SUMMARY
" Engineering-geological characteristics of slope zo--nes':8'hould give more attention, than has· been given
previously, to both differentiation of heterogeneous deposits of these zones 'and the processes modelling them. Three groups of processes: su:rface mass
move-ments,
downwash, and gully erosion are distinguished(Table). The gro\lps of deposits corresponding to these processes include: colluvia, deluvia, and proluvla,
·respectively. The deposits markedly differ in geolo-'gieal and physico-mechanical properties; this diffe-.rentiation is of ,remarkable imporhnce for evalua-tion of slope stability in geological-engineering sur-veys and in mapping. The above mainly applies to the colluvia and deluvia representing groups of slope
'depOsits; the typical features of which are not yet
,dearly defined. Basic c;riteria for identification and classification of the groups and ty'pes of slope depo-sits are given.
PE310ME
'B 'HHzeHepHo-reonOrH'leCJtMX OQeHKax CKJIOnOInoIX 30H He0«5XO~mlO B I5olIhwe1li CTl'neHH Y'lHThIB8"I'i,
pu-HOo~p83Me cnaraw~x MX Oca~OB pa3Horo reHe3HCa 'B YU3Ke c npou:eCCaMH Oca.I{KOO~P330BaHJUI. l" npe~ nozeHHoA KnaccM<I>HJtaQHH (T86n. 1) pa3.nwlaJOTCH TPK OCHOBHhlX rpynnhl CKJlOHOBhlX oca~KOB - KOJlJlWBJdi. ~eJIroBH:R M npOJIroBWl:, Upe.l\CTaBJlIIWIu:HC rIpO,uYKTh! TIpoIlBJleHHn onpe~eJleHHhlX TIpoQeCCOB, COOTBeTCTlIell-HO: nOBepXHOCTHoro ABmKeHHn MaCC, CMhIBQ- H OBpa1K-HoA Sp03MM. nepe'fHCne:'U!hle THnbl OCR,IUtOD CYIu:e-CTBeHHhIM otipa30M OTJlJAalOTCH ~yr OT ,!!;pyre CBOmm reonorH'leClOOlJ{ M <l>H3KKO-MeXaHH'leCKHMH cooAC'I"Ba-MM. B CBH3H C STMM OUK no-pa3HOMy JlJlHllWT Ha YCToA'IHBOCThCKnOHOB. l:£t'TKoe pa3rpaHM'IeHHe 01'-l!enhHhIX rpynn Oca.I{KOB ~onzHO npoH3RO;rutTbCII B DPOu:ecce reonorH'leCKoA I:'bt'MKM. B paeioTe ~8IOTCJI OCHoBHhle KpMTepMM onpe,ueneHHII YKa3aHHhlx rpynn M THIlOB CKn()HOBh~X OCa,llKOB.