DISTIRCT SURVEY REPORT
DISTRICT UJJAIN
MADHYA PRADESH
DIRECTORATE OF GEOLOGY AND MINING
MADHYA PRADESH BHOPAL (M.P
1. INTRODUCTION
The present report is prepared in the light of notification no. S.O. 141(E) New Delhi, the
15th January, 2016 of MINISTRY OF ENVIRONMENT, FOREST AND CLIMATE
CHANGE. This will a model and guiding document, which is compendium of available
mineral resources, geographical set up, environmental and ecological set up of the district
and replenishment of minerals. River channels and their floodplains are important sources
of construction grade aggregate materials like sand and gravel. The durability of river-
borne coarser clastics (e.g. sand and gravel) and their sorting by fluvial action make them
best suitable raw materials / ingredients for building constructions. Most of the rivers in the
world are overexploited for living and non-living resources and today the challenge posed
to the society is to restore its natural ecology. As transportation and construction
infrastructure expanded since the mid-twentieth century, the demand for construction
grade sand also increased exponentially. The market demand of river sand is high
throughout the world and Madhya Pradesh is not an exception. Ujjain district is situated in
the north- western part of Madhya Pradesh. Ujjain district occupy an area of about 6080
sq. km. and is bounded by latitudes 22° 49' 45" to 23°45' 25" N and longitudes 75°08' 05"
to 76° 15' 20" E. The district is bounded by Ratlam and Shajapur in the north, Dewas in
the east, Indore and Dhar in the south and Ratlam in the west. The shape of the district is
pentagonal with eastern projection resembling the neck of a tortoise. The district is divided
into seven tahsils. Ujjain is ancient city and it is cosmopolitan. The district headquarter is
also an important railways junction. It is well connected by road and rails by other places
of the country and in the state. Nagda-Ujjain branch, Indore-Dewas-Ujjain branch, Ujjain-
Bhopal broad gauge line and Khandwa –Ratlam, meter gauge line of the western railway
are the rail links passing through Ujjain. Mehidpur, Khachrod, Barnagar and Tarana are
some os the important towns in the district that are connected by state high ways. National
highway No. 3 passes through the eastern part of the district. Ujjain is an ancient town
celebrated for the Mahakaleshwar temple located on the banks of Kshipra.
2. OVERVIEW OF MINING ACTIVITY IN THE DISTRICT
Land and water are the basic aspects of development of any economy. Economic
development is the output of development of these natural resources in a sustainable
manner. District is well endowed with fabulous amount of building material like sand,stone
and murram. In all a sum total of 454 leases, including 199 quarry lease and 255 auction
quarry with a sum total of 963.231 hectare area, which is 0.015% of the area of the district,
have been sanctioned in the Ujjain district of M.P. and fetches 7.722 crores of revenue
during 2014-15.
3. THE LIST OF MINING LEASES IN THE DISTRICT WITH LOCATION AREA AND PERIOD OF VALIDITY
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06-07
29-05-08
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28-05-18
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28 jes'k firk ckcqyky xks;y
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36 Jh vfer firk
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37 Jh nsosanz firk /kjepanz
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09-04-20
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03-10
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21-04-20
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10-05-10
09-05-20
43 Jh vtqZuflag firk
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rglhy o ftyk mTtSu
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rglhy o ftyk mTtSu
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02-11-21
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panw[ksM+h] rglhy o ftyk
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09-05-12
08-05-17
53 Jh fnus'k firk enuyky
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107 iVsy uxj mTtSu
iRFkj 308 1.000 xqukbZ [kkylk 1189@11-
09-13
24-05-14
23-05-24
54 Jh v{k;dqekj firk
fnyhi dqekj tSu
fuoklh&30 {ki.kd ekxZ
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iRFkj 203 1.600 lqjtuoklk 1334@01-
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07-08-24
55 Jh fl)ukFk firk izHkqyky
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fuoklh&uede.Mh mTtSu
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24-05-14
23-05-24
56 Jh bnfj'k firk vCnqy
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eafty nsokl jksM mTtsu
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57 Jh nsosUnz firk tlaorflag
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59 Jh lanhidqekj firk
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1.000 pdt;jkeiqj 2157@16-
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07-08-24
60 Jh thou firk Hks:yky
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61 Jh jktsUnzflag firk
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fuoklh&xzke eaxjksy iksLV
fprkea.k tokfl;k rg- o
ftyk mTtSu
iRFkj 298 1.000 tyky[ksM+h 1235/18-
01-13
28-02-14
27-02-24
62 Jh pUnzs'k firk
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fuoklh&esgs'k fogkj
dkWyksuh mTtSu
iRFkj 311 4.000 xqukbZ [kkylk Mhth,e
18500&50
3
04-10-13
03-11-14
02-11-24
63 Jh lat; firk izrki
esgrk fuoklh&40
egk'osrk uxj mTtsu
iRFkj 159 4.000 xqukbZ [kkylk 1724
19-08-2016
30-08-
2016
29-08-
2026
64 Jhefr oanuk ifr ujs'k
dsu fuoklh& esudkiqjk
rglhy iksjlk ftyk
eqjSuk
vraj.k Jh lat; firk
ckcwyky pkS/kjh fu&xzke
dslwuh rg- o ftyk
mTtSu
iRFkj 203 2.000 lqjtuoklk 729
22-10-2014
25-04-15
24-04-25
65 Jh jQhd firk jgeku
vyh fuoklh& okM ua- 8
bankSj jksM lkaosj ftyk
bUnkSj
eqje 620 3.000 C;kojk 1088
19-03-2015
26-06-15
25-06-25
66 Jh ukjk;.k firk iwuepan
;kno fuoklh&180
vCnkyiqjk mTtSu
eqje 325,326 3.960 ekuiqjk 1028
05-03-15
22-05-15
21-05-25
67 Jh ukjk;.k firk iwuepan
;kno fuoklh&180
vCnkyiqjk mTtSu
eqje 328 2.100 ekuiqjk 1029
05-03-15
22-05-15
21-05-25
68 Jherh lkxj ifr
cgknqjflag fllkSfn;k
fuoklh xzke dslquh iksLV
ck<dqEesn r-mTtSu
iRFkj 148
171
182/2
1.920 pdt;jkeiqj 214
11-06-14
08-08-14
07-08-24
69 Jhefr vk'kk ifr lat;
esgrk fuoklh&40
egk'osrk uxj mTtSu
iRFkj 236 4.000 ck<dqEesn 584
27-09-14
05-12-14
04-12-24
70 Jh lat; firk izrki
esgrk fuoklh&40
egk'osrk uxj mTtsu
iRFkj 236 4.000 ck<dqEesn 585
27-09-14
05-12-14
04-12-24
71 Jh nsosUnz firk tlaorflag
fuoklh&fiiyksnk
}kjdk/kh'k mTtSu
iRFkj 198 199 1.910 ek/kksiqj 2778&79
30-10-2015
05-11-15
04-11-25
72 fot; firk nsoukjk;.k
tkV fu- xzke dslquh rg-
o ftyk mTtSu
iRFkj 134
135
1.000 lqjtuoklk 3067@26-
11-15
05-02-16
ls 04-02-
26
73 iwuepan firk xsankyky
ifjgkj] fu- 17 lqnkek
uxj mTtSu
iRFkj 205] 2.400 fiiY;k fcNk Mh-th-,e
133&135
@05-01-16
29-02-
2016
28-02-
2026
74 fgesUnzflag firk
f'koukjk;.kflag pansy] fu-
&34 cgknqjxat nzfoM
ekxZ xyh uacj 2 mTtSu
iRFkj 174 4.000 tEcwjk Mh-th-,e
129&131
@05-01-17
02-04-
2016
01-04-
2026
75 dsljflag firk jkes'oj
iVsy] fu0&101@2 nqxkZ
dkyksuh mTtSu
iRFkj 205 2.25 fiiY;kfcNk 3142@
05-12-15
09-03-
2016
08-03-
2026
76 vkj-ts-baVjzizkbtsl ikVZuj
_f"k firk jktho
JhokLro] fu-,y-th- 39
ch-lh-,e-fot; uxj bankSj
iRFkj 159 1.600 xqubZ[kkylk 2804@
31-10-2015
27-07-
2016
26-07-
2026
77 Jh y{ehukjk;.k firk
ujcrfalag /kuxj
fuoklh&HkkxZo ekxZ mTtSu
eqje 159 4.000 xqubZ[kkylk 1072
27-05-2016
30-07-
2016
29-08-
2025
78 'kqHke firk ?ku';ke 'kekZ
fuoklh&47@1 eaxy
m?kku xyh ua- 4
vaofriqjk mTtSu
iRFkj 639 2.000 rktiqj 6280&81
21-04-2016
Mh-th-,e
28-06-
2016
27-06-
2026
79 Jh egsUnz firk ?ku';ke
jkBkSj fuoklh&34 [kkjh
ckoMh nsokl
eqje 850 4.000 C;kojk 1393
13-05-2013
08@06@
2016
07@06@
2026
80 Jh jfoUnz firk jktsUnz
tkV fuoklh&xzke
gDdkuhiqjk rg- o ftyk
mTtSu
iRFkj 323 1.000 ugkfj;k 2219
23-11-16
26-12-16
25-12-
2026
81 Jh lqjs'k firk ckcwfalg
HkkfV;k fuoklh&jsYos
LVs'ku xzke vlykonk
iRFkj 129
132
0.930 pdt;jkiqj 1663
31-12-2007
30-06-
2008
29-06-
2018
rglhy&?kfÍ;k
1 egkdky LVksu Øs'kj
izks- lR;ukjk;.k firk
lksguyky vxzoky
fu- 75 is-lh-feYl
daikm.M vkxj jksM]
mTtSu
iRFkj 1210 2.20 utjiqj 670@11-
10-13
08-01-12
07-01-22
2 tqcsj [kku firk clhj
[kku
fuoklh 59] jkeizlkn
HkkxZo ekxZ] mTtSu
iRFkj 675
(675/2)
2.000 utjiqj 696@23-
05-07
18-06-07
17-06-17
3 jruflag firk jkeflag
nsiu
fuoklh xzke lksMax
rglhy ?kfV~V;k
iRFkj 665 1.500 utjiqj 1561@20-
11-07
01-12-07
31-11-17
4 fxjh'k firk lR;ukjk;.k
pkSgku
fuoklh 11 'kkarhukFk dh
xyh] NksVk ljkQk] mTtSu
varj.k
bdcky firk ljnkj [kku]
fuoklh&<kcyk gnwZ]
rglhy rjkuk
iRFkj 1210 / 1 1.000 utjiqj 185@19-
05-08
01-01-09
31-08-19
5 vk'kh"k firk clUr dqekj
ik.Ms;
fuoklh lh&35@10]
_f"kuxj] mTtSu
iRFkj 804 0.400 ?kfVV~;k 321@09-
06-08
25-0908
24-09-18
6 'kknhd firk eksgEen
'kQh
fuoklh pan dk dqavk]
mTtSu
iRFkj 1109/2 2.000 utjiqj 495@18-
07-08
15-07-8
14-07-18
7 vk'kh"k firk clUr dqekj
ik.Ms;
fuoklh lh&35@10]
_f"kuxj] mTtSu
iRFkj 945 la'kksf/kr
942
4.000 ?kfVV~;k 874@17-
07-09
01-01-09-
31-08-19
8 iou firk eqjyheuksgj
,sju
fuoklh 60 fo|kifruxj]
ukuk[ksM+k] mTtSu
iRFkj 665 2.000 utjiqj 9@01-01-
09
05-1-09
31-12-19
9 lqfer firk fnyhi vkuan
fuoklh 7@1] , lsDVj
egkuankuxj mTtSu
iRFkj 1210/1 0.800 utjiqj 10@01-01-
09
05-01-09
04-01-19
10 eukst firk f'konRr 'kekZ
fuoklh 90] laruxj]
mTtSu
iRFkj 23 2.330 ds'kjiqj 13@01-01-
09
05-01-09
04-01-19
11 jktkjke firk Hksjkth
cykbZ
fuoklh xzke dkfy;knsg
rslgy ?kfê;k
iRFkj 665 1.500 utjiqj 313@20-
02-09
28-05-09
27-05-19
12 Jherh laxhrk ifr
jfoanzflag HknkSfj;k]
fuoklh&7@8] egkdky
okf.kT; dsanz] ukuk[ksM+k]
mTtSu
iRFkj 675 3.700 utjiqj 663@06-
06-09
10-07-09
09-07-19
13 Jh v'kksd firk Hkkxey
tSu]
fuoklh&33] [kkjkdq¡vk]
mTtSu
iRFkj 144/1
159/1160
161/1 162
1.000 HknsM+e;pd 1001@03-
08-09
16-10-09
15-10-19
14 Jherh iq"ik ifr MkW-
?ku';ke 'kekZ]
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m|ku] xyh ua- 4]
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iRFkj 1109 2.000 utjiqj 1064@24-
05-2011
22-06-11
21-06-16
15 Jh jkds'k firk t;jke
ijekj fuoklh&t;jkeiqj
rg- ?kfÍ;k ftyk mTtSu
varj.k
fQjkst firk vCnqy j'khn
fu&xzke utjiqj mTtSu
iRFkj 945 1.000 ?kfVV~;k 2165@20-
01-14
12-02-14
27-2-24
16 Jh euh"k firk xksiky
ikVhnkj fuoklh&esu jksM
?kfÍ;k rg- efgniqj
iRFkj 944 1.000 ?kfVV~;k 2160@17-
01-14
18-02-14
17-2-24
17 Jh nylq[k firk ukjk;.k
HkkbZ iVsy fuoklh&16 ,
vjfoUn uxj vkxj jksM
mTtSu
iRFkj 313/1 1.000 ?kfVV~;k 2095@08-
01-14
23-01-14
22-01-24
18 Jh xksiky firk x.kir
vkatuk fuoklh&bUnzkuxj
mTtSu
eqje 564 2-000
vkteiqjk 'kk[kk&1@
30
31-05-14
14-06-14
13-06-24
19 Jhefr vatfy ifr nsosUnz
ikVuh fuoklh&106 xkSre
eksxZ mTtSu
iRFkj 1/min-1 3.000 fouk;xk 714@20-
10-14
17-11-14
16-11-24
20 Jh t;flag firk
bZ'ojflag jktir
fuoklh&xzke tsFky rg-
?kfÍ;k
iRFkj 1035 2.000 ?kfVV~;k 1891@24-
12-13
24-01-14
23-01-24
21 Jh fnus'k firk enuyky
iztkir fuoklh&xzke
fuukSjk rg- mTtSu
iRFkj 82 1.000 ?kfVV~;k 1968@26-
12-13
23-01-14-
22-01-24
22 Jh yksdsUnzflag firk
xtjktflag fllkSfn;k
fuoklh&xzke rqykgsMk rg-
?kfÍ;k ftyk mTtSu
varj.k
fQjkst firk vCnqy j'khn
fu&xzke utjiqj mTtSu
iRFkj 944 1.000 ?kfVV~;k 2352@21-
02-14
29-07-14
28-07-24
23 Jh lR;ukjk;.k firk
lksguyky vxzoky
fuoklh&82 vjfoan uxj
mTtSu
iRFkj 145 3.000 <kcykxkSjh 'kk[kk&1@
8
24-05-14
14-06-14
13-06-24
24 Jh cgknqj firk vEckjke
pkS/kjh fuoklh&xzke
jkrfM;k rg- ?kfÍ;k
eqje 327 3.000 jkrfM;k 'kk[kk
1@64
17-06-14
01-07-14
30-06-24
25 Jh ujsUnzflag firk
bZ'ojflag lksaydh
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rglhy ?kfÍ;k
iRFkj 82,83,84 1.000 ?kfVV~;k 'kk[kk 235
25-07-14
08-08-14
07-08-24
26 Jh lqjs'k firk eksguyky
ckjksM fuoklh&xzke jk?koh
rglhy efgniqj mTtsu
eqje 564 2.000 vkteiqjk 1638
09-06-15
12-07-15
11-07-25
27 Jh gVsflag firk jruflag
fuoklh&xzke xqubZ[kkylk
rg- o ftyk mTtSu
iRFkj 562 3.000 :nkgsMk 2428
11-09-2015
27-06-
2016
26-06-
2026
28 Hkxokunkl firk vejkth]
fu- 28 tkalkiqjk mTtSu
feÍh 247@1 3.880 xksalk 23@05-01-
16
03-02-16
ls
02-02-26
29 jkepanz firk lksekth
iztkir] fu-&28 tkalkiqjk
mTtSu
feÍh 246@2 1.440 xksalk 25@05-01-
2016
03-02-16
ls
02-02-26
30 'kch glu firk eks-
gqlSu] fu- U;qw gfjQkVd
mTtSu
iRFkj 1@fe&1 4.000 fouk;xk Mhth,e
2281&83
08-02-2016
11-05-16
10-05-26
31 ftrsUnz firk yYykflag
rksej] fu-21 jktsUnz uxj
vkxj jksM mTtSu
eqje 556 2.000 vkteiqjk 350
24-02-2016
22-06-
2016
21-06-
2026
32 jktsUnzflag firk
lR;ukjk;.kflag
fuoklh&xzzke ukansM rg-
rjkuk
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foDdh firk dey pkSgku
fu&,@9@11 egkdky
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mTtSu
eqje 1@fe&1 2.000 fouk;xk 3149
26-02-2016
21-07-
2016
20-07-
2026
33 Jh /kesZUnz firk euksgjyky
esgrk fu&53 dey
dkWyksuh vadikr ekxZ
mTtSu
iRFkj 145 2.000 <kcykxksjh 1669
12-08-2016
07-09-
2016
06-09-
2026
34 Jh /kesZUnz firk euksgjyky
esgrk fu&53 dey
dkWyksuh vadikr ekxZ
mTtSu
iRFkj 145 2.000 <kcykxksjh 1671
12-08-2016
07-09-
2016
06-09-
2026
35 Jh izrhd firk v'kksd
rksej fuoklh&5 ,evkbZth
y{eh uxj mTtSu
iRFkj 145 2.000 <kcykxksjh 2479
29-12-2016
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36 Jh izrhd firk v'kksd
rksej fuoklh&5 ,evkbZth
y{eh uxj mTtSu
iRFkj 145 2.000 <kcykxksjh 2481
29-12-2016
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37 Jh fnid firk jes'kpUnz
xqIrk fuoklh&lqHkk"k uxj
eqjSuk
iRFkj 1@fe&1 4.000 fouk;xk 02
02-01-2017
12-01-
2017
11-01-
2027
73.750
rglhy rjkuk
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tSu]
fuoklh dapuiqjk LVs'ku
jksM] 'kktkiqj
iRFkj 1508 2.000 cj.Mok 445@29-
03-10
07-02-11
06-02-21
2 Jh lksuiky flag firk
nqysflag pkSgku
fuoklh <kcyk jktiwr iks-
:ik[ksM+h rsglhy rjkuk
iRFkj 156 /2 0.700 ykyk[ksM+h 1489@14-
12-06
02-01-07
01-01-17
3 Jh /kesZUnz izrkiflag firk
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iRFkj 44 2.000 usukon 589@07-
05-07
11-04-07
10-04-17
4 xtsUnzflag firk dj.kflag
rksej
fuoklh 86] fot;uxj
'kktkiqj
iRFkj 44, 54 3.000 usukon s937@30-
06-07
05-07-07
04-07-17
5 Jherh uhykJh ifr eqds'k
xxZ
fuoklh u;kcktkj eDlh
iRFkj 494 0.800 dukfl;k 1536@14-
11-09
26-11-07
25-11-17
6 xkso/kZuflag firk jruflag
fuoklh 10 ubZokM+k]
'kktkiqj
iRFkj 54 2.000 usukon 1537@14-
11-07
16-11-07
15-11-17
7 gseUr firk 'kadjyky xxZ
fuoklh u;kcktkj eDlh
varj.k
d- Jqfr firk eqds'k xxZ]
fuoklh&>.Mk pkSd] eDlh
iRFkj 1414 2.100 cj.Mok 1109@03-
09-09
01-12-07
30-11-17
8 jk?kosUnz firk Jh
irukjk;.k falg
fuoklh ubZ vkcknh eDlh
iRFkj 1508/2
1508/4
3.000 cj.Mok 1558@20-
11-07
01-12-07
30-11-17
9 vfEcdk fLVksu Øslj
izksizk;Vj egsUnz firk
dkarhyky tSu fu-25]
Hkalkyh eksgYyk 'kktkiqj]
vUrj.k Jh —".kk xzqi
ikVZuj lat; firk Lo-Jh
gjhckcq frokjh] fuoklh&
lqHkk"k dkWyksuh] tSu eafnj
ds lkeus] xquk gk-eq-LVs'ku
jksM /kksch pkSjkgk] 'kktkiqj
iRFkj 35 3.000 ;'koaruxj 1855@05-
02-08
28-02-08
27-02-18
10 iq"isUnzflag firk mn;flag
fuoklh cl LVs.M dk;Fkk
rg-rjkuk
iRFkj 3 0.410 eksyxk 1877@13-
02-08
29-02-08
28-02-18
11 jQhd vgen firk
xQ~Q`j vgen fln~nhdh
fuoklh ubZ vkcknh eDlh
iRFkj 158 1.000 yqfu;k[ksM+h 1870@15-
02-08
27-02-08
26-02-18
12 'kSysUnz firk v'kksd tSu
fuoklh 27] lqHkk"k ekxZ]
rjkuk
iRFkj 1309 3.000 ukansM+ 146@05-
01-09
06-01-09
05-01-19
13 uosn v[rj eso firk
elwn v[rj eso]
fuoklh&vkokl uxj]
nsokl
iRFkj 1/2/3 4.000 drokfj;k 836@09-
07-09
27-07-09
26-07-19
14 eSllZ flag cznlZ]
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fuoklh&xk;=h fogkj
dkWyksuh] fiUVks ikdZ]
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iRFkj 165 1.750 catkjh 1213@05-
01-09
16-10-09
15-10-19
15 jk?kosUnz firk Jh
irukjk;.k falg
fuoklh ubZ vkcknh eDlh
iRFkj 79/2 2.000 cj.Mok 278@25-
02-10
21-04-10
20-04-20
16 egsUnzflag firk
HkkxhjFkflag]
fuoklh&xzke jkeM+h]
rglhy rjkuk] ftyk
mTtSu
iRFkj 48 2.000 ;'koaruxj 968@01-
07-10
01-09-10
30-08-20
17 Jh ukjk;.k firk
xkSjh'kadj uk;d
fuoklh&;'koar uxj]
iksLV uSukon] rglhy
rjkuk ftyk mTtsu
iRFkj 141 2.000 ;'koaruxj 3265@14-
11-11
30-11-11
29-11-16
18 Jh uohu firk v'kksd
dqekj tSu fuoklh&27
lqHkk"k ekxZ rjkuk
iRFkj 1325 4.000 ukansM+ 'kk[kk&1@
27
25-06-14
08-08-14
07-08-24
19 Jh v'kksd firk
dUgS;kyky lksaydh
fuoklh&9@6 iqjkuk
gWfLiVy jksM tkojk
iRFkj 85 3.000 xka/khuxj 1621
04-03-15
20-03-15
19-03-25
20 Jh vfuy firk
jkeykyth pkSgku
fuoklh&lqHkk"k pkSd
ekdMksu
iRFkj 2 2.000 xka/khuxj 1031
05-03-15
27-06-15
26-06-25
21 Jh xksfoUnz firk
ukjk;.kfalg fuoklh&28
dss'kouxj mTtSu
iRFkj 1309 2.000 ukansM+ 1666
16-06-15
26-06-15
25-06-25
22 Jh eqds'k firk jksMey
jkBksj fuoklh&ch&5
vatwJh ifjlj nsokl jksM
mTtSu
iRFkj 247/495 2.000 fiiY;kcktk
j
1274
01-05-15
11-05-15
10-05-25
23 Jh izHkqyky firk nqxkZth
xkSM fuokl&xzke
ykydyko ikssLV dMkfn;k
rjkuk ftyk mTtsu
iRFkj 1704 1.000 dMksfn;k 1286
05-05-15
23-05-15
22-05-25
24 Jh jkts'k firk
dSyk'kpUnz ikVhnkj
fuoklh&xzke bVkok
rglhy rjkuk ftyk
mTtSu
iRFkj 1313
1324
1.000 ukansM+ 2619&20
08-10-2015
13-10-15
12-10-25
25 egsUnzflag firk
HkkxhjFkflag] fu- xzke
jkeMh rg- rjkuk
iRFkj 48 2.000 ;'korauxj 2207@
22-08-2015
10-03-16
09-03-26
26 jkts'k firk dSyk'kpanz
ikVhnkj] fu-xzke bVkok
rg- rjkuk
iRFkj 1309 2.000 ukansM 3148@
07-12-2015
28-02-16
27-02-26
27 Jh ftrsUnz firk HkkxhjFk
ijekj fuoklh&2@1
utjvyh ekxZ mTtSu
iRFkj 1325 1.500 ukansM 2132
02-11-16
13-12-
2016
12-12-
2026
55.260
rglhy&ukxnk&[kkpjkSn
1 ferss'k dqekj firk lqjs'k
dqekj tSu
fuoklh cq) ekxZ [kkpjkSn
iRFkj 574@2 2..000 fpjksyk 1062@
25-05-16
14-07-
2016
13-07-
2026
2 Jherh lqfurk ifr
lw;Zizdk'k 'kekZ
fuoklh 90 lqHkk"k ekxZ]
[kkpjkSn
iRFkj 602/3 2.000 dqEgkjokM+h 1998@18-
03-08
25-03-08
24-03-18
3 ikVokyk feujYlZ ,.M
ekbZUl izk-fy-]
Mk;jsDVj jkgwy ikVokyk]
fuoklh&72] lq[kfuokl]
jkm] jaxoklk] bankSj
iRFkj 262/3 2.000 csM+koU;k 216@06-
02-10
19-02-10
18-02-20
4 ikVokyk feujYlZ ,.M
ekbZUl izk-fy-]
Mk;jsDVj jkgwy ikVokyk]
fuoklh&72] lq[kfuokl]
jkm] jaxoklk] bankSj
iRFkj 261/1 4.000 csM+koU;k 217
06-02-10
18-02-10
17-02-20
5 eukst firk f'konu 'kekZ
fuoklh 37] equhuxj]
mTtSu
iRFkj 505 1.000 ipyklh 695@23-
05-07
07-06-08
06-06-18
6 fot; firk y{ehukjk;.k
laxhryk fuoklh&9 foØe
ekxZ mTtSu njoktk
[kkpjkSn
iRFkj 185 0.800 ipyklh 23@03-01-
09
07-01-09
06-01-19
7 vkseizdk'k firk
y{ehukjk;.k laxhyky
fuoklh&9 foØe ekxZ
[kkpjkSn
iRFkj 946/2,947 1.320 cqjkukckn 700@08-
06-09
29-06-09
28-06-19
8 jes'k firk jruyky
ukansM+k
fuoklh LVs'ku jksM mUgsy
iRFkj 356 1.500 vkD;k
uthd
12@01-01-
09
09-06-09
08-06-19
9 Jh lfpu firk Jh
izdk'kpUnz ikVuh fuoklh
NksVk cktkj mUgsy ftyk
mTtSu
iRFkj 508 1.00 vkD;k
uthd
1281@9-
11-06
31-10-06
30-10-16
10 Jherh lhrkckbZ ifr
j.kNksMyky
fu- cSMkou rg- ukxnk
iRFkj 54,
59
1.33 ekyh[ksM+h 54@13-01-
04
259@30-
07-14
10-03-14
09-03-24
11 f'kojktflag firk
ukjk;.kflag
fuoklh fcjykxzke ukxnk
iRFkj 240 0.88 esgrokl 931@18-
11-04
2093@
07-08-15
24-12-04
23-12-14
12 y{eh LVksu Øs'kj Jherh
y{eh nsoh ifr clar
j?koa'kh fuoklh 1] lqHkk"k
ekxZ xyh ua-1 ukxnk
iRFkj 608 2.000 :isVk 1486@14-
12-06
20-12-06
19-12-16
13 dey firk rkjkpUnz
;kno
fuoklh 8@5] ,yvkbZth
_f"kuxj] mTtSu
iRFkj 356/2 2.000 vkD;k
uthd
233@20-
02-07
29-03-07
28-03-17
14 ckyfd'ku firk
teukyky nkl HkkfV;k
fuoklh fpfdRlky; ekxZ
ukxnk
iRFkj 550,
552
2.000 dpukfj;k 671@16-
05-07
23-05-07
22-05-17
15 lfpu firk izdk'k ikVuh
fuoklh NksVk cktkj
mUgsay
iRFkj 76 2.000 vkD;k
uthd
724@30-
05-07
18-06-07
17-06-17
16 x.kss'k LVksj Øs'kj
izksizk;Vj Jherh iq"ik ifr
iadt tSu fuoklh tokgj
ekxZ] ukxnk
iRFkj 518/3 1.000 >ka>k[ksM+h 1634@20-
12-07
18-01-08
17-01-18
17 Jh /kesZ'k firk psruLo:Ik
tk;loky
fuoklh 32] egkRek xka/kh
ekxZ] ukxnk
iRFkj 431,
432,
433
1.000 vthekckn
ikjnh
1853@05-
02-08
08-02-08
07-2-18
18 Jh ujsUnzflag firk
lq[kjkeflag
fuoklh&uk;u
varj.k Jh fnus'k firk
nqxkZyky <ksMfj;k
fuoklh&133 mTtSu
njoktk [kkpjkSn
iRFkj 1150,
1156,
1157,
1158,
1159
1.000 Hkhdeiqj 1864@06-
02-08
24-05-08
23-05-18
19 lfpu firk izdk'k ikVuh
fuoklh NksVk cktkj
mUgsay
iRFkj 76 4.000 vkD;k
uthd
8@01-01-
09
05-01-09
04-01-19
20 jes'k firk euksgjyky
tSu]
fuoklh&102] ,e-vkbZ-th-
jksM+] ukxnk
iRFkj 1289 la'kksf/kr
1268 1269
2.000 cucuk 397@22-
03-10
15-09-09
14-09-19
21 Jherh panzdq¡oj ifr
lqjsanzflag pkSgku
fuoklh&490] xqykcckbZ
dkWyksuh] ukxnk
iRFkj 418 2.000 edyk 827@07-
07-09
15-07-09
14-07-19
22 Jh }kjdk/kh'k firk
f'koukjk;.k esgrk]
fuoklh&LVs'ku jksM+] gk;j
lsds.Mjh Ldqy ds lkeus]
mUgSy
iRFkj 60, 61 4.000 vkD;k
uthd
536@15-
04-10
29-04-10
28-04-20
23 Jh 'ks[kkor LVksu Øs'kj]
izksizk;Vj] guqekuflag
ukjk;.kflag 'kS[kkor]
fuoklh&xoZUes.V dkWyksuh]
ukxnk
iRFkj 824 1.000 fxanokfu;k 583@27-
04-10
29-04-10
28-04-20
24 Jh 'ks[kkor LVksu Øs'kj]
izksizk;Vj] guqekuflag
ukjk;.kflag 'kS[kkor]
fuoklh&xoZUes.V dkWyksuh]
ukxnk
iRFkj 11
12
1.710 Hkxriqjh 591@27-
04-10
29-04-10
28-04-20
25 Jh vf'ou firk lrh'k
ek:]
fuoklh&NksVk cktkj] okMZ
ua- 13] mUgSy
iRFkj 62/1 2.000 vkD;k
uthd
3130
05-12-2015
01-01-16
31-12-21
26 Jh vf'ou firk lrh'k
ek:]
fuoklh&NksVk cktkj] okMZ
ua- 13] mUgSy
iRFkj 76 4.000 vkD;k
uthd
3131
05-12-2015
01-01-16
31-12-21
27 Jh vf'ou firk lrh'k
ek:]
fuoklh&NksVk cktkj] okMZ
ua- 13] mUgSy
iRFkj 575/11 4.000 dq.Myk 271@06-
08-14
08-08-14
07-08-24
28 Jh lfpu firk Jh
izdk'kpUnz ikVuh fuoklh
NksVk cktkj mUgsy ftyk
mTtSu
iRFkj 575/11 4.000 dq.Myk 271@06-
08-14
08-08-14
07-08-24
29 Jh dj.kflag firk
fuoklh&ch&15@5
egkuankuxj mTtSu
iRFkj 574 3.000 dq.Myk Mh-th-,e
17409&10
@ 11-09-
14
19-03-15
18-03-25
30 Jh gfjukjk;.k firk
y{ehukjk;.k /kkdM
fuoklh&egkRek xka/kh ekxZ
[kkpjkSn
iRFkj 4423
4464
4465
2.488 dLck
[kkpjkSn
1586
03-06-2015
26-06-15
25-06-25
31 Jh jes'k firk jruyky
ukansM fuoklh&LVs'ku jksM
mUgsy
iRFkj 356 2.000 vkD;k
uthd
747
11-04-2016
16-06-
2016
15-06-
2026
32 Jh jkes'oj firk ekaxhyky
ikVhnkj fuoklh&xzke
eMkonk rglhy [kkpjkSn
iRFkj 2644 1.000 eMkonk 1640
05-08-2016
05-10-
2016
04-10-
2026
33 Jh jhrs'k firk jes'kpUnz
tk;loky fuoklh&20
jk.kkizrki ekxZ [kkpjkSn
iRFkj 583 2.000 cqjkukckn 1608
04-08-16
24-09-
2016
23-09-
2026
34 Jhefr uhrw ifr lw;Zizdk'k
'kekZ fuoklh&35 xksiky
dqat jke}kjk ds ihNs
xksiky ekxZ [kkpjSkSn
iRFkj 583 2.000 cqjkukckn 1579
28-07-2016
15-12-16
14-12-26
35 Jh lw;Zizdk'k firk
uhydaB 'kekZ fuoklh&90
lqHkk"k ekxZ [kkpjkSn
iRFkj 602/3 2.000 dqEgkjokM+h 1905
27-09-16
15-12-16
14-12-26
180.544
rglhy cMuxj
1 Jh dkafryky firk
eqUukyky dqeB
fu- ehjkckbZ iFk cM+uxj
iRFkj 348 1.000 [kjlkSndyk 1557@
20-11-07
7-12-07
06-12-17
2 Jh xqykcflag firk
ioZrflag fuoklh&xzke
baxksfj;k rg- cMuxj
iRFkj 1 2.000 fldUnj[ksM
k
1118@27-
08-13
24-05-14
23-05-24
3 Jh txUukFk firk
cnzhyky fuoklh&xzke
ekSyku rglhy cMuxj
ftyk mTtSu
eqje 623 4.000 eksykuk 1384
13-05-15
26-06-15
25-06-15
4 Jh nsohyky firk
y{ehukjk;.k ikVhnkj
fuoklh&xzke vtMkonk
rg- cMuxj ftyk mTtSu
eqje 666 3.800 cjfM;k 2731
20-10-2015
02-12-15
01-12-25
10.800
rglhyr efgniqj
1 fnus'k firk ekaxhyky tSu
fuoklh efgniqj jksM+
iRFkj 993 1.000 ciS;k 590@29-
04-10
04-08-
2010
03-08-20
2 Jh fgrs'k dqekj dY;k.k
ckfB;k
fuoklh jktsUnz ekxZ]
efgniqj
iRFkj 404/1 1.000 lsdk[ksM+h 'kk[kk&1@
52
09-06-14
25-02-15
24-02-25
3 Jherh izHkk dsoyk ifr
yksdsUnzflag pkS/kjh
fuoklh 7] ;'koaruxj]
efgniqj
iRFkj 57/1 0.750 catkjh 1903@22-
02-07
10-03-08
09-03-18
4 tkosn [kku firk vetn
[kku iVsy
fuoklh efgniqj lhVh
iRFkj 44 1.000 dqaduh 2000@24-
03-08
08-04-08
07-04-18
5 Jherh fofurk ifr fojsUnz
xqIrk
fuoklh 83] lkabZukFk
dkWyksuh] mTtSu
iRFkj 1538/2 1.000 txksVh 430@30-
06-08
25-09-08
24-09-18
6 Jhefr dkS'kY;k nsoh ifr
dSyk'k pUnz lksuh
fuoklh&x.ks'k xyh
efgniqj lhVh
iRFkj 488 2.000 dkpfj;k 3104@22-
10-11
03-11-11
02-11-16
7 Jh fojsUnzflag firk
ukjk;.kflag fuoklh&xzke
txksVh rg- efgniqj
iRFkj 1538/2 2.000 txksVh 03@10@2
013
28@1@1
4
27@1@2
4
8 Jh dey fd'kksj firk
jk/ks';ke f=osnh fuoklh&
'kqxjfey ekxZ efgniqj
iRFkj 731 1.250 xksxkiqj 1890@24-
12-13
22@1@1
4
21@1@2
4
9 Jh ckcqyky firk ek/kksth
lq;Zoa'kh fuoklh&xzke
edyk rg- efgnqiqj
iRFkj 1/1 1.000 edyk 2119@13-
01-14
14@5@1
4
13@5@2
4
10 Jh eukst firk jes'kpUnz
tSu fuoklh 196 xzke
xksxkiqj efgniqj
iRFkj 167 1.000 dkuk[ksMh
,dykliqj
841@20-
11-14
5-12-14
04-12-24
11 Jh Hkxokuflag firk
ekaxwflag fuoklh& xzke
>Vkon rg- efgniqj
iRFkj 165 2.300 dkuk[ksMh
,dykliqj
'kk[kk&1@
11701-07-
14
01-07-14
30-06-24
12 fojsUnz firk ukjk;.k xqIrk]
fu-&83 lkbZukFk dkWyksuh]
mTtSu
iRFkj 1538@2 1.000 txksVh 4016@02-
11-15
19-01-16
18-01-26
13 eks- jQhd firk gkth pkan
eks- ukxkSjh] fu- 17@2
ukxkSjh eks- efgniqj
iRFkj 213
214
1.000 fprkon Mh-th-,e
137&139
@
05-01-16
19-01-
2016 ls
18-01-20
14 Jh foØe firk lsojke
vkatuk
fuoklh&<kcykfla;k
iRFkj 1237 2.000 jkuk;jkihj 2388
16-12-16
22-12-16
21-12-
2026
15 Jh ;'k firk dey
fd'kksj f=osnh
fuoklh&'kqxj fey ekxZ
efgniqj
iRFkj 1@1 2.000 MsyphcqtqxZ 2505
31-12-2016
4. DETAILS OF ROYALTY OR REVENUE RECEIVED IN LAST THREE YEARS
fofRr;
o"kZ vk; [kfut jktLo vk;
jktLo izkfIr iRFkj iRFkj&fxÍh feÍh jsr eq:e vU;
2013&14 50498706 & 33108690 260000 4388160 6619157 6122699
2014&15 77228448 100000 55589592 512408 3883853 2268713 14873882
2015&16 120282602 30000 101376195 469344 3168486 4292571 10946006
5. DETAILS OF PRODUCTION OF SAND OR BAJRI OR MINOR MINERAL IN LAST THREE YEARS
[kfut dk uke
o"kZ 2013&14 dk
mRiknu ?k-eh- esa
o"kZ 2014&15 dk
mRiknu ?k-eh- esa
o"kZ 2015&16 dk mRiknu
?k-eh- esa
iRFkj & 1000 300
iRFkj&fxV~Vh 752470 665202 1013761
feÍh 9629 6340 4693
jsr 82795 50620 31684
eq:e 245153 130249 85851
6. PROCESS OF DEPOSITION OF SEDIMENTS IN THE RIVERS
Rivers have a lot of energy and because they have energy, they do stuff. The obvious
things rivers do with their energy is flow but, besides this, they also transport load, erode
load and erode the channel through which they flow.
Erosion
Erosion is the breaking down of material by an agent. In the case of a river, the agent
is water. The water can erode the river’s channel and the river’s load. A river’s load is bits
of eroded material, generally rocks, which the river transports until it deposits its load.
A river’s channel is eroded laterally and vertically making the channel wider and
deeper. The intensity of lateral and vertical erosion is dictated by the stage in the river’s
course, discussed in more detail here but essentially, in the upper stage of the river’s
course (close to the source of the river) there is little horizontal erosion and lots of vertical
erosion. In the middle and lower stages vertical erosion is reduced and more horizontal
erosion takes place. There are several different ways that a river erodes its bed and
banks. The first is hydraulic action, where the force of the water removes rock particles
from the bed and banks. This type of erosion is strongest at rapids and waterfalls where
the water has a high velocity. The next type of erosion is corrasion. This is where the
river’s load acts almost like sandpaper, removing pieces of rock as the load rubs against
the bed & banks. This sort of erosion is strongest when the river is transporting large
chunks of rock or after heavy rainfall when the river’s flow is turbulent. Corrosion is a
special type of erosion that only affects certain types of rocks. Water, being ever so slightly
acidic, will react with certain rocks and dissolve them. Corrosion is highly effective if the
rock type of the channel is chalk or limestone (anything containing calcium carbonate)
otherwise, it doesn’t have much of an effect. Cavitation is an interesting method of erosion.
Air bubbles trapped in the water get compressed into small spaces like cracks in the river’s
banks. These bubbles eventually implode creating a small shockwave that weakens the
rocks. The shockwaves are very weak but over time the rock will be weakened to the point
at which it falls apart. The final type of erosion is attrition. Attrition is a way of eroding the
river’s load, not the bed and banks. Attrition is where pieces of rock in the river’s load
knock together, breaking chunks of rock off of one another and gradually rounding and
shrinking the load.
Transportation
When a river erodes the eroded material becomes the river’s load and the river will
then transport this load through its course until it deposits the load. There are a few
different ways that a river will transport load depending on how much energy the river has
and how big the load is. The largest of particles such as boulders are transported by
traction. These particles are rolled along the bed of the river, eroding the bed and the
particles in the process, because the river doesn’t have enough energy to move these
large particles in any other way. Slightly smaller particles, such as pebbles and gravel, are
transported by saltation. This is where the load bounces along the bed of the river
because the river has enough energy to lift the particles off the bed but the particles are
too heavy to travel by suspension. Fine particles like clay and silt are transported in
suspension; they are suspended in the water. Most of a river’s load is transported by
suspension. Solution is a special method of transportation. This is where particles are
dissolved into the water so only rocks that are soluble, such as limestone or chalk, can be
transported in solution.
Capacity & Competence
Rivers can only carry so much load depending on their energy. The maximum volume
of load that a river can carry at a specific point in its course is called the river’s capacity.
The biggest sized particle that a river could carry at a specific point is called the river’s
competence.
Deposition
To transport load a river needs to have energy so when a river loses energy it is forced
to deposit its load. There’s several reasons why a river could lose energy. If the river’s
discharge is reduced then the river will lose energy because it isn’t flowing as quickly
anymore. This could happen because of a lack of precipitation or an increase in
evaporation. Increased human use (abstraction) of a river could also reduce its discharge
forcing it deposit its load. If the gradient of the river’s course flattens out, the river will
deposit its load because it will be travelling a lot slower. When a river meets the sea a river
will deposit its load because the gradient is generally reduced at sea level and the sea will
absorb a lot of energy.
As rivers get nearer to their mouths they flow in increasingly wide, gentle sided valleys.
The channel increases in size to hold the extra water which the river has to receive from
its tributaries. As the river gets bigger it can carry larger amounts of material. This material
will be small in size, as larger rocks will have broken up on their way from the mountains.
Much of the material will be carried in suspension and will erode the river banks by
abrasion. When rivers flow over flatter land, they develop large bends called meanders. As
a river goes around a bend most of the water is pushed towards the outside causing
increased erosion. The river is now eroding sideways into its banks rather than downwards
into its bed, a process called lateral erosion. On the inside of the bend, in contrast, there is
much less water. The river will therefore be shallow and slow-flowing. It cannot carry as
much material and so sand and shingle will be deposited. This is called a point bar or slip
off slope.
Due to erosion on the outside of a bend and deposition on the inside, the shape of a
meander will change over a period of time. Notice how erosion narrows the neck of the
land within the meander. In time, and usually during a flood, the river will cut right through
the neck. The river will then take the new, shorter route. The fastest current, called the
thalweg, will now tend to be in the centre of the river, and so deposition is likely to occur in
gentler water next to the banks. Eventually deposition will block off the old meander to
leave an oxbow lake. The oxbow lake will slowly dry up , only refilling after heavy rain or
during a flood. Streams lose velocity and make deposits when their gradient decreases,
when the volume of water decreases, when there is an increase in cross section, when
they encounter obstructions, or when they enter still water. They deposit alluvial fans,
alluvial cones, piedmont alluvial plains, channel fill, bars, flood plains and deltas.
7. GENERAL PROFILE OF THE DISTRICT
S.No. Items Statistics
01 General Information
i) Geographical area ii) Administrative Divisions
Number of Tehsil/Blocks Number of Panchayats Number of Villages
613023 ha 07/06 612 1117
iii) Population(Census 2011) 1,986,597
iv) Normal Rainfall 914.5mm
02 Geomormology
1. Major Physiographic Units: Malwa plateau
2. Major Drainage: Ganga Basin I. Kshipra River II. Chhoti Kali Sindh III. Gambhir River IV. Chamla River
03 Land Use (‘000ha)
a) Forest area b) Cultivable area c) Net area sown
3.1 489.025 489.10
04 Major Soil Type Black cotton soil and Regur
05 Principal Crops Soyabean,Gram,Wheat
06 Irrigation by Different Sources No. Area irrigated(‘000ha)
Dug wells Tube wells/Bore wells Tanks/Ponds Canals Other Sources Net Irrigated Area Gross irrigated area
33390 47753 43 34 - - -
44.26 131.27 0.92 3.57 19.77 199.8 199.8
07 Number 0f Ground Water Monitoring Wells of CGWB (As on 31.3.2013)
Number of Dug Wells Number of Piezometers
19 26
08 Predominant Geological Formations 1. Alluvium 2. Deccan Trap basalts
-- Means Not Reported / Not Available or Reported Zero
Directorate of Economics &Statstics
Ministry of Agriculture, Govt. of India Page 1 of 1
8-: LAND UTILIZATION PATTERN IN THE DISTRICT: FOREST, AGRICULTURE, HORTICULTURE, MINING ETC.
Total Area and Classification of Area in Ujjain District of MADHYAPRADESH State for the year ending 2013- 14 (in Hectares)
District
Reporting
Area
For
Land
Utilization
Statistics
Area
Under
Mining activities
Forests
Not Available For Cultivation Other Uncultivated Land Excluding Fallow Land Fallow Land
Net
Area
Sown
Total
Cropped
Area
Area
Sown More than Once
Area
Under
Non
Agricultural
Uses
Barren
and
Un-Cultivable
Land
Total
Perman
ent
Pasture
s and
Other
Grazing
Lands
Land Under
Misc Tree
Crops and
Groves not
Included in
Net Area
Cultivable
Waste
Land
Total
Fallow
Lands
Other
than
Curre
nt
Fallows
Current
Fallow Total
(1) (2) (3) (4) (5) (6) (7) (8) (9) (10) (11) (12) (13) (14) (15) (16) (17)
Ujjain 609874 963.231 3149 58788 5900 64688 32285 129 7635 40049 1792 535 2327 499661 938003 438342
The topography of the area is outcome of the erosional agencies that are active in
shaping the land forms. The primary erosional agencies are water and wind.
Topographically the area of the district can be divided into two physiographic units.
1. Undulating planes.
2. Low altitudes ridges and mounds.
The District lies on the Malwa plateau at a general level of 500 metres. The variations
of altitude range from 450 metres in the north to 558 metres at the southern, isolated
peaks. On the whole the area is a broad undulating plateau with no marked hill range. The
general slope is from south to north, marked by a number of small rivers which later join
the Chambal and from the feeders of the Ganga system. The maximum elevation of 561m.
and minimum elevation of 465m. above m.s.l. are noticed in the western and north-
western part of the district.
10. RAINFALL: MONTH-WISE
RAINFALL IN MILIMETERS
Month 2011 2012 2013
January 0.00 0.00 0.00
February 0.00 0.00 18.00
March 2.10 0.00 26.60
April 0.00 0.00 1.90
May 2.60 7.60 0.00
June 131.50 33.60 221.30
July 395.40 465.90 471.40
August 402.00 268.30 372.90
September 148.20 219.40 98.10
October 0.00 0.00 56.50
November 0.00 0.00 0.00
December 0.00 0.00 6.20
TOTAL 1081.8 994.8 1272.9
11. GEOLOGY AND MINERAL WEALTH
A concise general geological stratigraphic sequence of the area is as
following:-
Recent ------------------ Black cotton soil, Red bole
Laterite, Lateritic soil and Alluvium.
Cretaceous to
Eocene Deccan Traps Basalt with intertrappean.
Entire area of the district is covered by Deccan trap basalt flows of late Cretaceous
to Palaeocene age (68-62 m. y. ). The district is more or less monotonous. The Deccan
traps which lie over the older formations, consisting of massive, zeollitic and vesicular
flows of varying thickness. Generally the hard massive trap is underlain by zeolitic and
vesicular trap. Some of the lava flows pinch out towards north-east. The top part of lava
flows is generally fragmentary with a meter thick impersistent red bole. The bottom of the
flow is composed of beautiful columnar joints. These can be seen near village Pat, parsi,
Roopakheri and other villages.
An impersistent inter-trappean bed comprising of thin laminated shale with siltstone,
chert bands with pockets of limestone and gastropod fossils are reported from few places.
At places alluvium has also been noticed in the valley of the rivers Kshipra and the
Chambal. Alluvium deposits of quaternary age occur along the courses of Chhoti kalisindh
and Lakundar rivers. It generally consists of yellowish to brownish sandy base. The
thickness varies from less than a meter to 15 m. Alluvium also occurs along the banks of
Chambal and its tributaries and has a thickness of more than 10 m.
Agate, chalcedony and secondary silica have also been noticed at few places in
limited quantity. Laterite occurrences are also noticed at some places.
DRAINAGE:-
The district falls in the Ganga drainage system.The main river of the district is the
Chambal which and all other tributary streams flow parallel from south to north in the
district.However in most of the areas, the drainages are lithologically controlled resulting in
dendritic to subdendritic type of drainage which is the very common characteristic feature
of Deccan trap country rock. The drainage of the area is controlled by northerly flowing
Chambal river and its tributaries Chamla, Gambhir, Sipra, Khan and Chhoti kalisindh river.
Drainage system with description of main rivers
SERIAL NO.
NAME OF THE
RIVER AREA DRAINED(KM2)
% AREA DRAINED IN THE DISTRICT
01 Chambal Originate in the Indore district About 20% of the area of district
02 Kshipra Originate in the Dewas district About 30% of the area of district
03 Choti Kali
Sindh Originate in the Dewas district About 30% of the area of district
04 Gambhir Originate in the Indore district About 15% of the area of district
05 Chamla Originate in the Dhar district About 05% of the area of district
Salient Features of Important Rivers and Streams
SERIAL NO.
NAME OF THE
RIVER OR STREAM
TOTAL LENGTH IN THE
DISTRICT(IN KM) PLACE OF ORIGIN
ALTITUDE AT
ORIGIN
01 Chambal 90 Janapao,indore district 854.35 meter
02 Kshipra 105 Kokri Bardi hills,Dewas district 747.00 meter
03 Choti Kali
Sindh 109 Sia village, Dewas district
600-700 Meter
04 Gambhir 60 Man Sarovar tank in Lunehra
village 560 meter
05 Chamla 45 Dhar District 750 meter
Sr.No.
PORTION OF THE DISTRICT OR
STREAM RECOMMENDED
FOR MINERAL CONCESSION
Village Tehsil
AREA RECOMMENDED
FOR MINERAL CONCESSION (IN HECTARE)
MINEABLE MINERAL
POTENTIAL(IN METRIC
TONE) (60% OF TOTAL MINERAL
POTENTIAL)
1 1 dkyqgsMk ?kfÍ;k 4.97 2500
2 197]437 rqeMonk ?kfÍ;k 4.66 2500
3 125 lkyk[ksMh ?kfÍ;k 4.96 2500
4 1 fiiY;kgkek ?kfÍ;k 4.95 2500
5 1 esjx< rjkuk 4.5 2500
6 410 xquk[ksMh rjkuk 4.5 2500
7 627]738]1122] 1140]75]6 lkexh rjkuk 4.5 2500
8 1]320]341 iklykSn cMuxj 4.99 2500
9 469 /kjsjh ¼unh½ cMuxj 4.98 2500
10 1 ekyiqjk cMuxj 4.96 2500
11 100]224 nsgVk ¼pEcy
unh½
cMuxj 4.97 2500
12 500 nqukytk cMuxj 4.97 2500
13 535]653 y[ksljk cMuxj 4.97 2500
14 1]11 fclkgsMk cMuxj 4.96 2500
15 284 :nz[ksMk efgniqj 4.97 2500
16 1125 fprkon efgniqj 4.96 2500
17 268 'ksjiqj efgniqj 4.96 2500
18 229]500 fpjeh;ka efgniqj 4.5 2500
19 496 vkD;k/kkxk efgniqj 4.5 2500
20 241 f?k;k[ksMh efgniqj 4.5 2500
21 89]317 [kjfM;k ekuiqj efgniqj 4.75 2500
22 716 ?kkVfiiY;k efgniqj 4.96 2500
23 1 c.kh efgniqj 4.96 2500
24 271]307]402 ckxsMh [kkpjkSn 4.5 2500
25 52 lksufpMh [kkpjkSn 4.5 2500
26 164 dfM;kyh [kkpjkSn 3.15 2000
27 689]738 uk;u ukxnk 4.96 2500
28 1]86 /kwysV ua- 1 ls 3 efgniqj 9 2700
29 1]6]147 czgke.k[skMh [kkpjkSn 5.79 1737
30 1 xksBMk [kkpjkSn 5.97 1791
31 160]209 mWpkgsMk ua 2 o
3
[kkpjkSn 7.97 2337
32 1]233 yksgfprkjk [kkpjkSn 6.62 1986
33 1101 ujflaxk cMuxj 5.15 1545
34 1]102 'ks[kiqj cMuxj 7.2 2160
35 1]14 >qedh cMuxj 7.18 2154
36 291 xqUnfMZ;k rjkuk 14.29 4287
37 1]899]828 dk;Fkk ua- 1 o
2
rjkuk 6.89 2069
38 1 fjaxfu;k [kkpjkSn 6.13 1839
39 114]472 fiiY;kcktkj rjkuk 6.22 1866
40 436 HkMflEck rjkuk 9.77 2931
41 496 fpjMh rjkuk 7.76 2328
42 1@189 xks;yk[kqnZ ua- 4 mTtSu 5.947 1784
43 139 jS;kiqj ukxnk 5 2000
44 10]80]124]305 :ik[ksMh ukxnk 5 2000
45 607]667]724 nhnh;k[ksMh ukxnk 5 2000
46 5 xquk;k ?kfÍ;k 4.5 2000
47 106 xquk;k ?kfÍ;k 4.5 2000
48 177 veykon dyk cMuxj 5 2000
49 1 gehj[ksMh mTtSu 5.97 2700
50 1 pwuk[ksMh rjkuk 5 2150
51 170 veykonkfcdk cMuxj 7.87 3350
52 291, 149 lsefy;k cMuxj 6.1 2900
53 246, 508 fltkork cMuxj 16.59 6900
54 904 cuflax efgniqj 5.25 7980
55 1030 bUnks[k efgniqj 12.24 8000
56 303 cksy[ksMk?kkV efgniqj 6 2650
57 266 cksy[ksMk?kkV efgniqj 7.59 3400
58 315 fiify;kHkhe efgniqj 6 10000
59 158 :nz[ksMk efgniqj 8.88 14100
60 78 lsdMhlqYrkuiqj [kkpjkSn 6.4 3150
61 1 vjU;kos.kk efgniqj 13.48 4044
62 80 cMxkWo efgniqj 6 1800
63 988 fprkon efgniqj 12.5 3750
64 18 ckjkiRFkj efgniqj 6 1800
65 632]511 JhoPN [kkpjkSn 9.24 1872
66 1]252 eqjkj[ksMh cMuxj 6.77 2031
67 78 catkjh rjkuk 7.2 2160
68 1 Vdoklk mTtSu 9.36 2808
69 1]3]11]12]13]15]41,oa 54 fiiY;kjk?kks mTtSu 7.88 2364
70 190]189 lsoj[ksMh mTtSu 9.71 2955
71 508]360]489 vkyeiqj mMkuk
ua- 1 o 2
mTtSu 6.97 2091
72 1 iaFkfiiykbZ mTtSu 9.36 2808
73 1]513 fuukSjk 1 mTtSu 7.91 2375
74 347 fuukSjk 2 mTtSu 8.57 2571
75 1 eq.Myk ukxnk 5 2000
76 168 gkik[ksMk ukxnk 5 2000
77 718]855 xqjkfM;k lkaxk ukxnk 5 2000
78 129]298]274 bVkok ukxnk 5 2000
79 1]272 vkyksV tkxhj ukxnk 5 2000
80 24]209]290 cStukFk[ksMh ukxnk 5 2000
81 373 ijksY;k inek ukxnk 5 2000
82 986 ljouk mUgsy ukxnk 5 2000
83 218 ft;kthx< ukxnk 5 2000
84 352 lwjtk[ksMh ukxnk 5 2000
85 583 xqjkNk ukxnk 4.66 2000
86 385 djukon ukxnk 1.66 800
87 229 ixkjk ukxnk 2.65 1200
88 1 f>jU;k mUgsy ukxnk 4.36 2000
89 1 nsgVk cMuxj 5 2000
90 45 ckofy;k efgniqj 9.89 2967
91 145 elokfM;k[kkylk cMuxj 8.08 2424
92 99]234]381]496]98@648 ikMlwfr;k [kkpjkSn 14.299 4499
93 1 358 529 554 fpMhjkofn;k ukxnk 5 2000
94 2 vkyksV tkxhj ukxnk 5 2000
95 14 vjksfy;k nsoMk ukxnk 5 2000
MINERAL POTENTIAL
Boulder(MT) Bajri(MT) Sand (MT) Total Mineable mineral
potential(MT)
Huge as majority of the district is occupied by the minor minerals i.e. basalt. But as per figures received from District Mining Section 1013761 M3 of aggregate and 300 M3 of stone was produced in 2015-16
It is associated with river sand
It is found mainly in Chambal, Kshipra, Choti Kali Sindh, Gambhir and Chamla rivers,Kurel rivers though the resources as per their area in the district is huge, the production of sand and bajri is 50620 M3 in 2014-15 and 31684M3 in 2015-16
Huge, immense as most of the district is occupied by minor minerals which include basalt .and granite and other stones as road metal and soil. Thus mineral potentials are immense.
ANNUAL DEPOSITION
Sr. no.
River or stream
Portion of the district or stream
recommended for mineral concession
Area recommended for
mineral concession (in
Hectare)
Mineable mineral potential(in metric tone) (60% of total mineral potential
1 Chambal Along the River banks of Chambal, in the Western part of the district
124.789 52053 M3
2 Kshipra Along the river banks, in the central part of the district
215.657 100487 M3
3 Choti Kali Sindh
Along the river banks, in the eastern part of the district
49.35 27699 M3
4 Gambhir Along the river banks, in the central part of the district
103.580 38295 M3
5 Chamla Along the River bank, in the south-western part of the district
05.00 4500 M3
6 Kurel Along the River banks, in the north-western part of the district
44.22 13212 M3
TOTAL 542.596 Hectare 236246 M3
The process of sand replenishment is highly dependent upon the rainfall received in
the catchment areas of rivers and their tributaries and velocity of river. It is a dynamic
process. Thus it is difficult to predict, what quantity of sand may be reclaimed/replenished
by river. Because, in case of less rain, less water in the river, there may be less erosion
and transportation may also be minimal and as a result deposition too will be less.
Moreover, in case of floods, the sudden gush of water may force the change in the river
course, thus old sites of sand deposition may not be relevant. Thus, the above figures may
just be a mere prediction, based on the production in the preceding years. More so,
practically, it is not possible that in such a short period, single person can visit each spot
within the district and determine how much quantity of sand may be replenished every
year. The data narrated in the report, regarding annual deposition of sand and associated
aggregates and mineable mineral potential is concerned, is only estimation based on the
production data provided by the district mining office. Thus, the figures may vary from area
to area and year on year basis. Therefore, this document is not static one but have to be a
dynamic one, the figures of which may vary with respect to time. The DEAC committee is
at liberty to make the spot inspection of the area under question for which the prior
environmental clearance will be sought. In order to establish a safe extraction limit, such
that the extracted sand gets replenished annually, a replenishment study is to be carried
out. For this purpose, the river bed RL at selected points in the dry portions of Riverbed
will be measured during pre–monsoon period and again during post –monsoon period in
order to assess the annual quantum of sand deposition. If it is observed that, there is an
average increase in riverbed RL, it shows that it is due to deposition of sand during the
monsoon flow of the river and by multiplying it with the area of lease one can measure the
quantity of sand replenished every year.
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