Volltext Seite (XML)
- 1 Saxon •ERz'GBH'iR'&BiiTKI 73 partly broken,’ partly unbroken..i: .Hereil are ^Por phyry, Sienite, newer Gi^nite,VQuartzi,'IandiSfir-‘ pentine.d: Still lower’downl we..meeb;with! T/an- litionHRooks, ofdwhich; the Limeftoiae appears at Kalk-grun and t Wildenfels; u 'the Amygdaloid < in Voightland, and tlie Grey-wacke ancl^Gtiey^wacke Hate at Braunfdorf near FrdybergJudSclll 'ddvVe'r dbvyfidand often covering; the-'preceding dforma- tions; we find Sandllone and Lime dono ¥ a hd' dn de- veral'^lace< : as'at fHainchen; JPotchappeln nefir Drfefdertdand: Xwiekaw,: there ar$; depatftiori&dof the Cbfll 'for'matmnii -Daftly; T lie - 5SJ e rv trap'formation cbv*trai£f the othev&,--ift tttfeottd form able; overly iiig abd Very brdkendtratificatidrt; ; 'i-> it: -ft r»h;n:y*‘i ; ;) b)lBiiiinot»b noacf :c; n.^a r ' ' ‘nP .odolg !' :i i b'jhfUiidii .. od Joniii,. '-nni-iml nii(i;H .lit 'lo flirm crti 03 OHAP. JV.' e;b--a bloi't 'lo yri,: o^idqlih v iil'dnhnn ’'mm ~ r l -.rl ton ; odol?, THEORY OF THE DILUTION OF .THE WA-TEgS (>£ . THE GLOBE. DESCRIPTION OF OVERLYING FOR- i) J T v. *. MATIONS.—AN INVESTIGATION OF THE C0N- TENtS OF THE ORIGLN AL W. A T ElR S1QF jlTHEi iQ I OB E ■'DOR 1 NO THE DIFFERENT PERIODS-OF-THE EAK'Eldd FORMATION.—IrHE'DIVISION^F'ttcrCKS-INTO-' PiVB - W GkfeA'¥ , cLkssE^ i;i “' / 1!h/ * him avid oj 1 , ,.j-:,b!ln<r.> y'r - bid iisintnq'tkl sits «UJ •ij«! i u:; 1 !;ij;:i j: iti j» . .. Ajc.i' iiibioisrfq; o;!l f>crf 43*'- rT F , WEj fphcroida} figM^oL^b^WMb t\ sftJL proof obits original 11 aid 1 tyu io.• This.iRife portant conclufion was" never difpiuted:^ 'thisdoniy Vol. Ill- K- queftion