that in other places j Copperous fluors are mixt with Leaden 
ones:' 
Whether the Relation , communicated to the carious 
than, Kircher (as may be feen in his Mmd.Subterr. ) viz. 
that the dudius's or veins of Metals, do in thofe parts fome- 
times run North and South^ foraetimes crofs-wayes^ may be re-f 
lied on f 
To inquire into all the Baths of Baden and Hnngar'j j and 
the manner of Bathings ufed there: And particularly. Whether 
the water of the Them^^ that pafs by Schemnitz^ depofe a cer- 
tain Sediment; which in time turns into a yellow ftonel And if 
foj to fendover fome of it, 
jhefe are the ^eries*^ to which we fha/l now fnijoyn the 
Anfwers of the abov e- mention d curiot^s Travailer, as thej were 
imparted by him at feveral times ^ According as he had occa(i- 
m to inform himfelf ^ when he was in thofe Farts, dtout fuch' 
matters. 
I have not been unmindful of the Inquiries, you were 
pleas'd to honour me- with upon the accompt of the Moja( 
Society y and in Anfwer to them , I fliall firft acquaint you with 
what I found and leartfd of the Salt-Mines concerning which 
I now prefent you with thofe two kinds of T ranfyhanian Stone- 
Salts, which you mentioned 5 and alfo with Salts- ood of the 
Mine at Eperies in Upper Hungary ^ together with fome accompr 
of that Mine. 
Of the Sd GemmsAhzvt fent you four pieces, and 
ftone of Salt, as it was taken out of the Mine^ which, if you: 
pleafe , for your further fatisfaiSion, to break with an Hammer-, 
you will find itto fplit into Tables or Parallelepipedons- in your 
ha-nd. 
With thefe comes along a Specimen of that Mineral Sale 
which is commonly ufed at Table. This is found in mofl 
of the Salt-Mines , as in that of the County, of Maromarus ^ 
nigh to the Caftle of Bu(lt, and in one at Bts ^ in two zt 
For da , in two at Cdos^ in two at Szitky and in one at Bi- 
xaknd; 
