5.
K.
arc z e W 8 ki
A. - M()rtodogia, strru.kt\l!."l8 itek-stura moreny dennej na obs'zllll."ze iP<llski Zachod-diej. P.OZll. Tow. iPrzyj. Nook,
t.
IV, z. 2, P02nan 1963.SUMMARY
BouJ.der clays
thaJtoccur on
the 19uI'fa.ce i.nan a~ea
between Zyr8ll'd6wam
iM61lcZlOln6w and Skierniewice belOlIllgto
lihe MJididJle Polish GilaC'iati<m. AB a rule, they I(.'()nsiBt of' sit !least ItIW10 .hori2lons sElParated with sa'll'dB aod ~ve1s, and !With s.ilt IinteTcaiations. The v8Iriation of Ibhese bouilderclays
is lOOIllBiderabily lrigb, this lbeiiing a 'l§rave hindraruce in perforrolalg a a.-igb-t ~eering-geological 1P~'iis.The al\1d;bo.r discUJS.SeB /the iPheru>mena of sedimenta-ti<m and ilaJter diilSt-\lII'Ibanc.es ial 'the Iboulder oloay1l of the area I\1nder oonsildEmlfl;ion.
6. K l' Y g 0
w
ski B. - KIDc:a sposta.-.zezefl nad war-.stwowa.niem i s.p~aniem glin morenowych. Sp.raw. !POZll. Tow. Plrzyj. Nauk.t.
XV, 1948.7. M iz e r i a W. - Z geologii oko1ic Zyu:ardoW8 i Blooia Bil\1l. PIG, 39, 11947.
PE310ME
BaJrYHBaS rmma OKPeCTHOCTeit ropO~OB :>ICHpap-~yB, MIIlOayB H CKepBeBH~e OTHOCHTCS K cpe~He nOJIhCKoMY OJIe~eHeHmO. KaK npammo, OHa COCTOHT
·H3 ~ByX roPH30HTOB, pa3~eJIeHHhIX necKaMH c rpmmeM H npOCJIOAxIWH aneBpwra. 3TH rmmhI xapaKTeP~l-3YJOTCS 6oJIbUIH'llol pa3Ho06pa3HeM, 'ITO B 3Ha'fHTeJUoao:A: Mepe 3a.TPy~H8eT npOBe~eHlHe l'H~reon01'H'lecKo:A: H !HBJKeBepHo-reonorH'IeCKo:A: o~eHKH.
.A!BTop omrehl'BaeT npo6J:teMhl CeAHMeHT~ H