This GMN report does not table the stream sediment analyses...

This GMN report does not table the stream sediment analyses (IMHO it should). But it seems that the measured Li value can be inferred by map colouration adjacent to the sample site. The map colours are otherwise of obscure origin. It is surprising that sampling sites downstream of a "find" do not have “shows”.

The map above locates the observed pegmatite outcrops (white) over the stream sampling sites (black diamonds).
The map also shows the 260m and 270m elevation contours. The contours show the location of "escarpments", and the "valleys".

IMO the geophysics shows that there are two parallel "spod parent rock" trends running SW-NE through the tenements.
The southern (and stronger) trend of the two runs near and to the south of the feldspar mine marked in Figure 1 (pg 2).
(The mine is about 5km NE of the pegmatite swarm in the NE corner of the GMN tenement) (-6.61839,-36.72882).
A very significant "hot" spot in that trend appears about 2km NW of the SE Corner of the GMN tenement.
A further 1km NW from that spot leads into the mapped field of peg outcrops and strong Li stream sediment shows.

Looking forward to seeing the rock chips assays/photos.