Cseh János: Régészeti tanulmányok a Közép - Tisza-vidékről (Tiszai téka 4-5. Szolnok, 1993)

is possible, that that spindle-whorl belongs to this era, which is remained half, and which of greyish (a little bit rough), laminated breaking-surface. I found it from the settlement-focus to north-east at 100-150 m. Whereas a bigger iron-slag lump is attached to the focus by place too. On the central part of the site comparatively much millstone was lying on the surface, hewn from porous, of volcanic origin rock - lower (catillus) and upper (meta) stones. From an approx. 10x5 m ground I had collected four such ones, that was giving fitted to one another thirdhalf of the very worn rotating-part. Of this that was become to be reconstructed also, which around 45 cm diameter, with thickness not larger than 5 cm. For the axis resp. its transversal fastening served an elongated-oval groove hewn with margin. But our another find may have been a lower stone, with circular hole making in it, diameter of 35-40 cm, about 3-4 cm thickness. The whetstone-fragmenta are of beigish-„pink" sandstone, and issuing from the nature of the matter, as the millstones too, they could have been belonged to the imperial epoch resp. the iron age as well. Reverted to the above written down late migration age material, so it seems, that widest the period has to be taken into account lasting from the second half of the 8th century to the first half of the 10th century (as it is not classic late avar ceramic-ensemble and not typical one of the early age of the Árpáds), emphasized the 9th century. (Finally still we must notice, that the site is loosely connected with the site 11st12nd-13rd.) Site 23. (8th of May) North-western field-part, Sarkad-brooklet, little-bridge The place of the data-inclusion is measured from the church of the community at distance of 4,9-5 air kilometres, where the minor road arriving from south, which is served as the boundary of the village also, leaves a wooded zone. Here it may be cross a little bridge over the bed of the Sarkad-rill (resp. Sarkad-rill-canal), that is of 100-150 m broad, reedy-damp-marchy. The environment is covered, grassy, unobservable, of 88-88,5 m altitude above sea-level. Archeological finds it was possible to gather on the minor road and in the wall of the no too deep trench running beside that on both sides, at approx. 50 m lenght. I was getting together somewhat more than a dozen things, ten pieces shards, burnt daub and animal bone. Among the former there were entirely indeterminable, characterless vesselfragments of old age (on one of which with the trace of the so-called sausage-technique?). There were occurred some granulous, brownish-coloured sides (and bottom-parts as well?) - it is hard to decide, that they are wheel-thrown or hand-made. These may be conditionally regarded as scythian ones. It was to be found a wheel-turned, grainy, brownish, of thiner wall-side adorned with combed in horizontal lines, which is perhabs of late migration eopch or early Árpád age (-of period of the Hungarian conquest). In the slanting eastern wall of the trench extending on the oriental side of the track, just at the height of the brooklet-bank I had found a grave's place. On the ripping canal-bank-edge judged from the traces the (cinerary-) urnnest was being trodden out in the course of ranging of cattle's herd. Undoing after the sherd-pile it was come to light a clay-vessel, while directly at 20-30 cm to north