y a ssito g ‘lik deb yuritiladi. Bunga O ‘rta Sibir, Braziliya yassitog‘liklari
misol b o ‘ladi (xaritadan toping). 39-rasm da turli balandlikdagi tekis
liklar, qirlar va to g ‘lar k o ‘rsatilgan.
T og‘lar ham balandligiga qarab, past, o ‘rtacha, o ‘rtacha baland
va b alan d to g ‘larga b o ‘linadi. A gar to g ‘larning b alan d lig i 500 m
dan 1000 m gacha b o ‘lsa,
p a s t to g ‘la r ; 1000 m dan 2000 m gacha
b o ‘lsa,
o ‘rtacha to g ‘lar; 2000 m dan 3000 m gacha b o ‘lsa,
o ‘rtacha baland to g ‘lar; 3000 m dan yuqori b o ‘lsa,
baland to g ‘lar deyiladi.
O ‘zbekistondagi B o ‘kantov, Tom ditov past to g ‘lar, N urota to g ‘lari
o ‘rtacha baland to g ‘lardir (X aritadan topib, nom lari va balandligini
geografiya daftaringizga yozib q o ‘ying).
B a’zan tog‘lar bir-biriga tutashib, uzoq masofalarga cho‘zilib ketgan
edurtm_uz
39-rasm.
Yer yuzasining dengiz past t0g‘
sathidan balandligiga qarab har (500-1000 m)
xil nom bilan atalishi. Qir
(200-500 m)
O ‘rtacha to g ‘
(1 0 0 0 -2 0 0 0 m)
^
Baland to g ‘
(3000 m dan
baland)
Botiq
(0 m etrdan past)
O ‘rtacha baland to g ‘
(2000-3000 m)
57 Y
E
R
N
IN
G
Q
A
T
T
IQ
Q
O
B
IG
T
—
L
IT
OSF
ERA
Y
E
R
N
IN
G
Q
A
T
T
IQ
Q
O
B
IG
T
—
LI
TOS
FER
A
b o ‘ladi. Bunday rely ef shakllari
