GOVERNMENT OF BIHAR DISTRICT GOPALGANJmines.bih.nic.in/DSR/MM/DSR-MM-Gopalganj.pdf · Gandak....

GOPALGANJ DISTRICT, BIHAR

1

District Survey Report of Minor Minerals, Gopalganj. Prepared in accordance with Para 7 (iii)(a) of S.O.141 (E)

Dated 15th January 2016, As Amended on S.O. 3611 (E), dated

25th July 2018 of

Ministry of Environment, Forest and Climate Change

Notification.

GOVERNMENT OF BIHAR DISTRICT GOPALGANJ

PREPARED BY

sathi planners pvt. Ltd.

Under the guidance of deiaa, gopalganj


2

CONTENT

Ch.No. Description Page No

Preamble 3

1 Introduction 5

1.1 Location and Geographical Area 7

1.2 Administrative Units 8

1.3 Connectivity 8

2 Overview of mining activity in the district 11

3 List of Mining lease in the district 12

3.1 List of Kiln/Bhatta in the district as per department record 12

3.2 List of Kiln/Bhatta in the district as per field survey report 30

3.3 List of Proposed sand ghat(Potential Area) 43

4 Detail of Royalty or Revenue received in last 3 years 52

5 Detail of Production of Sand or Bajri or minor mineral in last three

years

52

6 Process of Deposition of Sediments in the rivers of the District 53

7 General Profile of the District 59

8 Land Utilization Pattern in the district 71

9 Physiography of the District 72

10 Rainfall: Month Wise 73

11 Geology & Mineral wealth of the area 74

12 Additional Information 77

13 Disaster & Risk Management 78

14 Conclusion & Reference 83


3

PREAMBLE

Keeping in view of experience gained in period of one decade, the MOEF&CC came out with

Environmental Impact Assessment Notification S.O.-1533(E) dated 14th Sept.2006. It has been

made mandatory to obtain environmental clearance for different kinds of development

projects as listed in Scheduled -1 of notification.

Further, pursuance of the order of Hon’ble Supreme Court Petition (C) No. 19628-19629 of

2009, dated 27th Feb.2012 In the matter of Deepak Kumar etc., Vs State of Haryana and others

etc., prior environmental clearance has now become mandatory for Mining of Minor Minerals

irrespective of the area of Mining Lease.

And also in view of the Hon’ble National Green Tribunal, order dated the 13th Jan.2015 the

matter regarding Sand, Brick earth, & borrowed earth cutting for Road Construction has to take

prior E.C. For Mining Lease irrespective of the fact that whether the area involved is more or

less than 5 hectares. They also suggested to make a policy on E.C for sand including other minor

minerals mining lease in cluster.

Under 7(iii)(a) it was also suggested to prepare the district survey report for sand mining or

river bed mining and mining of other mineral as prescribed in appendix X. This has been

modified vide S.O. No.- 3611(E) dated 25th July 2018.

In the present DSR of Gopalganj district no minor minerals other than sand mining or river

bed sand and brick earth has been described.

MOEF&CC in consultation with State Government has prepared Guidelines on Sustainable Sand

& other Minor minerals mining detailing the provisions on Environmental Clearance for cluster.

Creation of District Environmental Impact Assessment Authority (DEIAA) & proper monitoring

of Minor Minerals Mining using Information Technology to track the mineral out material from

source to destination.

Appraisal Committee will scrutinize and recommend the prior environmental clearance of

Mining of Minor Mineral on the basis of District Survey report. This will model and guiding

document which is a compendium of available mineral resources, geographical setup,

environmental and ecological set up of the district and replenishment of minerals and is based

on data of various departments, published reports, Journal and websites. The District Survey

report will form the basis of application for environmental clearance, preparation of reports

and appraisal of projects. District Survey Reports are to be reviewed once in every five years as

per statue, however this is an interim report, which will be updated at regular intervals.

In line with above guideline Chief Secretary of Government of Bihar issued Sand Policy vide

M/M/(Ba)04/13 – 2214 dated 27 -08-2013 subsequently Bihar Minor Mineral Rule 2017 was

come into force from 10-10-2017 but Hon’ble High Court has stayed the operation of Bihar

Minor Mineral Rules 2017. The Hon’ble Court has further indicated that till such time, the

earlier rules shall remain operational.


4

In view of the situation arising out of the said order and in terms of the provisions under Rule

21(b) and clause 17(c) of Form –D of Bihar Minor Mineral Concessions Rule 1972 read with para

14 (ii) of the Sand Policy -2013 the state Govt orders the following vide Principal Secretary

order no -7297/M 29-11-2017:-

State Govt. authorizes the Bihar State Mining Corporation, (came for existence from 22-09-

2017) to commence the business of trading in Minor Minerals in terms of the proposal

submitted to the State Govt. and duly approved by it on 1-10-2013 and the District Survey

report will form the basis for application for environmental clearance.

This order took effect from 01-12-2017

The Main objective of the preparation of District Survey Report is to ensure the following:-

1. Identification of Sand Ghats with geo references.

2. Identification of potential areas of river silt with geo reference, which is being used for filling

purposes.

3. Identification of brick kilns and bangla bhatthas with geo reference.

4. Identification of other mineral resources if available.


5

1. INTRODUCTION

GOPALGANJ AT A GLANCE:- Gopalganj district, “The land Of Sugarcane”, is located on global map between 26°12' and 26°39' North latitude and 83°54' and 84°55' East longitude. The district occupies an area of 2,033 square kilometers. It covers 2.2 % of the total areas of the state of Bihar. The rank of the district in comparison to other districts of Bihar in terms of area is 26th. The district is located on the West North corner of the Bihar State. The district is bounded on the east by Purbra Champaran and Muzaffarpur, on the south by state of Uttar Pradesh, Siwan and Saran on the west by State of Uttar Pradesh and on the north by State of Uttar Pradesh and Pashchim Champaran. There are no hills in Gopalganj. Though the district presents the appearance of a level plain, the uniformity is broken here and there by the depressions and marshes dotted over the countryside. The district contains no forest as well. The Gandak supported by tributaries like Jharahi, Khanwa, Daha, Dhanahi etc. give a big status of river. Land of the district is fertile and alluvial because of this river the district is good in cultivation and irrigation. River Gandak by depositing the top quality of soil bringing from the Nepal is playing an important role in the economy of the district.

S.No Particular Year Unit Statistics

1 Geographical features

(A) Geographical Data

i) Latitude -- Degree minute 26° 12’ to 26° 39’ N

ii) Longitude ------ -do- 83° 54’ to 84° 55’ E

iii) Geographical Area -do- 2033 km²

(B) Administrative Units

i) Sub divisions - No.- 2

ii) Tehsils 2011 Nos. 14

iii) Sub-Tehsil - -do- --

iv) Patwar Circle 2010-11 -do- -

v) Panchayat Simitis/Nyay Panchayat

2010-11 -do- -

vi)Nagar nigam - - --

vii) Nagar Palika 2009-10 Nos. 1

viii) Gram Panchayats 2010-11 Nos. --

xi) Revenue villages 1564

x) Assembly Area 2011-12 Nos. 1 MP +6 MLA

2. Population (2,558,037)

(A) Sex-wise

i) Male 2011 Nos. 1,269,677


6

ii) Female 2011 Nos 1,288,360

(B) Rural Population 2011 Nos 2,402,764

3. Agriculture

A. Land utilization

i) Total Area 2009-10 hectare 115000

ii) Forest cover -do- “ -

iii) Non Agriculture Land

-do- “ 35400

v) cultivable Barren land

-do- “ 25487

4. Forest

(i) Forest 2009-10 Ha. ---

5. Livestock & Poultry

A. Cattle

i) Cows 2011 Nos. 10500

ii) Buffaloes 2011 Nos. 9750

B. Other livestock

i) Goats 2007 Nos. 5400

ii) Pigs 2007 Nos. 2500

iii) Dogs & Bitches 2007 Nos. 2400

iv) Railways

i) Length of rail line 2010-11 Kms 56

V) Roads

(a) National Highway 2009-10 Kms 68

(b) State Highway 2010-11 Kms 86

(c) Main District Highway

2010-11 Kms 120

(d) Other district & Rural Roads

2010-11 Kms

(e) Rural road/ Agriculture Marketing Board Roads

2010-11 Kms 188-

(f) Kachacha Road 2010-11 Kms 164

(VI) Communication

(a) Telephone connection 2010-11 15624

(b) Post offices 2010-11 Nos. 42 (PO) +11(TO)

(c) Telephone center 2010-11 Nos. 14

(d )Density of Telephone 2010-11 Nos./1000 person

(e) Density of Telephone 2010-11 No. per KM.

(f) PCO Rural 2010-11 No. 86

(g) PCO STD 2010-11 No. 82

(h) Mobile 2010-11 No. 15000


7

1.1 Location and Geographical Area An ancient state of "Mallyas" known for their bravery and love for civil liberty serves as the

frontier of Gopalganj. In Pre- historic time, Gopalganj was part of Nepal, up to the bank of the

Saryu river which bounds Siwan district on South of it. Siwan means the boundary - the Southern

boundary of Nepal Kingdom (earlier) Gopalganj, which till 1875 was only a tiny. Hamlet, was

made a subdivision of the old Saran district in the same year. The history of Gopalganj is a part of

the history of old Saran District. The composite Saran district lies on one of the main lines of the

Aryan advance. According to a tradition preserved in Vedic literature, the Videhas marched

eastwards from the Saraswati until they reached the banks of the Gandak and were informed by

Agni, the God of fire, that their home lay to the east of its broad stream. In obedience to his

directions, the Videhas crossed the river and founded a powerful kingdom on its eastern bank;

but it seems likely that some of them settled in Saran, while the majority of them crossed the

Gandak. Gopalganj is a town, municipality and headquarters of Gopalganj district in the Indian

state of Bihar. It was carved out of old Saran district (consisting of Chhapra, Siwan and Gopalganj)

on October 2, 1973. Gopalganj is one of the administrative districts in the Indian state of Bihar

and the district is a part of Saran Division.

It is one of the largest sugarcane producers in India. It also produces the best tobaccos

in the country. The district has provided the state with 3 chief ministers. Gopalganj is also

famous for producing large number of IAS and IPS officers. Geographical Location of Gopalganj

district lies between 26° 12 to 26° 39 North latitudes 83° 54 to 84° 55 East longitudes. The

district occupies an area of 2033 km² and is surrounded by - North: East & West Champaran

District, South: Siwan & Chappra District, East: East Champaran & Muzaffarpur District, West:

Uttar Pradesh. Gopalganj district is situated in the northwest part of the state. It lies between N

latitude 26012’ & 26039’ and E longitude between 83054’ & 84055’. It covers parts of Survey of

India toposheet Nos. 72 A/2, B/3, O/6, B/7, B/10, B/11 & B/25. This district comes under Indo-

Gangetic plain covering plain and Gandak-Ghaghra sub-basin. There are 14 development blocks

with two sub-basins. It is bounded by Uttar Pradesh on the north and west whereas by Gandak

river in the east and by Siwan district on south.

The district Gopalganj is having an area of 2033 sq.km with 14 blocks and 1564 villages. As per

2011 census the total population in the district is 2558037 with Rural 2396270 and Urban

161767.


8

1.2 Administrative Units:-

i) List of Tehsil/ Block:

Kuchaikote, Barauli, Hathua, Gopalganj,

Baikunthpur, Manjha, Bhorey, Uchkagaon,

Sidhwalia, Bijaipur, Katiya, Phulwaria, Thawe,

and Pach Deuri.

14 Blocks

ii) Number of Punchyat/Villages 1564

iii) Population (As on 2011 Census) 2558037

Rural population 2376270

Urban population 161767

1.3 Connectivity facilities in Gopalganj District:- Roads - The district of Gopalganj is well served by a network of roads. The roads are

classified as the National Highways, State Highways, Major district roads and other district

roads. They are maintained by the Public works Department, the Rural Engineering

Organisation, the Zila parishad, Municipalities. It is also connected with the interior of the

district by metalled road. Two National Highway and three State Highway Cross the

district. NH- 28 which connects the district to Gorakhpur, Uttar Pradesh and other parts of

Bihar and NH- 85 passes through the district and connects the district to Saran and Siwan,

Bihar. SH-45, SH-47 and SH-53 also pass through the district.

Railways - The district of Gopalganj has a well-knit communication system through

railways also. It is served by the North-Eastern Railway. The North-Eastern Railway has

two branches in the district. One runs through Siwan-Thawe-Gorakhpur and other

through Siwan-Thawe-Gopalganj- Chapra route. Five block headquarters of the district

have the privilege of being very near to the railway stations.

Airway - The district has a landing ground. There is, however, one landing ground at

Hathwa, where small airplane lands. However, there is no regular air service in the

district.

Waterway – Gopalganj being a riverine district, water transport plays an important role

in the means of transport. In the past, when the railways and other steam services were

not developed, boats were the chief means for transport of goods and passengers.

http://www.census2011.co.in/data/subdistrict/1225-manjha-gopalganj-bihar.html

http://www.census2011.co.in/data/subdistrict/1217-bhorey-gopalganj-bihar.html

http://www.census2011.co.in/data/subdistrict/1222-uchkagaon-gopalganj-bihar.html

http://www.census2011.co.in/data/subdistrict/1227-sidhwalia-gopalganj-bihar.html

http://www.census2011.co.in/data/subdistrict/1216-bijaipur-gopalganj-bihar.html

http://www.census2011.co.in/data/subdistrict/1215-katiya-gopalganj-bihar.html

http://www.census2011.co.in/data/subdistrict/1220-phulwaria-gopalganj-bihar.html

http://www.census2011.co.in/data/subdistrict/1223-thawe-gopalganj-bihar.html

http://www.census2011.co.in/data/subdistrict/1218-pach-deuri-gopalganj-bihar.html


9

Map showing location of Gopalganj district in Bihar


10

Representative Map of Gopalganj District

(Source: Geological Survey of India)


11

2. Overview of Mining Activity in the District

There is no mining and heavy industry in the district. There are no minerals except nodular limestone (kankar) of good quality which is found throughout the district. It is used for metalling roads and for ballast on the railway but the supply is diminishing. However, the district is rich in kiln brick production and has more than one hundred working brick kilns or bhatthas as on date.



12

3. List of Mining Lease in the District

3.1 List of Brick Field as per Dept. Record:- (Total 131)


13


14


15


16


17


18


19


20


21


22


23


24


25


26


27


28


29


30

3.2 List of Brick Kiln/Bhattha as per survey record (Total 147) : Sl. No. Thana / Block Village

Brick Field Name

Boundary

Points Longitude Latitude

1 THAWE VRINDAWAN 2X & 2X 84° 22' 51.58"E 26° 25' 6.2"N

2X & 2X A 84° 22' 50.76"E 26° 25' 5.59"N

2X & 2X B 84° 22' 51.69"E 26° 25' 7.94"N

2X & 2X C 84° 22' 52.28"E 26° 25' 7.73"N

2X & 2X D 84° 22' 51.34"E 26° 25' 5.33"N

2 THAWE VRINDAWAN 3X & 2X 84° 23' 13.48"E 26° 25' 10.26"N

3X & 2X A 84° 23' 13.5"E 26° 25' 11.47"N

3X & 2X B 84° 23' 14.29"E 26° 25' 11.2"N

3X & 2X C 84° 23' 13.6"E 26° 25' 9.2"N

3X & 2X D 84° 23' 12.73"E 26° 25' 9.5"N

3 THAWE VRINDAWAN 7X 84° 22' 52.86"E 26° 24' 44.03"N

7X A 84° 22' 51.89"E 26° 24' 43.32"N

7X B 84° 22' 52.78"E 26° 24' 42.96"N

7X C 84° 22' 53.89"E 26° 24' 45.21"N

7X D 84° 22' 53.14"E 26° 24' 45.36"N

4 MANJHAR MANJHAR A & U 84° 30' 38.14"E 26° 25' 1.88"N

A & U A 84° 30' 36.85"E 26° 25' 2.07"N

A & U B 84° 30' 38.88"E 26° 25' 1.23"N

A & U C 84° 30' 39.13"E 26° 25' 1.8"N

A & U D 84° 30' 36.98"E 26° 25' 2.65"N

5 VIJAYIPUR MUSHARI A+K 85° 0' 30.24"E 26° 36' 58.53"N

6 BAIKUNTHPUR RAVJUVTI A1 84° 44' 35.56"E 26° 15' 11.45"N

A1 A 84° 44' 34.68"E 26° 15' 11.22"N

A1 B 84° 44' 34.79"E 26° 15' 11.95"N

A1 C 84° 44' 36.82"E 26° 15' 11.67"N

A1 D 84° 44' 36.63"E 26° 15' 10.97"N

7 HATHUA CHAINPUR ABC 85° 19' 23.85"E 27° 19' 23.48"N

8 HATHUA KALOPALTI ABM 84° 16' 26.21"E 26° 33' 17.76"N

9 HATHUA HATHUA ABT 84° 18' 32.1"E 26° 20' 58.47"N

ABT A 84° 18' 31.95"E 26° 20' 59.37"N

ABT B 84° 18' 31.6"E 26° 20' 57.4"N

ABT C 84° 18' 32.18"E 26° 20' 57.31"N

ABT D 84° 18' 32.6"E 26° 20' 59.3"N

10 PHOOLWARIYA CHHATI AH 84° 15' 5.11"E 26° 28' 27.48"N

AH A 84° 15' 4.72"E 26° 28' 27.37"N

AH B 84° 15' 5.22"E 26° 28' 27.78"N

AH C 84° 15' 5.59"E 26° 28' 27.38"N

AH D 84° 15' 5.21"E 26° 28' 27.04"N

11 BAIKUNTHPUR MAHUA AJA 84° 21' 13.64"E 26° 29' 48.2"N

AJA A 84° 21' 12.98"E 26° 29' 47.28"N

AJA B 84° 21' 13.52"E 26° 29' 47.07"N

AJA C 84° 21' 14.41"E 26° 29' 48.96"N


31

AJA D 84° 21' 13.73"E 26° 29' 49.3"N

12 KATEYA MATHEYA AKP 84° 8' 10.13"E 26° 30' 22.61"N

13 HATHUA KALOPALTI AKS 84° 16' 26.83"E 26° 23' 16.75"N

14 KUCHAIKOT MAHAICHA AKS+PATEL 84° 21' 37.35"E 26° 22' 50.77"N

AKS+PATEL A 84° 21' 36.27"E 26° 22' 49.77"N

AKS+PATEL B 84° 21' 37.38"E 26° 22' 49.38"N

AKS+PATEL C 84° 21' 38.11"E 26° 22' 51.81"N

AKS+PATEL D 84° 21' 37.25"E 26° 22' 52.01"N

AKS A 84° 16' 26.28"E 26° 23' 15.93"N

AKS B 84° 16' 26.74"E 26° 23' 17.61"N

AKS C 84° 16' 27.58"E 26° 23' 17.42"N

AKS D 84° 16' 26.89"E 26° 23' 15.75"N

15 THAWE VRINDAWAN AKY 84° 21' 49.04"E 26° 23' 15.69"N

AKY A 84° 21' 48.57"E 26° 23' 16.33"N

AKY B 84° 21' 48.29"E 26° 23' 15.32"N

AKY C 84° 21' 49.49"E 26° 23' 15.06"N

AKY D 84° 21' 49.7"E 26° 23' 16.07"N

16 VIJAYIPUR GHURANAKUND AM 84° 3' 46.36"E 26° 33' 3.94"N

AM A 84° 3' 45.72"E 26° 33' 2.85"N

AM B 84° 3' 47.47"E 26° 33' 4.41"N

AM C 84° 3' 47.06"E 26° 33' 4.79"N

AM D 84° 3' 45.29"E 26° 33' 3.16"N

17 UCHKAGAON SALONA AMAR 84° 35' 23.2"E 26° 23' 50.55"N

AMAR A 84° 35' 23.01"E 26° 23' 51.51"N

AMAR B 84° 35' 23.93"E 26° 23' 51.29"N

AMAR C 84° 35' 23.32"E 26° 23' 48.98"N

AMAR D 84° 35' 22.31"E 26° 23' 49.15"N

18 VIJAYIPUR KALYANAPUR ANIL 84° 3' 51.32"E 26° 33' 20.07"N

ANIL A 84° 3' 49.91"E 26° 33' 20.09"N

ANIL B 84° 3' 52.34"E 26° 33' 19.27"N

ANIL C 84° 3' 52.73"E 26° 33' 19.89"N

ANIL D 84° 3' 50.39"E 26° 33' 20.72"N

19 GOPALGANJ YADAHAV TOLA ASHOK 84° 28' 2.76"E 26° 28' 47.13"N

ASHOK A 84° 28' 1.96"E 26° 28' 46.32"N

ASHOK B 84° 28' 2.83"E 26° 28' 46.18"N

ASHOK C 84° 28' 3.29"E 26° 28' 47.89"N

ASHOK D 84° 28' 2.66"E 26° 28' 48.1"N

20 VIJAYIPUR MAJHALIYA ASJ 84° 1' 17.93"E 26° 29' 20.91"N

ASJ A 84° 1' 17.11"E 26° 29' 19.58"N

ASJ B 84° 1' 17.87"E 26° 29' 19.4"N

ASJ C 84° 1' 18.86"E 26° 29' 22.35"N

ASJ D 84° 1' 18.12"E 26° 29' 22.59"N

21 GOPALGANJ ADARSH NAGAR BARALI ASM 84° 36' 12.26"E 26° 22' 45.61"N

ASM A 84° 36' 11.54"E 26° 22' 44.9"N


32

ASM B 84° 36' 12.45"E 26° 22' 44.64"N

ASM C 84° 36' 12.89"E 26° 22' 46.52"N

ASM D 84° 36' 12.14"E 26° 22' 46.72"N

22 UCHKAGAON MATHOLI BABA 84° 19' 10.22"E 26° 27' 4.28"N

23 BHOREY KALYANPUR BDY 84° 10' 1.15"E 26° 28' 40.94"N

BDY A 84° 10' 1.27"E 26° 28' 41.85"N

BDY B 84° 10' 0.48"E 26° 28' 40.01"N

BDY C 84° 10' 1.3"E 26° 28' 39.9"N

BDY D 84° 10' 1.92"E 26° 28' 41.62"N

24 KUCHAIKOT MAHAICHA BHARAT 84° 21' 37.75"E 26° 22' 33.44"N

BHARAT A 84° 21' 36.8"E 26° 22' 32.37"N

BHARAT B 84° 21' 37.94"E 26° 22' 34.86"N

BHARAT C 84° 21' 38.66"E 26° 22' 34.56"N

BHARAT D 84° 21' 37.61"E 26° 22' 32.23"N

25 THAWE KHANPUR BHAVAN 84° 18' 17.79"E 26° 21' 26.66"N

BHAVAN A 84° 18' 18.92"E 26° 21' 26.31"N

BHAVAN B 84° 18' 18.55"E 26° 21' 25.83"N

BHAVAN C 84° 18' 16.54"E 26° 21' 27.08"N

BHAVAN D 84° 18' 17.09"E 26° 21' 27.45"N

26 THAWE KHANPUR BHAVAN 84° 22' 2.38"E 26° 23' 49"N

BHAVAN A 84° 22' 1.65"E 26° 23' 48.33"N

BHAVAN B 84° 22' 2.42"E 26° 23' 48.02"N

BHAVAN C 84° 22' 3.18"E 26° 23' 49.94"N

BHAVAN D 84° 22' 2.58"E 26° 23' 50.17"N

27 HATHUA HATHUA BHAWAN 84° 18' 8.41"E 26° 20' 56.06"N

28 GOPALGANJ SURBAL BHR 84° 33' 52.44"E 26° 22' 20.93"N

BHR A 84° 33' 51.28"E 26° 22' 20.9"N

BHR B 84° 33' 52.43"E 26° 22' 19.98"N

BHR C 84° 33' 53.18"E 26° 22' 20.63"N

BHR D 84° 33' 52.04"E 26° 22' 21.5"N

29 BAIKUNTHPUR DIGHWA DUBAULI BHRI 84° 43' 39.53"E 26° 14' 52.94"N

BHRI A 84° 43' 40.47"E 26° 14' 52.91"N

BHRI B 84° 43' 40.19"E 26° 14' 52.4"N

BHRI C 84° 43' 38.51"E 26° 14' 52.75"N

BHRI D 84° 43' 38.69"E 26° 14' 53.38"N

30 BHOREY JIGINA BNS 84° 6' 35.45"E 26° 29' 42.5"N

31 Brick Field 1 84° 1' 16.4"E 26° 30' 27.67"N

Brick Field 1 A 84° 1' 16.61"E 26° 30' 28.76"N

Brick Field 1 B 84° 1' 15.96"E 26° 30' 26.31"N

Brick Field 1 C 84° 1' 16.46"E 26° 30' 26.27"N

Brick Field 1 D 84° 1' 17.24"E 26° 30' 28.55"N

32 MANJHA MIRALLIPUR Brick Field 2 84° 28' 36.47"E 26° 27' 14.93"N

Brick Field 2 A 84° 28' 36.37"E 26° 27' 16.1"N

Brick Field 2 B 84° 28' 35.54"E 26° 27' 13.94"N


33

Brick Field 2 C 84° 28' 36.44"E 26° 27' 13.65"N

Brick Field 2 D 84° 28' 37.17"E 26° 27' 15.85"N

33 MANJHA MIRALLIPUR Brick Field 3 84° 28' 52.43"E 26° 27' 14.97"N

34 GOPALGANJ NAWADA Brick Field 4 84° 26' 42.42"E 26° 30' 8.83"N

35 BARAULI Brick Field 5 84° 33' 17.11"E 26° 22' 9.15"N

Brick Field 5 A 84° 33' 16.86"E 26° 22' 8.36"N

Brick Field 5 B 84° 33' 17.72"E 26° 22' 9.15"N

Brick Field 5 C 84° 33' 16.91"E 26° 22' 9.71"N

Brick Field 5 D 84° 33' 16.18"E 26° 22' 9.22"N

36 HATHUA Brick Field 6 84° 16' 0.66"E 26° 20' 2.28"N

37 HATHUA Brick Field 7 84° 16' 2.35"E 26° 20' 32.48"N

38 HATHUA PAKRI Brick Field 8 84° 15' 28.64"E 26° 22' 47.05"N

Brick Field 8 A 84° 15' 29.91"E 26° 22' 46.4"N

Brick Field 8 B 84° 15' 30.14"E 26° 22' 47.11"N

Brick Field 8 C 84° 15' 27.93"E 26° 22' 47.79"N

Brick Field 8 D 84° 15' 27.62"E 26° 22' 47.33"N

39 UCHKAGAON CHANDPARNA CASH 84° 38' 53.93"E 26° 20' 59.55"N

CASH A 84° 38' 54.12"E 26° 21' 0.77"N

CASH B 84° 38' 54.8"E 26° 21' 0.55"N

CASH C 84° 38' 53.77"E 26° 20' 58.43"N

CASH D 84° 38' 53.05"E 26° 20' 58.71"N

40 KATHUA GHATMIHTA CDS 84° 18' 42.51"E 26° 23' 34.98"N

CDS A 84° 18' 41.61"E 26° 23' 35.52"N

CDS B 84° 18' 41.48"E 26° 23' 34.88"N

CDS C 84° 18' 43.09"E 26° 23' 34.48"N

CDS D 84° 18' 43.37"E 26° 23' 35.13"N

41 GOPALGANJ RATAN SARAI CITY 84° 33' 44.58"E 26° 23' 10.78"N

CITY A 84° 33' 43.66"E 26° 23' 10.1"N

CITY B 84° 33' 44.33"E 26° 23' 9.77"N

CITY C 84° 33' 45.73"E 26° 23' 11.74"N

CITY D 84° 33' 45.05"E 26° 23' 12.1"N



CITY A 84° 34' 2.43"E 26° 22' 59.82"N

CITY B 84° 34' 3.52"E 26° 22' 59.49"N

CITY C 84° 34' 2.67"E 26° 22' 57.34"N

CITY D 84° 34' 1.88"E 26° 22' 57.61"N

44 HATHUA CHAINPUR DNR 85° 19' 24.83"E 27° 19' 23.5"N

45 HATHUA CHAINPUR DNR 84° 14' 39.58"E 26° 17' 39.14"N

46 KATEYA SAMOBAR ESB 84° 3' 57.35"E 26° 34' 8.13"N

ESB A 84° 3' 56.73"E 26° 34' 6.82"N

ESB B 84° 3' 57.46"E 26° 34' 9.32"N

ESB C 84° 3' 58.13"E 26° 34' 9.14"N

ESB D 84° 3' 57.39"E 26° 34' 6.69"N

47 GOPALGANJ BRACHA GOLD 84° 32' 25.98"E 26° 21' 18.08"N


34

GOLD A 84° 32' 25.47"E 26° 21' 17.62"N

GOLD B 84° 32' 25.85"E 26° 21' 19.37"N

GOLD C 84° 32' 26.54"E 26° 21' 19.22"N

GOLD D 84° 32' 26.14"E 26° 21' 17.36"N

48 SIDHWALIA SARIYA GORI 84° 38' 12.4"E 26° 20' 34.42"N

GORI A 84° 38' 12.1"E 26° 20' 35.45"N

GORI B 84° 38' 12.92"E 26° 20' 35.19"N

GORI C 84° 38' 12.43"E 26° 20' 33.16"N

GORI D 84° 38' 11.65"E 26° 20' 33.39"N

49 HATHUA JIGANA MORE HERO 84° 38' 49.57"E 26° 19' 13.55"N

50 HATHUA JIGANA MORE HERO 85° 19' 58.96"E 26° 20' 18.87"N

HERO A 84° 38' 49.89"E 26° 19' 14.71"N

HERO B 84° 38' 50.51"E 26° 19' 14.48"N

HERO C 84° 38' 49.45"E 26° 19' 12.63"N

HERO D 84° 38' 48.73"E 26° 19' 12.91"N

51 HATHUA JIGNA MINGANJ HIRA 84° 20' 18.23"E 26° 20' 29.94"N

52 HATHUA JIGNA MINGANJ HIRA 84° 21' 10.94"E 26° 21' 58.23"N

HIRA A 84° 20' 17.78"E 26° 20' 29.33"N

HIRA B 84° 20' 18.45"E 26° 20' 29.33"N

HIRA C 84° 20' 18.72"E 26° 20' 30.75"N

HIRA D 84° 20' 18.19"E 26° 20' 30.79"N

53 KUCHAIKOTE PIPRAHI HMT 84° 20' 16.55"E 26° 29' 37.38"N

HMT A 84° 20' 16.57"E 26° 29' 38.26"N

HMT B 84° 20' 15.79"E 26° 29' 36.72"N

HMT C 84° 20' 15.92"E 26° 29' 50.46"N

HMT D 84° 20' 17.32"E 26° 29' 37.94"N

54 KUCHAIKOTE PIPRAHI HMT 84° 20' 15.02"E 26° 29' 49.54"N

HMT A 84° 20' 14.04"E 26° 29' 48.39"N

HMT B 84° 20' 14.72"E 26° 29' 48.13"N

HMT C 84° 20' 16.49"E 26° 29' 36.37"N

HMT D 84° 20' 14.92"E 26° 29' 50.74"N

55 VIJAYIPUR HP 84° 7' 10.44"E 26° 36' 53.52"N

HP A 84° 7' 10.13"E 26° 36' 54.5"N

HP B 84° 7' 10.07"E 26° 36' 52.54"N

HP C 84° 7' 10.64"E 26° 36' 52.49"N

HP D 84° 7' 10.86"E 26° 36' 54.5"N

56 GOPALGANJ JAJ 84° 25' 29.47"E 26° 30' 27.35"N

JAJ A 84° 25' 28.08"E 26° 30' 27.6"N

JAJ B 84° 25' 30.6"E 26° 30' 26.59"N

JAJ C 84° 25' 31.05"E 26° 30' 27.03"N

JAJ D 84° 25' 28.36"E 26° 30' 28.15"N

57 UNCHKAGAON JAGARNATHA JANTA 84° 16' 21.63"E 26° 24' 39.4"N





35


JANTA A 84° 28' 2.42"E 26° 27' 54.64"N

JANTA A 84° 18' 9.56"E 26° 27' 8.99"N

JANTA A 84° 16' 20.26"E 26° 24' 39.35"N

JANTA B 84° 28' 3.04"E 26° 27' 54.49"N

JANTA B 84° 18' 10.36"E 26° 27' 8.86"N

JANTA B 84° 16' 22.63"E 26° 24' 39.01"N

JANTA C 84° 28' 3.91"E 26° 27' 56.09"N

JANTA C 84° 18' 10.89"E 26° 27' 10.45"N

JANTA C 84° 16' 22.7"E 26° 24' 39.52"N

JANTA D 84° 28' 3.12"E 26° 27' 56.26"N

JANTA D 84° 18' 10.12"E 26° 27' 10.65"N

JANTA D 84° 16' 20.25"E 26° 24' 39.86"N

62 KUCHAIKOT MADHOMATH CHAWK JAWAL 84° 22' 56.71"E 26° 30' 13.5"N

JAWAL A 84° 22' 56.83"E 26° 30' 14.64"N

JAWAL B 84° 22' 56.69"E 26° 30' 12.62"N

JAWAL C 84° 22' 55.91"E 26° 30' 12.85"N

JAWAL D 84° 22' 57.49"E 26° 30' 14.42"N

63 KATEYA SUKSENWA JMD 84° 8' 29.47"E 26° 38' 9.13"N

JMD A 84° 8' 30.49"E 26° 38' 8.07"N

JMD B 84° 8' 28.28"E 26° 38' 9.48"N

JMD C 84° 8' 28.77"E 26° 38' 10.09"N

JMD D 84° 8' 31"E 26° 38' 8.56"N

64 BIJAIPUR BARKATTA KBF 84° 1' 29.96"E 26° 27' 43.06"N

KBF A 84° 1' 30.75"E 26° 27' 44.1"N

KBF B 84° 1' 29.88"E 26° 27' 41.75"N

KBF C 84° 1' 29.21"E 26° 27' 41.86"N

KBF D 84° 1' 29.86"E 26° 27' 44.28"N

65 PHOOLWARIYA FAKARPUR KISAN 84° 11' 50.23"E 26° 26' 40.22"N

KISAN A 84° 11' 50.36"E 26° 26' 41.5"N

KISAN B 84° 11' 49.54"E 26° 26' 39.17"N

KISAN C 84° 11' 50.05"E 26° 26' 39"N

KISAN D 84° 11' 50.96"E 26° 26' 41.38"N

66 VIJAYIPUR BHARPURA KY 84° 1' 14.3"E 26° 30' 28.4"N

67 KATEYA RUDALPUR MB 84° 0' 27.61"E 26° 34' 29.52"N

68 KATEYA RUDALPUR MB 84° 6' 29.72"E 26° 37' 49.99"N

MB A 84° 6' 29.65"E 26° 37' 51.28"N

MB B 84° 6' 29.13"E 26° 37' 48.64"N

MB C 84° 6' 29.86"E 26° 37' 48.6"N

MB D 84° 6' 30.26"E 26° 37' 51.22"N

69 HATHUA BIGHIJAGEDISH MBF 85° 15' 27.97"E 26° 22' 37.75"N

70 HATHUA Farhadwa MFI 84° 14' 45.77"E 26° 21' 58.24"N

MFI A 84° 14' 46.18"E 26° 21' 59.57"N

MFI B 84° 14' 44.65"E 26° 21' 57.21"N


36

MFI C 84° 14' 45.47"E 26° 21' 56.91"N

MFI D 84° 14' 46.8"E 26° 21' 59.29"N

71 KUCHAIKOTE MAHUBALA MK 84° 20' 44.74"E 26° 29' 57.6"N

72 KUCHAIKOTE MAHUBALA MK 84° 20' 54.07"E 26° 29' 53.51"N

MK A 84° 20' 43.71"E 26° 29' 57"N

MK B 84° 20' 44.11"E 26° 29' 56.61"N

MK C 84° 20' 45.83"E 26° 29' 58.18"N

MK D 84° 20' 45.13"E 26° 29' 58.58"N

73 HATHUA MUNRERA MOTI 84° 18' 31.67"E 26° 20' 52.94"N

74 KATEYA SUKSENWA MP 84° 6' 53.44"E 26° 35' 51.76"N

MP A 84° 6' 52.7"E 26° 35' 50.6"N

MP B 84° 6' 53.29"E 26° 35' 50.4"N

MP C 84° 6' 54.29"E 26° 35' 53.06"N

MP D 84° 6' 53.56"E 26° 35' 53.21"N


MP A 84° 7' 53.66"E 26° 37' 15.03"N

MP B 84° 7' 53.75"E 26° 37' 15.62"N

MP C 84° 7' 51.41"E 26° 37' 16.42"N

MP D 84° 7' 50.99"E 26° 37' 15.66"N


MP A 84° 3' 40.86"E 26° 33' 22.69"N

MP B 84° 3' 41.61"E 26° 33' 22.5"N

MP C 84° 3' 42.42"E 26° 33' 25.1"N

MP D 84° 3' 41.65"E 26° 33' 25.23"N



MP A 84° 4' 34.39"E 26° 33' 36"N

MP B 84° 4' 37.23"E 26° 33' 35.79"N

MP C 84° 4' 37.04"E 26° 33' 35.16"N

MP D 84° 4' 34.48"E 26° 33' 35.35"N

79 KATEYA SUKSENWA MP 84° 4' 1.24"E 26° 34' 3"N

MP A 84° 4' 1.1"E 26° 34' 4.29"N

MP B 84° 4' 0.85"E 26° 34' 1.61"N

MP C 84° 4' 1.43"E 26° 34' 1.56"N

MP D 84° 4' 1.77"E 26° 34' 4.22"N


MP A 84° 8' 45.03"E 26° 37' 53.42"N

MP B 84° 8' 45.82"E 26° 37' 53.23"N

MP C 84° 8' 46.27"E 26° 37' 55.78"N

MP D 84° 8' 45.61"E 26° 37' 55.84"N

81 VIJAYIPUR SAMOGAR MS 84° 3' 45.01"E 26° 32' 43.42"N

MS A 84° 3' 43.95"E 26° 32' 43.9"N

MS B 84° 3' 43.72"E 26° 32' 43.29"N

MS C 84° 3' 46.08"E 26° 32' 42.69"N

MS D 84° 3' 46.41"E 26° 32' 43.29"N


37

82 GOPALGANJ BARALI NAGINA 84° 36' 15.67"E 26° 22' 46.44"N

NAGINA A 84° 36' 15.34"E 26° 22' 47.63"N

NAGINA B 84° 36' 14.99"E 26° 22' 45.1"N

NAGINA C 84° 36' 15.75"E 26° 22' 44.94"N

NAGINA D 84° 36' 16.35"E 26° 22' 47.45"N

83 KUCHAIKOT BELWA NKL 84° 23' 20.25"E 26° 30' 19.87"N

NKL A 84° 23' 19.22"E 26° 30' 19.9"N

NKL B 84° 23' 21.01"E 26° 30' 19.38"N

NKL C 84° 23' 21.35"E 26° 30' 19.97"N

NKL D 84° 23' 19.51"E 26° 30' 20.43"N

84 KATHUA GASAI PIPRA NM 84° 18' 43.96"E 26° 23' 5.65"N

NM A 84° 18' 43.12"E 26° 23' 5.92"N

NM B 84° 18' 43.74"E 26° 23' 4.97"N

NM C 84° 18' 44.67"E 26° 23' 5.74"N

NM D 84° 18' 44.03"E 26° 23' 6.32"N

85 MANJHAR BRINTOLA PATNA 84° 30' 55.83"E 26° 24' 17.18"N

PATNA A 84° 30' 54.49"E 26° 24' 17.41"N

PATNA B 84° 30' 54.66"E 26° 24' 16.75"N

PATNA C 84° 30' 57.34"E 26° 24' 17.2"N

PATNA D 84° 30' 57.05"E 26° 24' 17.85"N

86 UNCHKAGAON HARPUR PAWAN 84° 20' 21.35"E 26° 29' 1.04"N

87 UNCHKAGAON HARPUR PAWAN 84° 20' 28.04"E 26° 29' 8.42"N

PAWAN A 84° 20' 27.43"E 26° 29' 7.55"N

PAWAN B 84° 20' 28.13"E 26° 29' 7.43"N

PAWAN C 84° 20' 28.83"E 26° 29' 9.48"N

PAWAN D 84° 20' 28.08"E 26° 29' 9.73"N

88 VIJAYIPUR GANGA CHAPPAR PBB 84° 1' 51.12"E 26° 27' 35.81"N

PBB A 84° 1' 50.59"E 26° 27' 35.07"N

PBB B 84° 1' 51.13"E 26° 27' 36.77"N

PBB C 84° 1' 51.79"E 26° 27' 36.48"N

PBB D 84° 1' 51.19"E 26° 27' 34.8"N

89 GOPALGANJ BAGARIYADAWA PDS 84° 25' 14.14"E 26° 29' 58.3"N

90 BHOREY DUMAR NARENDRA PNS 84° 6' 34.22"E 26° 27' 36.08"N

PNS A 84° 6' 34.6"E 26° 27' 37.08"N

PNS B 84° 6' 33.35"E 26° 27' 35"N

PNS C 84° 6' 34.08"E 26° 27' 34.73"N

PNS D 84° 6' 35.31"E 26° 27' 36.84"N

91 KATEYA RASAUTI PR 84° 7' 10.21"E 26° 33' 22.89"N

PR A 84° 7' 9.64"E 26° 33' 22.14"N

PR B 84° 7' 10.19"E 26° 33' 23.69"N

PR C 84° 7' 10.75"E 26° 33' 23.47"N

PR D 84° 7' 10.3"E 26° 33' 22.06"N

92 UCHKAGAON PASAINI PX 84° 20' 32.75"E 26° 29' 20.23"N


38

PX A 84° 20' 32.14"E 26° 29' 20.02"N

PX B 84° 20' 33.31"E 26° 29' 19.65"N

PX C 84° 20' 33.54"E 26° 29' 20.66"N

PX D 84° 20' 32.46"E 26° 29' 20.96"N

93 BHOREY RAUDAPUR R+Y 84° 4' 47.82"E 26° 27' 18.87"N

R+Y A 84° 4' 46.39"E 26° 27' 19.44"N

R+Y B 84° 4' 46.2"E 26° 27' 18.8"N

R+Y C 84° 4' 49.07"E 26° 27' 18.04"N

R+Y D 84° 4' 49.46"E 26° 27' 18.65"N

94 HATHUA SOHAGEPUR RAHI 84° 18' 31.85"E 26° 20' 8.65"N

RAHI A 84° 18' 33.02"E 26° 20' 8.18"N

RAHI B 84° 18' 32.92"E 26° 20' 8.78"N

RAHI C 84° 18' 30.76"E 26° 20' 9.02"N

RAHI D 84° 18' 30.78"E 26° 20' 8.31"N

95 HATHUA BIGHIJAGEDISH RAJA 84° 15' 49.49"E 26° 22' 40.78"N



RAJA A 84° 15' 49.53"E 26° 22' 41.96"N

RAJA B 84° 15' 49.06"E 26° 22' 39.91"N

RAJA C 84° 15' 49.54"E 26° 22' 39.83"N

RAJA D 84° 15' 50.2"E 26° 22' 41.93"N

98 HATHUA RATANCHAK RAJAN 84° 18' 9.12"E 26° 21' 8.12"N

99 HATHUA RATANCHAK RAJAN 84° 18' 8.29"E 26° 21' 0.36"N

RAJAN A 84° 18' 8.66"E 26° 21' 7.3"N

RAJAN B 84° 18' 9.17"E 26° 21' 7.18"N

RAJAN C 84° 18' 9.69"E 26° 21' 8.9"N

RAJAN D 84° 18' 9.12"E 26° 21' 9.08"N

100 UCHKAGAON SIYAVALIYA RAJU 84° 39' 25.89"E 26° 20' 31.81"N

RAJU A 84° 39' 27.1"E 26° 20' 31.8"N

RAJU B 84° 39' 24.66"E 26° 20' 32.25"N

RAJU C 84° 39' 24.56"E 26° 20' 31.67"N

RAJU D 84° 39' 26.94"E 26° 20' 31.15"N

101 UCHKAGAON BHULWAR RAMA 84° 18' 2.25"E 26° 24' 36.28"N

RAMA A 84° 18' 1.88"E 26° 24' 35.62"N

RAMA B 84° 18' 1.3"E 26° 24' 36.43"N

RAMA C 84° 18' 2.22"E 26° 24' 37"N

RAMA D 84° 18' 3.13"E 26° 24' 36.28"N

102 BHOREY DUMAR NARENDRA RCS 84° 6' 35.6"E 26° 28' 42.39"N

103 KATEYA BATWANIYA RM 84° 4' 6.6"E 26° 33' 39.18"N

104 GOPALGANJ BARALI BHARUKURWA ROSE 84° 35' 54.88"E 26° 22' 23.2"N

ROSE A 84° 35' 54.31"E 26° 22' 22.3"N

ROSE B 84° 35' 55.12"E 26° 22' 22.21"N

ROSE C 84° 35' 55.39"E 26° 22' 24.26"N


39

ROSE D 84° 35' 54.72"E 26° 22' 24.36"N

105 BAIKUNTHPUR RPS 84° 43' 55.02"E 26° 15' 6.97"N

RPS A 84° 43' 54.99"E 26° 15' 8.13"N

RPS B 84° 43' 55.91"E 26° 15' 7.86"N

RPS C 84° 43' 54.92"E 26° 15' 5.53"N

RPS D 84° 43' 54.06"E 26° 15' 5.79"N

106 KATEYA RS 84° 6' 37.62"E 26° 34' 33.29"N

RS A 84° 6' 36.39"E 26° 34' 33.37"N

RS B 84° 6' 38.66"E 26° 34' 32.75"N

RS C 84° 6' 39.06"E 26° 34' 33.14"N

RS D 84° 6' 36.75"E 26° 34' 33.96"N

107 THAWE VRINDAWAN RX & OX 84° 22' 55.28"E 26° 25' 18.21"N

S_A 84° 7' 4.1"E 26° 35' 51.79"N

S_B 84° 7' 6.9"E 26° 35' 51.09"N

S_C 84° 7' 6.56"E 26° 35' 50.55"N

S_D 84° 7' 3.93"E 26° 35' 51.17"N

108 GOPALGANJ NAKA TOLA KHARNI SATHI 84° 36' 32.92"E 26° 22' 32.17"N

SATHI A 84° 36' 32.77"E 26° 22' 33.11"N

SATHI B 84° 36' 33.53"E 26° 22' 32.88"N

SATHI C 84° 36' 32.86"E 26° 22' 30.87"N

SATHI D 84° 36' 32.17"E 26° 22' 31.24"N

109 HATHUA FARAHDAWA SBI 84° 14' 47.45"E 26° 22' 39.82"N

110 UCHKAGAON VITTI TOLA SBS 84° 18' 59.74"E 26° 24' 3.27"N

SBS A 84° 18' 58.97"E 26° 24' 2.43"N

SBS B 84° 18' 59.54"E 26° 24' 2.16"N

SBS C 84° 19' 0.46"E 26° 24' 3.99"N

SBS D 84° 18' 59.88"E 26° 24' 4.35"N

111 VIJAYIPUR UDAYPURA SCR 84° 1' 16.17"E 26° 29' 55.9"N

SCR A 84° 1' 16.3"E 26° 29' 57.45"N

SCR B 84° 1' 15.44"E 26° 29' 54.65"N

SCR C 84° 1' 16.09"E 26° 29' 54.44"N

SCR D 84° 1' 17.11"E 26° 29' 56.97"N

112 UCHKAGAON KOTWA SK 84° 34' 17.38"E 26° 23' 57.82"N

SK A 84° 34' 18.21"E 26° 23' 59"N

SK B 84° 34' 17.13"E 26° 23' 59.22"N

SK C 84° 34' 16.76"E 26° 23' 56.55"N

SK D 84° 34' 17.56"E 26° 23' 56.45"N

113 MANJHAR PHULBARIYA SKY 84° 30' 42.66"E 26° 23' 45.75"N

SKY A 84° 30' 42.39"E 26° 23' 46.97"N

SKY B 84° 30' 42.07"E 26° 23' 45.1"N

SKY C 84° 30' 42.69"E 26° 23' 44.94"N

SKY D 84° 30' 43.16"E 26° 23' 46.73"N

114 BHOREY DUMAR NARENDRA SON 84° 6' 37.52"E 26° 28' 42.39"N


40

115 SIDHWALIA BRAMPURA SONA 84° 38' 43.73"E 26° 20' 19.97"N

SON A 84° 6' 37.74"E 26° 28' 43.71"N

SONA A 84° 38' 43.92"E 26° 20' 21.26"N

SONA B 84° 38' 43.03"E 26° 20' 19.26"N

SONA C 84° 38' 43.67"E 26° 20' 19.06"N

SONA D 84° 38' 44.52"E 26° 20' 21.09"N

SON B 84° 6' 36.66"E 26° 28' 41.48"N

SON C 84° 6' 37.21"E 26° 28' 41.19"N

SON D 84° 6' 38.44"E 26° 28' 43.46"N

116 GOPALGANJ BRACHA SONE 84° 32' 14.98"E 26° 21' 21.53"N

SONE A 84° 32' 14.87"E 26° 21' 22.09"N

SONE B 84° 32' 14.26"E 26° 21' 21.44"N

SONE C 84° 32' 15.01"E 26° 21' 20.95"N

SONE D 84° 32' 15.74"E 26° 21' 21.62"N

117 VIJAYIPUR RAMPUR AHIYAPUR SP 84° 7' 5.33"E 26° 35' 51.15"N



SP A 84° 3' 35.96"E 26° 33' 4.7"N

SP B 84° 3' 35.75"E 26° 33' 2.23"N

120 KATEYA DHARAMALA SPC 84° 6' 55.49"E 26° 34' 18.14"N

SP C 84° 3' 36.32"E 26° 33' 2.12"N

SPC A 84° 6' 55.56"E 26° 34' 19.05"N

SPC B 84° 6' 54.9"E 26° 34' 17.04"N

SPC C 84° 6' 55.41"E 26° 34' 16.9"N

SPC D 84° 6' 56.16"E 26° 34' 18.83"N

SP D 84° 3' 36.91"E 26° 33' 4.62"N

121 VIJAYIPUR DHOUWAL BAZAR SPG 84° 2' 7.87"E 26° 28' 25.94"N

SPG A 84° 2' 6.59"E 26° 28' 25.99"N

SPG B 84° 2' 8.98"E 26° 28' 25.27"N

SPG C 84° 2' 9.22"E 26° 28' 25.63"N

SPG D 84° 2' 6.84"E 26° 28' 26.39"N

122 GOPALGANJ HARIHARPUR SPS 84° 25' 47.32"E 26° 31' 4.97"N

SPS A 84° 25' 47.57"E 26° 31' 5.99"N

SPS B 84° 25' 46.67"E 26° 31' 4"N

SPS C 84° 25' 47.38"E 26° 31' 3.82"N

SPS D 84° 25' 48.21"E 26° 31' 5.76"N

123 BHOREY KALYANPUR SRY 84° 10' 5.1"E 26° 29' 5.53"N

SRY A 84° 10' 4.35"E 26° 29' 5.91"N

SRY B 84° 10' 4.33"E 26° 29' 5.46"N

SRY C 84° 10' 6.15"E 26° 29' 5.16"N

SRY D 84° 10' 6.28"E 26° 29' 5.77"N

124 HATHUA MADHAGAR SSB 84° 16' 9.61"E 26° 27' 50.47"N


41

125 HATHUA MADHAGAR SSB 84° 15' 14.48"E 26° 22' 40.56"N

126 PHOOLWARIA BHARPATIA STAR 84° 14' 45.61"E 26° 26' 52.28"N

STAR A 84° 14' 45.56"E 26° 26' 53.46"N

STAR B 84° 14' 44.83"E 26° 26' 51.57"N

STAR C 84° 14' 45.43"E 26° 26' 51.31"N

STAR D 84° 14' 46.08"E 26° 26' 53.25"N


STAR A 84° 15' 26.35"E 26° 27' 15.93"N

STAR B 84° 15' 25.28"E 26° 27' 13.3"N

STAR C 84° 15' 25.9"E 26° 27' 13.11"N

STAR D 84° 15' 27"E 26° 27' 15.65"N



STAR A 84° 39' 45.55"E 26° 23' 3.58"N

STAR B 84° 39' 46.44"E 26° 23' 3.18"N

STAR C 84° 39' 45.28"E 26° 23' 1.09"N

STAR D 84° 39' 44.5"E 26° 23' 1.63"N

130 HATHUA JIGANADOLA SUN 85° 19' 58.96"E 26° 20' 5.12"N

131 BAIKUNTHPUR DHIWA SUPER 84° 45' 18.83"E 26° 17' 7.65"N

SUPER A 84° 45' 18.68"E 26° 17' 8.72"N

SUPER B 84° 45' 19.37"E 26° 17' 8.61"N

SUPER C 84° 45' 19"E 26° 17' 6.55"N

SUPER D 84° 45' 18.41"E 26° 17' 6.67"N

132 KUCHAIKOTE KHARHARWA TATA 84° 21' 18.6"E 26° 29' 39.91"N

133 KATHUA KANGOPI USHA 84° 18' 44.05"E 26° 24' 14.87"N

USHA A 84° 18' 43.98"E 26° 24' 16.13"N

USHA B 84° 18' 43.27"E 26° 24' 13.75"N

USHA C 84° 18' 43.93"E 26° 24' 13.57"N

USHA D 84° 18' 44.77"E 26° 24' 15.93"N

134 HATHUA CHAINPUR VAP 84° 16' 26.46"E 26° 20' 14.82"N

VAP A 84° 16' 26.65"E 26° 20' 15.39"N

VAP B 84° 16' 25.77"E 26° 20' 14.65"N

VAP C 84° 16' 26.19"E 26° 20' 14.33"N

VAP D 84° 16' 27.1"E 26° 20' 15.19"N

135 HATHUA BABHNETI VBF 84° 18' 11.09"E 26° 23' 33.34"N

136 UNCHKAGAON HARPUR VIP 84° 38' 38.2"E 26° 19' 51.66"N

VIP A 84° 38' 37.7"E 26° 19' 52.44"N

VIP B 84° 38' 37.39"E 26° 19' 50.74"N

VIP C 84° 38' 38.27"E 26° 19' 50.52"N

VIP D 84° 38' 38.69"E 26° 19' 52.38"N


VIP A 84° 20' 30.54"E 26° 28' 55.03"N

VIP B 84° 20' 29.82"E 26° 28' 52.97"N

VIP C 84° 20' 30.39"E 26° 28' 52.82"N

VIP D 84° 20' 31.08"E 26° 28' 54.9"N


42





VIP A 84° 20' 18.84"E 26° 29' 17.56"N

VIP B 84° 20' 18.31"E 26° 29' 17.68"N

VIP C 84° 20' 18.86"E 26° 29' 19.23"N

VIP D 84° 20' 19.37"E 26° 29' 19"N

142 BHOREY VISAL 84° 6' 23.76"E 26° 28' 26.17"N

VISAL A 84° 6' 25.21"E 26° 28' 25.89"N

VISAL B 84° 6' 24.92"E 26° 28' 25.33"N

VISAL C 84° 6' 22.16"E 26° 28' 26.22"N

VISAL D 84° 6' 22.52"E 26° 28' 26.91"N

143 VIJAYIPUR BARKUIYA VKS 84° 29' 33.44"E 26° 26' 24.22"N

VKS A 84° 29' 32.54"E 26° 26' 23.14"N

VKS B 84° 29' 33.56"E 26° 26' 25.33"N

VKS C 84° 29' 34.06"E 26° 26' 25.07"N

VKS D 84° 29' 33.3"E 26° 26' 22.94"N

144 UCHKAGAON PASAINI TMT 84° 20' 38.50"E 26°29'34.66"N

145 UCHKAGAON SIRSHA NBC 84° 40' 72.37"E 26°24'08.78"N

146 BAIKUNTHPUR GORAUH PNC 84° 45' 58.06"E 26°18'02.86"N

147 MANJHAR KOENI RAI 84° 30' 41.53"E 26°24'50.61"N

There are number of villages listed above, have the potential of producing kiln bricks in the non-

cultivated land, which can be made cultivable after using 1 or 2 metre of earth cutting for manufacturing

the kiln bricks. Apart from that, further study in near future can be made to identify such areas at

regular intervals.


43

3.3 LIST OF PROPOSED SAND GHATS (POTENTIAL AREA) IN THE DISTRICT : SL

NO DISTRICT

BLOCK OFFICE(BDO)

MOUZA BLOCK AREA IN

HECT NAME OF

RIVER SL.NO LATITUDE LONGITUDE

1 GOPALGANJ KUCHAIKOTE SAPAHIYA

KHAS BLOCK -

A 24.9 GANDAK

A

26°35'54.46"N

84°23'37.74"E

B

26°35'42.59"N

84°23'58.43"E

C

26°35'32.93"N

84°23'49.62"E

D

26°35'46.06"N

84°23'29.52"E

2 GOPALGANJ GOPALGANJ NIRANJANA BLOCK -

B 24.9 GANDAK

A 26°35'9.38"N

84°25'42.17"E

B 26°35'9.84"N

84°25'51.57"E

C

26°34'38.28"N

84°25'52.02"E

D

26°34'38.35"N

84°25'42.89"E

3 GOPALGANJ GOPALGANJ NIRANJANA BLOCK -

C 5 GANDAK

A

26°33'31.89"N

84°26'20.44"E

B

26°33'31.67"N

84°26'13.40"E

C

26°33'23.47"N

84°26'13.69"E

D

26°33'23.59"N

84°26'20.78"E

4 GOPALGANJ GOPALGANJ JAGIRI TOLA BLOCK -

D 24.9 GANDAK

A

26°30'57.28"N 84°28'2.73"E

B

26°30'46.05"N

84°28'23.50"E

C

26°30'35.71"N

84°28'16.20"E

D

26°30'48.47"N

84°27'55.04"E

5 GOPALGANJ GOPALGANJ JAGIRI TOLA BLOCK -

E 24.9 GANDAK

A

26°30'36.65"N

84°28'43.48"E

B

26°30'27.02"N 84°29'7.13"E

C

26°30'16.87"N 84°29'0.96"E

D

26°30'27.15"N

84°28'37.54"E

6 GOPALGANJ GOPALGANJ KHAP

MAKSHUPUR BLOCK -

F 24.9 GANDAK

A 26°30'8.06"N

84°29'29.00"E

B 26°30'3.48"N

84°29'46.86"E

C

26°30'18.23"N

84°29'52.00"E

D

26°30'22.64"N

84°29'33.08"E

7 GOPALGANJ GOPALGANJ MANJHARIYA BLOCK -

G 24.9 GANDAK

A

26°30'15.95"N

84°30'29.29"E

B 26°30'6.05"N 84°31'8.71"E

C

26°29'59.26"N 84°31'5.96"E

D 26°30'9.29"N

84°30'26.83"E

8 GOPALGANJ BAIKUNTHPUR SITALPUR BLOCK-

H 10 GANDAK

A 26°16'2.67"N 84°50'3.03"E

B 26°16'3.96"N 84°50'7.52"E


44

C

26°15'39.47"N

84°50'13.18"E

D

26°15'38.60"N 84°50'8.37"E

9 GOPALGANJ BAIKUNTHPUR MUNJA BLOCK-I 1.4 GANDAK

A

26°13'53.85"N

84°51'13.82"E

B

26°13'50.71"N

84°51'17.74"E

C

26°13'50.19"N

84°51'17.75"E

D

26°13'50.50"N

84°51'15.80"E

E

26°13'49.07"N

84°51'15.54"E

F

26°13'50.14"N

84°51'11.66"E

G

26°13'52.89"N

84°51'11.79"E

Few more potential areas awaiting statutory clearances

SL NO.

Name of River

Name of Ghat Area Pillar Cordinates

1 GANDAK Rajwahi Yadavpur

Ghat 3.5

1 26°33'47.69N 84°27'06.37"E *

2 26°33'43.89N 84°27'07.99"E

3 26°33'41.04N 84°27'03.28"E

4 26°33'45.89N 84°26'56.59"E *

2 GANDAK Batardeh Jokaha

Ghat 2.5

1 26°25'38.66N 84°36'12.79"E

2 26°25'35.39N 84°36'13.59"E

3 26°25'33.87N 84°36'03.95"E

4 26°25'35.96N 84°36'03.58"E

5 26°25'38.29N 84°36'09.79"E

3 GANDAK Rampurwa

Banjaria Ghat 1.4

1 26°24'19.89N 84°42'53.43"E

2 26°24'08.96N 84°42'57.73"E

3 26°24'08.73N 84°42'56.60"E

4 26°24'19.59N 84°42'51.78"E

4 GANDAK Dipu Dumaria Ghat 2.4

1 26°21'27.57N 84°44'57.15"E *

2 26°21'20.77N 84°45'03.62"E

3 26°21'19.42N 84°44'59.60"E

4 26°21'26.15N 84°44'55.09"E*

Note-

1. *The distance of 300m from bridge has been considered as per rule- 2 of “New sand policy’’

No.- CC-2/ MM (BA)/ 04/13/2214/ M, PATNA, DATED 27.08.13.

2. Some of the above mentioned sand blocks were found to be having low sand deposit during field

exploration. Such blocks may be considered for mineral concession depending upon the rate of

replenishment in subsequent years.


45

Google images as per KML data of Proposed Sand Ghats :


46


47


48


49

Site Photographs of Proposed Sand Ghats (Potential Areas)


50


51


52

4. Detail of Royalty or Revenue Received in last three years

Year wise Total Revenue Collection (in Rupees Lakhs)

S.N0 District 2014-15 2015-16 2016-17 2017-18 till Dec.17

1 Gopalganj 609.55 878.01 1060.9 432.77

5. Details of Production of Sand Or Bajri or Minor Mineral In Last

Three Years

Sl. No. Year Production

1 2015-16 NA

2 2016-17 NA

3 2017-18 NA


53

6.Process of Deposition of Sediments In The Rivers of The District

Replenishment of Sand :-

The deposition in a river bed is more pronounced during rainy season although the quantum of deposition varies from stream to stream depending upon numbers of factors such as catchment, lithology, discharge, river profile and geomorphology of the river course where annual deposition is one meters, but it is noticed that during flood season whole of the pit so excavated is completely filled up and as such the excavated area is replenished with new harvest of minerals.

In order to calculate the mineral deposits in the stream beds, the mineral constituents have been categorized as clay, silt, sand, bajri and boulder. However during present calculation, the waste material i.e silt which vary from 10 to 20% in different streams has also been included in the total production. Further the Survey of India Topo-Sheets are used as base map to know the extent of river course. The mineral reserves have been calculated only upto 1.00 meter depth although there are some portions in the river beds such as channel bars, point bars and central islands where the annual deposition is raising the level of river bed thus causing shifting of the rivers towards banks resulting in to cutting of banks and at such locations, removal of this material upto the bed level is essential to control the river flow in its central part to check the bank cutting. While calculating the mineral potentials, the mineral deposits lying in the sub- tributaries of that particular stream/river has not been taken into consideration. Since these mineral deposits are adding annually.

Surface runoff

Also known as overland flow is the flow of water that occurs when excess storm water, melt water, or other sources flows over the Earth's surface. This might occur because soil is saturated to full capacity, because rain arrives more quickly than soil can absorb it, or because impervious areas (roofs and pavement) send their runoff to surrounding soil that cannot absorb all of it. Surface runoff is a major component of the water cycle. It is the primary agent in soil erosion by water.

Runoff that occurs on the ground surface before reaching a channel is also called a nonpoint source. If a nonpoint source contains man-made contaminants, or natural forms of pollution (such as rotting leaves) the runoff is called nonpoint source pollution. A land area which produces runoff that drains to a common point is called a drainage basin. When runoff flows along the ground, it can pick up soil contaminants including petroleum, pesticides, or fertilizers that become discharge or nonpoint source pollution.

In addition to causing water erosion and pollution, surface runoff in urban areas is a primary cause of urban flooding which can result in property damage, damp and mold in basements, and street flooding.

https://en.wikipedia.org/wiki/Water

https://en.wikipedia.org/wiki/Meltwater

https://en.wikipedia.org/wiki/Meltwater

https://en.wikipedia.org/wiki/Earth#Surface

https://en.wikipedia.org/wiki/Soil

https://en.wikipedia.org/wiki/Surface_runoff#Saturation_excess_overland_flow

https://en.wikipedia.org/wiki/Surface_runoff#Infiltration_excess_overland_flow

https://en.wikipedia.org/wiki/Surface_runoff#Infiltration_excess_overland_flow

https://en.wiktionary.org/wiki/impervious#Adjective

https://en.wikipedia.org/wiki/Roof

https://en.wikipedia.org/wiki/Road_surface

https://en.wikipedia.org/wiki/Water_cycle

https://en.wikipedia.org/wiki/Soil_erosion#Rainfall_and_runoff

https://en.wikipedia.org/wiki/Channel_(geography)

https://en.wikipedia.org/wiki/Nonpoint_source_pollution



https://en.wikipedia.org/wiki/Drainage_basin

https://en.wikipedia.org/wiki/Soil_contamination

https://en.wikipedia.org/wiki/Petroleum

https://en.wikipedia.org/wiki/Pesticide

https://en.wikipedia.org/wiki/Fertilizer

https://en.wikipedia.org/wiki/Discharge_(hydrology)

https://en.wikipedia.org/wiki/Urban_runoff

https://en.wikipedia.org/wiki/Flood#Urban_flooding

https://en.wikipedia.org/wiki/Basements


54

Effects of surface runoff

Erosion and deposition

Surface runoff can cause erosion of the Earth's surface; eroded material may be deposited a considerable distance away.

There are four main types of soil erosion by water:

splash erosion,

sheet erosion,

rill erosion,

gully erosion.

Splash erosion is the result of mechanical collision of raindrops with the soil surface: soil particles which are dislodged by the impact then move with the surface runoff.

Sheet erosion is the overland transport of sediment by runoff without a well-defined channel.

Soil surface roughness causes may cause runoff to become concentrated into narrower flow paths: as these incise, the small but well-defined channels which are formed are known as rills. These channels can be as small as one centimeter wide or as large as several meters.

If runoff continue to incise and enlarge rills, they may eventually grow to become gullies.

Gully erosion can transport large amounts of eroded material in a small time period.

https://en.wikipedia.org/wiki/Erosion

https://en.wikipedia.org/wiki/Sediment

https://en.wikipedia.org/wiki/Deposition_(geology)

https://en.wikipedia.org/wiki/Erosion#Rainfall_and_runoff

https://en.wikipedia.org/wiki/Rill

https://en.wikipedia.org/wiki/Gully

https://en.wikipedia.org/wiki/Sediment

https://en.wikipedia.org/wiki/Rill

https://en.wikipedia.org/wiki/Gully


55

Reduced crop productivity usually results from erosion, and these effects are studied in the field of soil conservation. The soil particles carried in runoff vary in size from about .001 millimeter to 1.0 millimeter in diameter. Larger particles settle over short transport distances, whereas small particles can be carried over long distances suspended in the water column.

There are many sediment transport equations which are suitable for use in the prediction of the replenishment rate of rivers/ watershed. Some of the Famous sediment transport equations are: ‐

1. Dandy – Bolton Equation 2. Yang Equations 3. Engelund‐Hansen Equation

4.Modified Universal Soil Loss Equation (MUSLE)

DANDY ‐ BOLTON EQUATION Dandy Bolton formula is often used to calculate the sedimentation yield. But use of these equations to predict sediment yield for a specific location would be unwise because of the wide variability caused by local factors not considered in the equations development. However, they may provide a quick, rough approximation of mean sediment yields on a regional basis for preliminary watershed planning. Computed sediment yields normally would be low for highly erosive areas and high for well stabilized drainage basins with high plant density because the equations are derived from average values. The equations express the general relationships

Soil erosion by water on intensively-tilled farmland.

.

https://en.wikipedia.org/wiki/Soil_conservation

https://en.wikipedia.org/wiki/Precipitate

https://en.wikipedia.org/wiki/Water_column

https://en.wikipedia.org/wiki/Water_column

https://en.wikipedia.org/wiki/Erosion#Rainfall_and_runoff

https://en.wikipedia.org/wiki/File:Wassererosion_Acker.jpg


56

between sediment yield, runoff, and drainage area. Many variables influence sediment yield from a drainage basin. They include climate, drainage area, soils, geology, topography, vegetation and land use. The effect of any of these variables may vary greatly from one geographic location to another, and the relative importance of controlling factors often varies within a given land resource area. Studies revealed that sediment yield per unit area generally decreases as drainage area increases. As drainage area increases, average land slopes usually decrease; and there is less probability of an intense rainstorm over the entire basin. Both phenomena tend to decrease sediment yield per unit area. In arid regions, sparse precipitation and low run‐off are the limiting factors. As precipitation increases, density of vegetation also increases, resulting in less erosion. In areas with adequate and evenly distributed precipitation, vegetation thus becomes the limiting factor. The accuracy of the sedimentation surveys varied, ranging from reconnaissance type measurements of sediment deposits to detailed surveys consisting of closely spaced cross‐sections or contours. Runoff data are translated to inches per year per unit area and sediment deposition data to tons per year per square mile of net drainage area. Net drainage area is defined as the sediment‐contributing area and normally excluded areas above upstream reservoirs or other structures that were effective sediment traps. Actual sediment yields undoubtedly were slightly higher because most reservoirs do not trap inflowing sediment. Sediment Yield vs. Drainage Area: ‐ On the average, sediment yield is inversely proportional to the 0.16 power of drainage area between 1 and 30,000 square miles. Sediment Yield vs. Runoff: ‐ Sediment yield increased sharply to about 1,860 tons per square mile per year as run‐off increased from 0 to about 2 inches. As runoff increased from 2 to about 50 inches, sediment yield decreased exponentially. Because sediment yield must approach zero as runoff approaches zero, a curve through the plotted points must begin at the origin. The abrupt change in slope of a curve through the data points at Q equals 2 inches

Precluded the development of a continuous function that would adequately define this relationship. Thus, there are two equations derived for when Q was less than 2 inches and when Q was greater than 2 inches.

Combined Effect of Drainage area and Surface Run off on Sediment Yield

Dandy‐ Bolton determined the combined influence of runoff and drainage area on sediment yield to compute the sediment yield. They developed two equations i.e. for run off less than 2 inch and for run off more than 2 inch, which are given below:‐ Where: S = Sediment yield (tons/sq miles/yr) Q = Mean Annual runoff (inch) A = Net drainage are in sq mile

For run off less than 2 inch. (Q<2in) S=1289*(Q) 0.46*[1.43-0.26 Log (A)] F

For run off more than 2 inches.


57

(Q > 2 in): S= 1958*(e ‐0.055*Q)*[1.43‐0.26 Log (A)]

s.NO Factors Probable Replenishment

1 River Parwati

2 Catchment Area 5001 km2

3 Average Annual Runoff 800 mm

4 *sediment yield formula

For Q < 2 in: S=1280*(Q) 0.46 *[1.43‐0.26 Log(A)] For Q

> 2 in: here: Q = Mean Annual runoff (inch)=

800 mm A = Catchment Area= 2892 km2

Sediment yield S= (tonnes/yr)

S= 1958*(e ‐0.055*Q )*[1.43‐0.26 Log (A)] *Source:‐ Calculation of sediment yield by the

Dandy‐ Bolton formula.

70.11 M. tons/km2 /yr Or

350631.57 M. tons/year

The area 5001 Km2 is representing the catchment area of the Parwati,. Thus, about

350631.57 M tons/year sediment will be regenerated every year in the catchment

area as replenishment against the mined out quantities. The maximum annual

production is 1.656120 million TPA. The amount of sediment regenerated every

year derived hypothetically by Dandy‐Bolton’s equation will be around

350631.57 M. tons/year for the proposed lease area. Therefore, the percentage of

replenishment is around 21 % every year .The hypothetical derivation of

replenishment data is not supported by any ground evidence as the same can be

derived only after annual study due to inconsistent rains in Rajasthan. The derived

replenishment data is based on macro‐watershed data taken from satellite

imagery with sample ground truth and annual average rainfall. The data derived is

based on SRTM 30m resolution processed using ARCGIS software with linear and

resolution factors affecting the derivation.

UNIVERSAL SOIL LOSS EQUATION

Sediment loss from water erosion Modeling sediment loss

MUSLE is a modification of the Universal Soil Loss Equation (USLE). USLE is an


58

p

estimate of sheet and rill soil movement down a uniform slope using rainfall energy as the erosive force acting on the soil (Wischmeier and Smith 1978). Depending on soil characteristics (texture, structure, organic matter, and permeability), some soils erode easily while others are inherently more resistant to the erosive action of rainfall. MUSLE is similar to USLE except for the energy component. USLE depends strictly upon rainfall as the source of erosive energy. MUSLE uses storm-based runoff volumes and runoff peak flows to simulate erosion and sediment yield (Williams 1995). The use of runoff variables rather than rainfall erosivity as the driving force enables MUSLE to estimate sediment yields for individual storm events. The water erosion model uses an equation of the form:

Y X EK CVF PE SL ROKF

where: Y = sediment yield in tons per hectare EK = soil erodibility factor CVF = crop management factor that captures the relative effectiveness of soil and

crop management systems in preventing soil loss PE = erosion control practice factor (including management practices such as

terraces, contour farming, and strip cropping) SL = slope length and steepness factor ROKF = coarse fragment factor For estimating MUSLE, the energy factor, X, is represented by

X 1.586Qq 0.56

WSA0.12

where: Q = runoff volume in millimeters qp = peak runoff rate in millimeters per hour WSA = watershed area in hectares

Runoff volume is estimated using the SCS curve number method. Peak flow was estimated using a modification of the rational method which relates rainfall to peak flow on a proportional basis. The rational equation is:

q C i A

where: q = peak flow rate C = runoff coefficient representing watershed characteristics i = rainfall intensity for the watershed’s time of concentration A = watershed area


59

7. GENERAL PROFILE OF THE DISTRICT

7.1 River System

Gopalganj district is situated in the northwest part of the state. It lies between N-latitude

26012’ & 26039’ and E longitude between 83054’ & 84055’. It covers parts of Survey of India

toposheet Nos. 72 A/2, B/3, O/6, B/7, B/10, B/11 & B/25. This district comes under Indo-

Gangetic plain covering plain and Gandak-Ghaghra sub-basin. There are 14 development blocks

with two sub-basins. It is bounded by Uttar Pradesh on the north and west whereas by Gandak

river in the east and by Siwan district on south.



60

The district is mainly drained by Gandak river that has taken the present course, which forms the eastern and north eastern boundary of the district. The Gandak river flows in a south easterly direction with an average gradient of 0.28 m/km. The river brings a lot of silt, which is deposited in the river bed resulting in oscillation of course.

Apart from this main rivers there are numerous ephemeral streams flowing in the district namely Jharbi, Dahe, Khanua, Ghoghli, Kedanjot, Sona etc. They all emerge near Gandak embankment which are locally known as Chaurs and Tal. In course of time these beds get silted and their course start shifting. During the process of shifting of course there streams leave behind abandoned channels and a number of marques locally known as Chaus. These Chaus are also responsible for water logging in the area by spreading their span with the onset of monsoon and become localize during summer. Most of the ephemeral streams have their flow direction in north south.

7.2 Climate Gopalganj has a varied climate. It is exceptionally hot and dry during summer with

temperature reaching as high as 45 degrees Celsius. Gopalganj receives about 1218 mm

rainfall during monsoons, which is followed by pleasant temperature in winter. District

receives an average rainfall of about 1218 mm and the temperature varies from 10 to 45

degree Celsius. Total physical area can roughly be put in two categories i.e. Normal Area and

Lowly Area (flood affected area). Parts of the six blocks like Gopalganj, Kuchaykot, Manjha,

Sidhwalia, Barauli and Baikunthpur are flood affected areas. These areas remain under

water in the rainy season. But so far as cultivation and agriculture is concern these areas are


61

called the stock of food grains. Rest of the parts is normal area with full greenery and

cultivable land. In the area monsoon sets in somewhere in June and lasts upto September.

The average annual rainfall in Gopalganj district is about 1218 mm. Most of the rainfall

receives from South West monsoon. Data reveals that there is a large variation in the ranfall

over year to year. The behaviour of isohyte is given in Plate.

7.3 Geomorphology

Flat alluvial formations of considerable thickness is very common in the entire district. The entire flat terrain has been divided into two main categories.

a) Alluvial Low Tracts: - They are most commonly found in the immediate vicinity of river Gandak which is subjected to periodical submergence by flood water.

b) Diara Land: - They are nothing but heap and sands, brought by rivers during flood and usually found in the bed of the river Gandak. There is a gradual slope from the north western to south eastern direction. The general slope varies between 70.69 mt MSL to 57.09 mabMSL. In general the surface gradient in about 0-11 m/km in the area.


62



63

7.4 Soil Characteristics


As per the U.S. Survey Staff (1975) the soil of the area is broadly divided into three groups

based upon the diffluent conditions of pedogeny, climate and texture.

a) Entisols – These are younger alluvial soil, fringes near the bank of Gandak and the eastern

bank of Ghaghra in the western part of the district. The entisols are generally a light, friable,

loam with higher proportion of sand and silt. The maximum percent of clay is found to be

upto 35%. They are often associated with calcareous nodules. The higher content of sand


64

keeps the soil, except in the river bed, fairly drained and makes it suitable for autumn and

rabi crops which do not need much water. These soils are most suitable for cultivation of

high yielding crops like sugar cane and wheat.

b) Inceptisols - There are locally known as Bangar and there calcareous alluvial soils occur

mostly in the central part of the district. This forms the typical paddy land of Bihar. The clay

and silt % ranges between 30-45%.

c) Alfisols – These soils occur in patches around eastern part of the district. These are farely

matured soils subject to continuous leaching operation, leading to formation of calcareous

nodules and ferruginous clay pans. Texturally there are well-drained reddish yellow silty

sandy and clayey loams.

7.5 Irrigation:-

IRRIGATION BY DIFFERENT SOURCES

The rapid growth of population demands for greater production in bringing more and more land

under cultivation. The socio-cultural and economic political factors play significant role over land

use in soft rural and urban area in the district. The blockwise details of land utilization reveals that

74% of the total area in net shown. (Areas and Number of Structures)

IRRIGATION BY DIFFERENT SOURCES (Areas sq.km

and number of structures)

Area No.

Dugwell - 4580

Tubewell/Borewell 644.10 21299

Tank/ponds Nil -

Canals 319.72 -

Other sources 1.89 72

Net irrigated area 970.71

Gross irrigated area 1094.35

7.6 Demography Population Persons Males Females

Total 2562012 1267666 1294346

In the age group 0-6 years 449530 230014 219516

Scheduled Castes (SC) 320064 159265 160799

Scheduled Tribes (ST) 60807 29833 30974

Literates 1382998 793905 589093

Illiterate 1179014 473761 705253

Total Worker 728201 539586 188615

Main Worker 363111 300336 62775

Main Worker - Cultivator 138969 120197 18772

Main Worker - Agricultural Labourers 108576 84113 24463

Main Worker - Household Industries 12455 9186 3269

Main Worker - Other 103111 86840 16271

Marginal Worker 365090 239250 125840

Marginal Worker - Cultivator 69990 46553 23437


65

Out of the total Gopalganj population for 2011 census, 6.07% lives in urban regions of district.

In total 155273 people live in urban areas, whereas, 93.93 % population, i.e. 2402764, of the

districts live in rural areas of villages. Agriculture is the main livelihood of most of the

population dependant on the vagaries of monsoon and a good network of canal system within

canal of Gandak.

7.7 Forest

The forest cover in the state, based on interpretation of satellite data of Nov 2008- Jan

2009, is 6,845 km2 which is 7.27% of the state's geographical area. In terms of forest canopy

density classes, the state has 231 km2 very dense forest, 3,280 km2 moderately dense forest,

and 3,334 km2 open forest.

Marginal Worker - Agriculture Labourers

230090 145901 84189

Marginal Worker - Household Industries

13594 8517 5077

Marginal Workers - Other 51416 38279 13137

Marginal Worker (3-6 Months) 284214 192706 91508

Marginal Worker - Cultivator (3-6 Months)

52665 36153 16512

Marginal Worker - Agriculture Labourers (3-6 Months)

178588 117620 60968

Marginal Worker - Household Industries (3-6 Months)

10101 6532 3569

Marginal Worker - Other (3-6 Months) 42860 32401 10459

Marginal Worker (0-3 Months) 80876 46544 34332

Marginal Worker - Cultivator (0-3 Months)

17325 10400 6925

Marginal Worker - Agriculture Labourers (0-3 Months)

51502 28281 23221

Marginal Worker - Household Industries (0-3 Months)

3493 1985 1508

Marginal Worker - Other Workers (0-3 Months)

8556 5878 2678

Non Worker 1833811 728080 1105731

Sex ratio (females/1000

males)

1,015

Literacy Rate Total 53.98%

Males 62.62%

Females 45.51%


66

District-wise Forest Cover Area in BIHAR (Area in Km2) 2011 Assessment

District Geograph ical Area Km2

Very Dense Forest

Moder-ate.

Dense Forest

Open Forest

Total Percent of GA

Change Scrub

Araria 2,830 0 12 76 88 3.11 2 0

Aurangabad 3,305 0 54 97 151 4.57 0 13

Banka 3,022 0 111 110 221 7.31 0 12

Begusaral 1,918 0 20 23 43 2.24 0 0

Bhabhua 3,381 0 555 507 1,062 31.41 0 20

Bhagalpur 2,567 0 29 13 42 1.64 0 0

Bhojpur 2,390 0 16 3 19 0.79 0 0

Buxar 1,708 0 2 1 3 0.18 0 0

Darbhanga 2,279 0 41 144 185 8.12 0 0

Gaya 4,976 0 124 506 630 12.66 0 46

Gopalganj 2,033 0 2 2 4 0.20 0 0

Jamui 3,107 0 383 249 632 20.34 0 2

Jehanabad 1,569 0 2 1 3 0.19 0 5

Katihar 3,057 0 18 44 62 2.03 0 0

Khagaria 1,486 0 2 6 8 0.54 0 0

Kishanganj 1,884 0 26 49 75 3.98 0 0

Lakhisarai 1,356 0 180 14 194 14.31 0 2

Madhepura 1,788 0 6 20 26 1.45 0 0

Madhubani 3,501 0 18 118 136 3.88 0 0

Munger 1,347 0 251 14 265 19.67 0 7

Muzaffarpur 3,172 0 102 75 177 5.58 21 0

Nalanda 2,367 0 5 23 28 1.18 0 6

Nawada 2,494 0 187 323 510 20.45 0 10

Pashchimi Champ1uan

5,228 231 524 166 921 17.62 8 0

(Source: India state of forest report 2011-Bihar)


67

Flora of the area:-

Gopalganj falls under greenbelt areas. Roughly all types of trees and plants are found in the district namely Babbul, Neem, Shisham, Mango, Sagwan, Katahal, Sal, Shakhuwa, Peepal, Bargad etc.

Unfortunately the people of Gopalganj due to lake of awareness are cutting trees without carrying for its bad impacts. Awareness about the ecological balance must be spread amount the general people specially the children.

Fauna of the area:- Animals widely found in the district are Cows, Buffaloes, Horses, Sheep, Goats and Pigs. These animals play an important role in the life of farmers. Some small wild animals like Nil Gay, Rabbits, Sahil, Jackals, Fox and Peacock are in the area within the district. Some times Deers, Elephants and Leopards and also seen within the district.


68

7.8 Hydrogeology

(Source: Geological Survey of India) The district forms a part of the vast alluvial terrain of Gandak and Ghaghra sub-basins forming a part of Indo-Gangetic alluvium consisting of a thick pile of unconsolidated quaternary sediments. They are recent to sub-recent deposits underlain by erosional basement of Vindhyan formation of pre-cambrian age. The thickness of alluvium is still not yet confirmed through boreholes. These quaternary sediments consist of sequences of finer clastics like clay and silts with various grades of sand and gravel associated with Kankar. The lithological characteristics are mainly governed by the depositional environments namely distance from the provenance, agencies of deposition and the medium of transport. Marked lateral and vertical variations is texture and composition of sediments support these propositions. The Gangetic alluvial deposits can be sub-divided into two types viz. newer alluvium and older alluvium. The older alluvium of Pleistocence age in the area is rather dark in colour, occupies


69

the higher ground and generally rich in kankar which are concretion of nodules of impure calcium carbonate ranging in size from small grains to loose lumps whereas the newer alluvium of recent age occupying the lower grounds constitute a thick sequence of clay, silt and sand with occasional kankar. Depth to water level in pre-monsoon 2011 and post-monsoon 2011 is ranges between 2.72 to 6.32 and 1.41 to 3.63 m bgl, respectively.

Pre-monsoon depth to water level for Gopalganj district of Bihar (Year 2011).

Post-monsoon depth to water level map for Gopalganj district (year 2011).


70

Block wise Dynamic Ground Water Resource of Gopalganj District (2008-09)

Assessment of Dynamic Ground Water Resources of the Bihar state Gopalganj district(as on 31st March 2009)

( in hectare meter)

Sl.

No

.

Assessment

Unit/District

Net Annual

Ground

water

Availability

Existing

Gross

Ground

Water

Draft for

Irrigatio

n

Existing

Gross

Ground

water Draft

for

Domestic

and

Industrial

Water

Supply

Existing

Gross

Ground

Water

Draft For

all Uses

(10+11)

Allocation

for

Domestic

and

Industrial

Requireme

nt supply

upto year

2025

Net

Ground

Water

Availabilit

y for

future

irrigation

developm

ent (9-10-

13)

Stage of

Ground

Water

Developm

ent

(12/9)*100

(%)

1 2 9 10 11 12 13 14 15

1 Baikunthpur 5456 2791 309 3100 475 2190 56.8

2 Barauli 4789 2393 532 2925 601 1795 61.1

3 Bijaipur 4266 3067 202 3268 310 889 76.6

4 Bhore 4841 3348 259 3608 399 1094 74.5

5 Gopalganj 5379 1688 330 2018 533 3158 37.5

6 Hathua 4493 2936 328 3264 504 1053 72.6

7 Kateyan 4075 1902 281 2183 459 1714 53.6

8 Kuchaikot 8504 3960 484 4444 744 3800 52.3

9 Manjha 4188 2295 300 2595 461 1432 62.0

10 Phulwaria 3077 1626 191 1817 294 1157 59.0

11 Panchdeori 2784 1429 146 1575 224 1131 56.6

12 Sidhwalia 2785 996 199 1195 305 1484 42.9

13 Thawe 1699 959 169 1127 259 481 66.3

14 Uchkagaon 4020 2501 372 2873 425 1094 71.5

Total 60356 31889 4102 35992 5993 22474 59.63

Block-wise groundwater resources and stage of groundwater development in Gopalganj district, Bihar

Blockwise stage of ground water development


71

8. Land Utilization Pattern In The District

Agriculture is the main occupation of the people of the district. The soil of the district is highly calcareous. Among the different kinds of the soil, one can find here sandy, loamy, hard clayey and Usar soil. Paddy is the most important of the crops in the district. One - fifth of it is Bhadai rice, harvested in the autumn and the remaining four fifths is Aghani or winter rice. Other important crops grown in the district are wheat, sugar-cane and maize besides potato, pulses and oil-seeds. Sugar-cane and tobacco are the cash crops grown in the district. The soil in the district is alluvial and varies from the hard clay found in the low swamps, which is locally known as bangar to the light sandy loam of the uplands called bhath. The former grows winter rice only while from the latter an autumn rice crop is generally obtained followed by a spring crop of cereals, pulses and oil-seeds. In the district as a whole these two soils are found in fairly regular proportions. All types of food grains and crops are found in this region as Wheat, Paddy, Grams, Arahar, Maize, Sarso, Tishi, Potato, Sugar Cane etc. But Wheat, Paddy and Maize are the main crop of the district. The district is also known for production of Green Vegetables, Fish, Sugar Cane, Milk and Milk products.

Land utilization

i) Total Area 2009-10 hectare 115000

ii) Forest cover -do- “ -

iii) Non Agriculture Land -do- “ 35400

v) cultivable Barren land -do- “ 25487


72

9. Physiography of The District

The Bihar state can be broadly subdivided into three major units i.e main physical subdivisions are the Northern Mountains, the Gangetic Plains and the Central Highlands. Northern Mountains comprises the Himalayan ranges including their foot hills. The Gangetic plains, situated between the Himalayas and the Deccan plateau, constitute the most fertile plains of the sub-basin ideally suited for intensive cultivation. The Central highlands lying to the south of the Great plains consists of mountains, hills and plateaus intersected by valleys and river plains. They are largely covered by forests. Aravali uplands, Bundelkhand upland, Malwa plateau, Vindhyan ranges and Narmada valley lie in this region. Predominant soil types found in the sub-basin are sandy, loamy, clay and their combinations such as sandy loam, loam, silty clay loam and loamy sand soils. There are no hills in Gopalganj. Though the district presents the appearance of a

level plain, the uniformity is broken here and there by the depressions and marshes dotted

over the countryside. The district contains no forest as well. The Gandak supported by

tributaries like Jharahi, Khanwa, Daha, Dhanahi etc. give a big status of river . Land of the

district is fertile and alluvial because of this river the district is good in cultivation and

irrigation. River Gandak by depositing the top quality of soil bringing from the Nepal is

playing an important role in the economy of the district.


73

10. Rainfall: Month wise

Gopalganj District 5 Year’s

Average Rainfall in mm

Year 2012 2013 2014 2015 2016

Sl. No. Month Avg Avg Avg Avg Avg

1 Jan 12.30 0.00 0.00 5.50 0.00 3.56

2 Feb 0.00 42.20 21.00 0.00 0.00 12.64

3 Mar 0.00 0.00 9.70 38.00 0.00 9.54

4 Apr 6.50 5.00 0.00 46.70 0.00 11.64

5 May 0.00 43.20 16.60 24.70 113.00 39.5

6 Jun 93.00 232.50 77.60 74.00 99.50 115.32

7 Jul 297.10 84.80 121.80 242.70 257.10 200.7

8 Aug 244.00 172.40 281.50 278.40 48.50 204.96

9 Sep 299.90 68.20 110.30 77.00 327.90 176.66

10 Oct 0.00 230.30 83.00 34.70 19.00 71.4

11 Nov 0.00 0.00 0.00 0.00 0.00 0.00

12 Dec 0.00 0.00 5.30 0.00 0.00 1.06

The Indian Meteorological Department, Nagpur, vide letter No. NAGPUR RMC/CS-312, dated 18th January, 2016 has provided the period of Rainy Season viz. Normal dates of Onset and Withdrawal of South West Monsoon over India as state-wise. The duration for the period is 10th June to 15th October.


74

11. GEOLOGY AND THE MINERAL WEALTH OF THE AREA

The area forms parts of the North- Western track of Gandak Basin. Correlation among

different litho units have been established on the basis of a number of natural and

excavated sections in the area. The morpho/litho units of the area occur in the following

chronological order.

Diara formation/Surface

Vaishali formation/Surface

Hajipur formation/Surface

Miraganj formaton/Surface

The above sequence also represents the order of superposition of the litho-units. The

different morpho-statigraphic units been designated as surface. Lithologically Mirganj

formation is the oldest and consists yellowish brown clayey silty sand. This formation is

micaceous and clayey silt and sand contains are almost equal proportion upto a depth of

2.5m to 3.0m. The Mirganj formation outcrops mostly in relatively higher patches of land.

Mirganj formation provides good raw material for the manufacture of bricks due to

presence of suitable quantity of clay. Hajipur formation comprises yellowish brown to

greyish brown compact clay with dissemination of calc. kankars. The Vaishali formation

comprises dirty white to light grey silt and silty clay and lies unconformably on eroded

surfaces of Hajipur formation. Diara formation consists of light grey fine clayey silt, silty sand

and sand. Yhe Diasa formation occurs mainly between the high banks of the main rivers of

the area.

Mirganj formation and Hajipur formation provide good source for bricks industry

due to clayey sand.


75



76



77

12. ADDITIONAL INFORMATION

12.1 Drainage system with description of main rivers

Drainage system with description of main river

Sl.no Name of the River

Cross Section area of catchment (square

km) (Cosidering 500 m Both Side from bank of the river)

District of Gopalganj area in (square km)

% Area Drained in the District

1 Gandak 50 2,033 2.46

12.2 Salient features of Important Rivers and Streams

Salient Features of Important River and Streams

S.no Name of the River

Stream Total Length in the

District (in km) place of Origin Altitude at Origin

1 Gandak 29 Mudi 3617

12.3 Mineral Potential and Annual Deposition

Name of the River

Portion of the River

Strem Recommended for Mineral

Concession ( in km )

Length of are

recommended for mineral

concession (in km)

Length of are

recommended for mineral

concession (in

meter)

Average width of

are recommen

ded for mineral

concesion (in

meters)

Depth in

meter (as per statue

)

Area recommen

ded for mineral

concesion (in square

meters)

Volume recommende

d for mineral concesion (in cum)

Mineable Mineral

Potential (in metric

tonne)60% of tatal mineral

potential

Gandak 23 5.161 5161 320 0.5 1651520 825760 936411.84

Note: Density of sand = 1.89 Ton/cum.

Current Mineral Potential (2018 pre monsoon period)

Name of the River Boulder (MT) Bajari (MT) Total resuorcess in

mt recommended for mineral consesion

total Mineable Mineral Potential

at 60% (MT)

Gandak Nil Nil 1560686.4 936411.84

Average annual depotion observed (2018 post monsoon period)

Gandak Nil Nil 1560686.4 936411.84


78

13. DISASTER RISK MANAGEMENT

The Basis

The fundamentals of existence lie in the struggle one has fought, the instruments one has used and the lessons one has learnt to survive. In this respect, Bihar‘s struggle for existence is far more grim than most of the states. It has undergone mitosis for as many as four times and has suffered through disasters of the worst kind many a time.

The Vision :

Right from the days following the battle of Buxar in 1764 after which Bihar was passed

on to East India Company as a part of the Bengal Presidency, to 1912 when Bihar and

Orissa were separated as one State, to 1936 when both Bihar and Orissa were made

independent States, to 1956 when some key areas of Bihar was included in West

Bengal, to 2000 when Bihar was divided to form the state of Jharkhand, the State has

went on losing its natural resource base and got pushed to confine within an area

prone to all sort of hazard: earthquake, flood, cyclonic storm/Gale /Hail Storm,

drought, fire, extreme cold and heat waves etc.

For such a state of hazards which Bihar is, the VISION of Disaster Management is :

“To attain a position where people are ready to help themselves, local

bodies to extend mutual help, the administration to organize public help and

the government to facilitate the helping of helpers.”

The Objectives:

In order to achieve the Mission, the objectives of the plan have been set as :

i. Treating community as the primary stakeholder and first respondent in the Disaster Management Plan, focusing on disaster risk reduction, prevention, mitigation and preparedness measures.

ii. Emphasizing preparedness at the community level and readiness at the local bodies level

iii. Facilitating the role play by the administration and government departments and other stakeholders through institutional mechanism.

iv. Creation of specialized institutions to make disaster management an inclusive exercise and to wed it to development initiatives.

v. To create a dependable early warning system to warn the people and activate other stakeholders.


79

vi. Ensuring quick response and providing relief with care and attention to those belonging to the marginalized section.

vii. To undertake rehabilitation with "Build Back Better" motif.

The Approach :

The process adopted for the formulation of the Plan has been

i. Holistic: Covering all the hazards the state is vulnerable to.

ii. Integrative: Covering prevention, mitigation, preparedness & response measures.

iii. Participative: Including the affected people, the Panchayati Raj Institutions,the district administration, the government departments & expert institutions.

iv. Associative: Creating space for the support and help from the corporate bodies, civil societies, NGOs, CBOs and others and solicit their participation in disaster management.


80

EQ Zone V- 10.9%

Wind Velocity m/s 55 & 50 - 5%

Flood Prone Area in % - 7.9%

IV- 17.3% 47- 40.2%

III- 30.4% 44&39- 48%

II- 41.4% 33- 6.7%


81

FLOOD PRONE AREA IN BIHAR:

Source: Developed on Inputs from DMD, GoB

2. Flood— Most Vulnerable : East Champaran, Sheohar, Sitamarhi, Katihar,

Madhubani, Vaishali, Muzaffarpur, Darbhanga,

Samastipur, Madhepra, Supaul, Saharsa,

Khagaria, Begusarai, Bhagalpur.

Vulnerable : West Champaran, Gopalganj, Siwan, Saran,

Buxar, Bhojpur, Patna, Nalanda, Lakhisarai,

Sheikhpura, Purnia, Araria, Kishanganj


82

DROUGHT PRONE AREAS

Source: Developed on Inputs from DMD, GoB

3. Drought — Vulnerable District : Gaya, Nawada Jamui, Nalanda, Lakhisarai

Prone District : Jehanabad, Arwal, Aurangabad

Likely District : Kaimur, Bhojpur, Buxar, Rohtas, Banka


83

Conclusion 6 (six) sand ghats of approx area around 24 hectare, one sand ghat of 10, one six sand ghat less than

5 Ha. each in Gandak river has been identified with mineable mineral potential of around 936411.84

MT, where sand mining can be done with consultation of government authorities before opting for

E.C. or any other statutory clearences. The KML images of the geo references file of all those ghats is

attached for ready reference.

Since it is an interim report, it is proposed to identify such potential areas at certain interval and get

the data bank of DSR to be updated.

References

District Mining Office – Gopalganj

Geology of Bihar and Jharkhand by T. M. Mahadevan

National Institute of Disaster Management Report

Report of Central Ground Water Board, Ministry of Water Resources- State Unit

Office, Patna, September 2013

http://mines.bih.nic.in/

http://gopalganj.bih.nic.in/

https://en.wikipedia.org/wiki/Gopalganj_district

Geology & Mineral Resources Of The States Of India – Geological Survey Of India,

Part V – Bihar And Jharkhand

http://mines.bih.nic.in/

http://gopalganj.bih.nic.in/

https://en.wikipedia.org/wiki/Gopalganj_district

Date post:	29-Oct-2019
Category:	Documents
Upload:	others
View:	2 times
Download:	1 times

GOVERNMENT OF BIHAR DISTRICT GOPALGANJmines.bih.nic.in/DSR/MM/DSR-MM-Gopalganj.pdf · Gandak....

Documents