6i 
kjokkenmodding type of axe. One class of the quartzite imple- 
ments, obtained from the laterite deposits of Madras, have the 
edge formed by bold flaking, as is the case with the kjokken- 
modding axes. 
The specimens on Tablets 14 and 15, 13 a, are flint flakes and 
cores from the shell-mound at Solager ; upon Tablet 7 Case C 
24, is a rude pounding-stone or hammer from the same 
locality. 
C 24. 
Upon Tablets 5 and 6 are flint flakes and implements from the 
shell-mound at Havelse ; 7 (5 is a rude pounding-stone from the 
same locality. The shell-mound at Havelse, on the Isefjord, is 
of small extent, and although close to the shore, is quite beyond 
the reach of the waves. It is in the form of an irregular ring, 
enclosing a space on which the ancient dwelling or dwellings 
probably stood. Upon Tablet 8 is a flint core from the shell- 
mound at Magleo. Upon Tablet 9 are some flint flakes from the 
shell -mound at Gundsomagle. Upon Tablet 10 are flint flakes 
from the shell-mound at Bilidt, on the Isefjord. Upon Tablets 1 1 
to 15 are flint flakes, cores, and rude implements from the 
coast-find" at Korsor. 
Coast-finds" of Denmark. 
"Coast-finds" are discoveries of rude flint implements, which 
are found lying in large numbers on certain spots along the old 
line of coast. They are called Kystfunden" by the Danish 
antiquaries. Owing, probably to the elevation of the land 
which has taken place in Jutland since the Stone period, some 
of these " coast-finds" are now on dry ground, and as the shore 
is very flat, the elevation, slight as it is, has in some cases been 
sufficient to separate them by a considerable distance from the 
present water-line. Some, on the other hand, are at lower 
levels ; one, for instance, close to the Railway Station at 
Korsor, is exposed only at low tide, and others are always 
covered. The coast-finds probably belong to different classes. 
Thus, one at Anholt was evidently a workshop of flint imple- 
ments, as is shown by the character of the chips, and by 
the discovery of more than sixty flint cores. Those, on the 
contrary, which even at the present day are under water, 
