montmorillonite, Laponite RD, a synthetic hectorite and mined Sepiolite. The Claytone and Laponite were sterically stabilized whereas Sepiolite formed a relatively stable suspension in K15 without any surface treatment. Micrographs of the different suspensions revealed that all three suspensions contained large scale structures. The nature of these aggregates was investigated using small angle X-ray scattering. For the clays with sheet-like particles, Claytone and Laponite, the flocs contain a mixture of stacked and single platelets. The basal spacing in the stacks was independent of particle concentration in the suspension and the phase of the solvent. The number of platelets in the stack and their percentage in the suspension varied with concentration and the aspect ratio of the platelets. The lath shaped Sepiolite did not show any tendency to organize into ordered structures. Here the aggregates are networks of randomly oriented single rods. [Pizzey 2004], particularly for platelets with a high aspect ratio, for example sterically stabilised montmorillonite particles. Small angle X-ray scattering (SAXS) revealed that these platelets dispersed in K15 (4-pentyl-4'-cyanobiphenyl) form stacks of 5±2 platelets with a basal layer spacing of 37Å independent of the temperature and concentration of the suspension. The spacing and stack size is however influenced by the host. The non-mesogenic host toluene favoured a higher percentage of single platelets and the stacks formed had on average two platelets with a basal layer spacing of 48Å. Particles with a smaller aspect ratio, for example sterically stabilised Laponite, a synthetic hectorite of 1 nm thickness and ~13 nm radius, seemed to delaminate almost completely in both solvents. Only 10% of the particles were found in stacks of 2±1 platelets with the same spacings as for montmorillonite, i.e. 37Å in K15 and 52±7 Å in toluene. The minimum scattering vector, Q, probed in these experiments was 0.03 Å -1 so it was not possible to determine whether the stacks and platelets were isolated or part of a larger aggregate. In this paper we report SAXS measurements extended to a lower Q range (0.003 Å -1 to 0.3 Å -1 ) to investigate the possibility of larger scale aggregation. The low Q was achieved using station 2.1 at the Daresbury Synchrotron Radiation Source [Daresbury] and beamline BM02 at the ESRF in Grenoble [Grenoble] rather than the laboratory based SAXS apparatus employed in the previous work. Furthermore, the high intensity of synchrotron radiation allowed short measurement times so that the flocculation could be monitored as a function of time. In addition results are presented on suspensions of Sepiolite, a naturally occurring clay consisting of lath shaped particles.