/ UPPISTOVUBEITINUM. SITK AND SETTKKMKNT 39 - a cattle passage - which connected the settlement with the outfields through the surrounding infield. If we take into account our present knowledge of settlement continuity, these settlement areas or heimrust are exceeding- ly important to archaeologists and histori- ans alike, as they conceal settlement re- mains from over a long period of time - re- mains which are the basic source of our knowledge of early Faroese history, unless they of course have been disturbed by later activity. In Leirvík all three settlements or býling- ar, are located on the oldest map of Leirvík dating from 1793, where the extent of the infield extant at the time is also indicated. It is still possible to register the extent of the heimrust of each of the three býlingar, and - as mentioned in the beginning - we have archaeological evidence that the heimrust at Toftanes was allready settled during the Viking-Age, although the Me- dieval settlement as yet eludes us. The heimrusts of the two other settle- ments - við Garð and um A, have not been subjected to archaeological excavations and we do not therefore, know how far back in time previous to 1584 AD they date. The place-name við Garð indicates though, that the settlement was established alongside the then existing infield wall - when though not known. Remains of the old infield wall can still be seen east and west of the settlement, fíg. 10. Any attempt to view the settlement re- mains at í Uppistovibeitinum in the context of settlement development must take anoth- er ruin into consideration. Some 70 m be- yond the excavation, lies the so-called Bøn- hústoft - ruin of one of the many churches or chapels abolished under the Reformation around 1540 AD. The church ruin has nev- er been investigated and it's age is therefore unknown. The ruin measuring some 9X5,5 m is encircled by a dyke built of stone and turf with a total cross section of some 25 m The site of the ruin, placed as it is within the old infield, has always aroused aston- ishment. Traditionally the site has been connected with the settlement of við Garð, which is the closest existing settlement. Al- though við Garð and Bønhústoft lie close, I am of the opinion that the stream of Brúsá acts as a distinctive and natural division be- tween the two. The question is, on the basis of the aforementioned, whether it is not far more likely to see the remains of í Uppi- stovubeitinum and the church ruin as an en- tity, allthough there are indications that oth- er settlement remains lie hidden in the area. The question of whether í Uppistovubeit- inum could be the original settlement of við Garð must also be considered. Tradition has it, that the settlement of í Uppistovubeit- inum had to move to við Garð as a result of problems with water seepage and flooding from the stream. This remains at the present a theory, however the fact is that í Uppis- tovubeitinum is entered in the land register as a beiti - that is as an area where cattle be- longing to the farm of Uppistova, of the set- tlement of við Garð, grazed. As mentioned above heimrusts were not only settlement areas reserved for building, but also included grazing areas. A logical supposition would thus be that the settle- ment of í Uppistovubeitinum lies on the site