cation and the factoral analysis of the
structural accordance between elements of
the landscape by the method of the clas-
teral,correlational,regressional,factoral
informational-statistical analysis and
others).
Basic-program is composed in the opera-
tional system of MS DOS 3.3 version which
is designed for composing the colour
structural-analytical maps (complex of
Basic-program is called "GEOGRAPHICAL
EDITOR" (GEOEDIT) of the landscape struc-
ture of the place,
By means of this program of supply phy-
sico-geographical regionating of the Eas-
tern part of the Caucasis-Minor on the
basic of the structural pecularities of
the components of the geographical lan-
dscape is conducted by us. While doing it
the large-scaled geological,geomorpholo-
gical,soil,geobotanic,landscapian,hydro-
logical,topographic maps and others had
been used by us,
At first in the grid of squares with si-
de size of 5 sm. equal to 100 km^.squ-
are had been put into all maps and then
all the territory of the investigated
region was divided into 273 square 100
of which were full ones. Then for each
square above-mentioned characteristics
of the space structure of the landscape
and its components were found out and
other thorough analysis of the mathema-
tical-geographic models the physico-geo-
graphical areas of the investigated re-
gion was distributed by us. In the last
Space structural-analytical maps were
composed on the printer of personal com-
puters IBM PC AT,
EXAMPLE PROGRAM SUPPLY AND RESULT.
1.Classification Of "Landscape-Hydrolo-
gical complexes"
The function of the distance of Euclid:
N f
: Y. mM e, Md
d (X X)={2, 0x Xi)
where d(X;,X) -is the Euclide distance,
Xik -the amount of "k" changeable on the
"i" object, XjK the value of "k" changab-
le on the "j" object.
2.Program Supply.
Programming language-"FORTRAN-ST",
126
Operational system OS US 6,1 version.
-//CLUSTER JOB MSGIEVEL#(1,1),MSGCLASS=P
//KAVKAZ EXEC FORTGCLG,PARM.FORT=SOURCE
//FORT.SYSPRINT DD SYSOUT zP
//FORT.SYSIN DD *
C NABIYEV ALIPASHA ALIBEK
DIMENSION X(200,200),8(200,200)
READ(5,4)N,M
PRINT 4,N,M
4 FORMAT(2I3)
DO 5 1=1,N
READ(5,6) (X(1,J) ,J24,M)
WRITE (6,6) (X(I,J),J=1,M)
6 FORMAT(10F8.2)
S CONTINUE
AN=N
DO 100 I=1,M
DO 100 J=1,M
RASTOzO,
DO 50 K=1,N
RAS TO=RASTO+(X(K,1)-X(K,J))**2
50 CONTINUE
S(I,J)sSQRT(RASTO/AN)
100 CONTINUE
STOP
END
/*
//LKED,.SYSPRINT DD SYSOUT-P
//G60.FT96F001 DD SYSOWT=P
//GO.SYSIN DD *
******Landscape - Hydrolozival data*****+
//
RESULT
The Classificational map of the River fustens aoconding to the
similarity sf the Hydralagisal data -Rivers Caucasi Minor
?
-
"-
MeAsune e -
Classification Level similarity acxi X J2-90(7043,
Hamer River Systems: i.Janjachai-v.Euranpad-à Curakuhai=v.Dosular
DUpranchai-v.Jukhari-AgJakend.4.Tartar-v.Madagiz.3.Khachinohai
pM TVAAHSITUHDD ASH ATH HmHad vA» mn T.Gondt ai - -—
Cusuchai-u.Tuag,9.Atagust-u.Tug.10.Hekaniohal nn NY rA TE 8:
n
A
11.Zabukhohai-v.Zabukh and others, haaHer,
The Classificational map af the River systems according to the
similarity of the landscapes somlexes data -Rivers Causasis Minor
Trot
The measures Euslide distance: OMiJ-0 SUMCHIE-X jEO««2)2«1/2
Classification level zimilarity diXi.X,psiSO(CTÓX)
Hame River systeus: LJanjaohal —wZurnahbad,Z.Gurakohal-v.Dozu-
lar,3.Jpranohai-u.Iukhari-Agjakend,4.Tantar-v.Madagiz,
JT.Khaohinohai-v.Uanolu,6.Caroanohai-v.AsKenan
f cL c 9, 009 ——
I.
p—— d I RP int AN fam]
