DISTRICT SURVEY REPORT OF LAKHISARAI Sand Mineral &...

8/17/2018

DISTRICT SURVEY REPORT OF LAKHISARAI Sand Mineral & Brick Kilns

As per Notification No. S.O. 3611 (E) New Delhi, the 25th July, 2018 of Ministry of Environment Forest and Climate change, Government of India

Prepared by

INSTITUTE OF ENVIRONMENT & ECO- DEVELOPMENT, PATNA

Ground Floor, Shyam Nagar Colony, Maurya Path, Khajpura P.O. B.V. College, Patna-800014, Bihar, India E-mail- [email protected] Website-

www.ieedindia.in Tel.: 0612-2590373, Telefax- 0612-2590373 M- +91-9472919161, 7004620817

Submitted to

Under Secretary Mines& Geology Department, Government of Bihar

District Survey Report - Lakhisarai Page 1

PREFACE

The Ministry of Environment, Forests & Climate Change (MoEF&CC), Government of India, made

Environmental Clearance (EC) for mining of minerals mandatory through its Notification of 27th

January, 1994 under the provisions of Environment Protection Act, 1986. Keeping in view the

experience gained in environmental clearance process over a period of one decade, the MoEF&CC

came out with Environmental Impact Notification, SO 1533 (E), dated 14th September 2006. Now

again Ministry of Environment, Forests & Climate Change (MoEF&CC), Government of India

amended the notification S.O. 141(E) Dated 15th January, 2016 vide S.O. 3611(E) Dated 25th July,

2018. It has been made mandatory to obtain environmental clearance for different kinds of

development projects as listed in Appendix-X of the Notification.

Further, in pursuance to the order of Hon’ble Supreme Court dated the 27th February, 2012 in I.A.

No.12- 13 of 2011 in Special Leave Petition (C) No.19628-19629 of 2009, 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 January, 2015 in the matter regarding sand

mining has directed for making a policy on environmental clearance for mining leases in cluster for

minor Minerals, The Ministry of Environment, Forest and Climate Change in consultation with State

governments has prepared Guidelines on Sustainable Sand Mining detailing the provisions on

environmental clearance for cluster, creation of District Environment Impact Assessment Authority

and proper monitoring of minor mineral mining using information technology and information

technology enabled services to track the mined out material from source to destination.

The DEIAA and DEAC will scrutinize and recommend the prior environmental clearance of mining

of minor minerals on the basis of District Survey Report. This will a model and guiding document

which is a compendium of available mineral resources, geographical set up, environmental and

ecological set up of the district and replenishment of minerals and is based on data of various

departments, published reports, journals and websites. The District Survey Report will form the basis

for application for environmental clearance, preparation of reports and appraisal of projects. The

Report will be updated once every five years.


OBJECTIVES

The main objective of the preparation of District Survey Report (as per the Sustainable Sand Mining

Guideline, 2016) is to ensure the following–

Identification of areas of aggradations or deposition where mining can be allowed;

Identification of areas of erosion and proximity to infrastructural structures and

installations where mining should be prohibited and calculation of annual rate of

replenishment and allowing time for replenishment after mining in that area.

Identification of mineral wealth in the district.


Index

Sl.No. Chapters Page No.

Chapter-1 Introduction 04

Chapter-2 Overview of Mining Activity in the District 11

Chapter-3 The List of Mining Leases in the District with location, area and

period of validity

19

Chapter-4 Details of Royalty or Revenue received in last three years 20

Chapter-5 Detail of Production of Sand or minor mineral in last three years 21

Chapter-6 Process of Deposition of Sediments in the rivers of the District 21

Chapter-7 General Profile of the District 25

Chapter-8 Land Utilization Pattern in the district: Forest, Agriculture,

Horticulture, Mining etc.

26

Chapter-9 Physiography of the District 28

Chapter-10 Rainfall: month-wise 31

Chapter-11 Geology and Mineral Wealth

Drainage System with description of main rivers.

Salient Features of Important Rivers and Streams

33

Chapter-12 Status of Brick Kilns in Lakhisarai 38

References 39

Annexures 40


CHPATER-1 Introduction

As per Gazette Notification S.O. 141(E) Dated 15th January, 2016 vide S.O. 3611(E) Dated 25th

July, 2018 a survey shall be carried out by the District Environment Impact Assessment Authority

(DEIAA) with the assistance of Geology Department or Irrigation Department or Forest

Department or Public Works Department or Ground Water Boards or Remote Sensing

Department or Mining Department etc. in the district for preparation of District Survey Report as

per the sustainable sand mining guidelines to ensure identification of area of aggradations or

deposition where mining can be allowed, and identification of areas of erosion and proximity to

infrastructural structures and installation where mining should be prohibited and calculation of

annual rate of replenishment and allowing time for replenishment after mining in that area.

Every effort has been made to cover sand mining locations, areas and overviews of mining

activity in the district with all the relevant features pertaining to geology and mineral wealth in

replenish-able and non-replenish-able areas of rivers, stream and other sources. The mineral

potential is calculated based on field investigation taking coordinates of the area and gather all

relevant information and geology of the catchment area of the river or stream. Also gather all

data for bricks mining, taking area coordinates with local soil quality, availability of soil etc. Also

as per the site condition and location depth of mineable mineral is defined. The area of removal of

mineral in the river and stream is decided on geomorphology and other factors, it can be 50% to

60% of the area of a particular river or stream. Similarly for bricks and soil mining all data will be

gathered. Other constituents like clay and slit are excluded as waste while calculating the mineral

potential of particular river or stream. This District Survey Report shall form the basis of

application for environmental, preparation of reports and appraisal of projects. The report shall be

updated once every 5 years.


Administration

Lakhisarai district was a carved out of erstwhile Munger district on 3rd July 1994. Earlier it

was a sub-division within Munger District. It is located in southern part of Bihar state and

extends from 250 01’ to 250 22’ North Latitude and 850 50’ to 860 17’ East Longitudes with

a geographical area of 1301 sq km. The district is bounded on the north by Patna and

Begusarai districts, on the west by Nalanda and Sheikhpura, on the east by Munger, while on

the south it is bounded by Jamui district. Lakhisarai district is a part of Munger division. It has

06 developmental blocks (Fig.-1) comprising 476 villages with its headquarters at Lakhisarai.

The total population of the district is 4476043 as per census year 2011 with a Rural: 4311466

& Urban 164577 population.

Figure: Present Locations / Subdivision / Blockwise Map of Lakhisarai District

Lakhisarai was an established administrative and religious centre during the golden period of

Pal bansh. Lord Buddha also stayed here for three years on Chaliya Mountain and delivers the

Sermons.

Topography

The landscape in the district lies in south of the Ganges River in the Gangetic plain apart of

Angakshetra. Its height from sea level is 73 ft. the soil of the district is very fertile so it is rich

in agriculture. This district is blessed with Ganga & Harohar River which is perennial in

nature and Kiul River which is rain fed. Ganga and Harohar bring alluvial soil in times of

flood and maintains the fertility of soil. It has vast stretch of low lying area known as TAL

area which is famous for pulses production in the state.


Basin/sub-basin, Drainage

Lakhisarai district forms a part of Phalgu-Kiul sub-basin of Ganga Basin. The district

comprises catchments of Ganga and Kiul river systems. The district is having moderate to low

drainage density with dendritic and radial patterns dominating in the hilly regions, while

parallel to sub-parallel drainage pattern in the plains. The Ganga, Kiul and Harohar are the

three main rivers flowing through the district. The Ganga flowing to the east touches the

northern border while Kiul river flowing to the north almost bisects the district and joins the

river Ganga in the north.

Irrigation Practices

The agro climatic condition of the district favours the plantation of cereal crops such as

paddy, wheat, maize etc and pulses like gram and masoor. These together with vegetables

form the main crops. Irrigational facilities are not sufficient. There are only two irrigation

systems, the Kiul minor irrigation and Shringi Rishi dam.

As per the statistics of year 2004-2005 (Govt. of Bihar) the gross irrigated area is 51384

hectares where 30017ha is irrigated by deep and shallow tube wells, 16640 ha by canals and

4632 ha by other sources out of total cultivable area of 86151 hectare. Conjunctive use of

surface and ground water can bring the desired development in this water scarce district.

Connectivity:

Lakhisarai is well connected to the rest of the state and India by rail, road and air connections.

By Air: Jai Prakash Narayan International Airport, Patna is the nearest Airport from

Lakhisarai district. Patna is linked by regular flights to important cities like: Delhi, Kolkata

Varanasi, Lucknow and so on. One can also reach Patna from Katmandu.

By Road: A convenient road network covers Lakhisarai connecting it to a number of

important cities in Bihar, such as: Patna (80 km), Muzaffarpur (115 km), which are in turn

linked to rest of the country.

By Rail: The Major railway station is Lakhisarai in the district. Important trains run through

the railway station regularly for Kolkata, Jharkhand Orissa and other States. One can approach

Lakhisarai from major cities from all over India like: Delhi, Kolkata, Mumbai, Chennai etc.


Location / Subdivision / Block wise Map of District


Demography of Lakhisarai District

Lakhisarai 35th in terms of population (10,00,912) and 34th in terms of area (1,228 sq.km)

inthe state of Bihar.

In terms of population per sq.km. Lakhisarai is the 32st densely populated district in the

state with 815 persons per sq.km as against the states 1,106.

Lakhisarai ranks 29th in terms of sex-ratio (902) against the state’s 918.

Lakhisarai ranks

33th in terms of

children-ratio (920)

against state’s 935.

There are 110

uninhabited villages

(out of 472 total

villages) in the

district of Lakhisarai.

Surajpur (under

SurajgarhaC.D.

Block) is the most

populated village

(13,438) and

Ratanpur(under

Surajgarha C.D.

Block) is the least

populated village (3)

in the district.

C.D. Block

Surajgarha has the

highest number of

villages (184) in the district and C.D. Block Pipariya has the lowest number of villages

(22).


Hill Block (under Surajgarha C.D. Block) has the largest area (7,580 hectare) and 5

villages (underSurajgarha C.D. Block) have the smallest area (1 hectare each) among the

villages in the district.

Source: Census of India 2011

Natural Divisions

Lakhisarai is a beautiful and important place in the state of Bihar. Lakhisarai district was

established on the 3rd of July 1994. Before coming into existence as a new district, Lakhisarai

was a sub-division within Munger District. Historians established on the basis of analysis of

evidences, that this place was a reputed religious center for the Hindus in the period of Pal. The

ruler of that time was fond of making Temples and other religious spots. It is one of the reasons

that there are so many temples and other religious places within this region. Some significant

temples and religious spots within the district are Ashokdham, Bhagwati Mandir of Barahiya,

Sringi Rishi, Jalappa Asthan, Abhainath Asthan on Abhaipur Mountains, Maharani Asthan of

Abhaipur, Govindbaba Asthan (Mandap) Rampur and Durga Asthan Lakhisarai etc.

The district can be divided into three parts viz.

(i) Hilly area : The hilly area comprises of hill series and rocks like Kachhua hills, Kajra

Mountains up To Abhaipur and Jaynagar Mountains including forest area

(ii) Flood hit area: Almost whole of Pipariya block and some part of Barahiya is

considered as flood hit area. This area remains almost drowned in rainy season. But so

far as cultivation and agriculture is concerned this area is called the stock of food

Grains

(iii) Plain area: Rest of the part except Hilly and flood hit area is plain area with full

greenery and cultivable land.

Railway main and loop line and NH 80 pass through the district headquarter, paving the way for

its development. Railway main line and loop line cross each other at Kiul Junction.

Rivers

The Ganges, Kiul and Harohar are the main three rivers flowing through the district. The Ganges

fixes the north east border, while Harohar separates Diyara region from the other parts of the

district and Kiul River almost bisects the whole district. Due to these rivers Lakhisarai district is

good in cultivation and forest. These rivers impart prosperity to the people and play an important


role in making this district significant and unique. River Kiul also, by depositing top quality of

sand, plays an important role in the economy of the district and creates an opportunity of

employment too.

Climatic conditions

The climate of the district is somewhat extreme in nature, i.e., quite hot during the summer and

fairly cold during the winter. January is the coldest month when the mean minimum temperature

comes down to approximately 4oC. The temperature starts rising from March and reaches its peak

in May when the mercury touches about 45oC. Rain starts sometime in mid-June and lasts till

mid-September. The district gets easterly winds from June to September, and from October to

May wind direction reverses. Maximum rains occur during the months of July and August (289

mm). Sometimes winter rains occur in Jan-February

Forest

Lakhisarai district has got the forest area coverage of 33225.26 acres in which no dense forest is

present. The forest area of district has presence of Teak Wood, Seesam, Paisar, Kendu, Amla,

Mahua, Mango, Neem and Gamhar Tree. The District has forest coverage in only 10.46 percent

area of the total geographical area and so industrial and commercial exploitation of the forest is

very less


CHAPTER - 2 Overview of Mining Activity of District

Geomorphology of the district The district has a diverse landscape ranging from hills to flood plains. The major geomorphic

units are rocky upland; Pedi plain, alluvial plain and flood plains The Rocky Upland area

comprises series of Kachhua and Kajra hills. These hill tracts constitute elevated and rugged

landmasses surrounded by alluvial plains. The altitude of hills varies from 250 to 500m amsl. It

comprises mainly quartzite, phyllite and schist of Kharagpur formation. The rocks of Kharagpur

formation have undergone tectonic deformation giving rise to variety of deformational structures.

The rocky uplands are limited mainly in Surajgarha block.

a) Pedi plain is represented by an area formed through coalescence of pediments and thus

forms rolling topography and comprises residual soil overlain by mixture of sheet wash

deposits. It extends all along the Kharagpur hills.

b) Older Alluvial Plain forms a major part of the district. It comprises sediments deposited by

Ganga River and also the sediments derived from the denudation of Chota Nagpur plateau

and Kharagpur hills. This is also known as marginal alluvial plain due to its limited

thickness. Although the thickness of this alluvium at Ashok dham village is about 123m but

reduces considerably in the southeastern parts ranging from 15 to 20m.

c) Younger Alluvial Plain forms the northern parts of the district and stretches few km to the

south of Ganga rive. Almost all of Pipariya and some part of Barahiya blocks are

considered as flood prone area. These areas remain inundated in rainy season. Locally, this

is called “Tal” area. Diara area is level to gently undulating ground. The mighty Ganga

meanders in this parts and usually remains flooded from middle of July to the end of

September. The relief of this plain varies on an average from 25 to 65m above mean sea

level.

Approach to Sand Mining:

River sand mining is a common practice as habitation concentrates along the rivers and the

mining locations are preferred near the markets or along the transportation route, for reducing the

transportation cost. River sand mining can damage private and public properties as well as aquatic


habitats. Excessive removal of sand may significantly distort the natural equilibrium of a stream

channel.

Main objectives of Sustainable Sand Mining:

To ensure that sand and gravel mining is done in environmentally sustainable and socially

responsible manner.

To ensure availability of adequate quantity of aggregate in sustainable manner.

To improve the effectiveness of monitoring of mining and transportation of mined out

material:

Ensure conservation of the river equilibrium and its natural environment by protection and

restoration of the ecological system.

Avoid aggradations at the downstream reach especially those with hydraulic structures

such as jetties, water intakes etc.

Ensure that the rivers are protected from bank and bed erosion beyond its stable profile.

No obstruction to the river flow, water transport and restoring the riparian rights and in

stream habitats.

Avoid pollution of river water leading to water quality deterioration.

To prevent depletion of ground water reserves due to excessive draining out of ground

water.

To prevent ground water pollution by prohibiting sand mining on fissures where it works

as filter prior to ground water recharge.

To maintain the river equilibrium with the application of sediment transport principles in

determining the locations, period and quantity to be extracted

Streamlining and simplifying the process for grant of environmental clearance (EC) for

sustainable mining.


Figure 2.1 River Basin Map of Bihar Mode of grant of mineral concession

i) Before giving details of actual sites/number of sites or mineral concessions it would be

appropriate to explain that the mineral concession respect of minor minerals area granted

as per provisions of the state rules, Framed by the respective state Government in

Exercise of power under section 15 of the Mines and Minerals (D&R) Act,1957

ii) The state of Bihar at the time of bifurcation opted Prevailing rule Namely “Bihar Minor

Minerals Concession Rules 1972” and amended by 2014.These Rule were amended form

time to time as per policy of the state government for minor minerals. The Hon’ble

Supreme Court vide its order dated 27.02.2012 directed all state Government to revise

their state rule making provisions in accordance with various recommendations contained

in the report of the group of MOEF&CC, on mining of minor and the model draft

guidelines issued by Ministry of Mines, Gol


iii) Accordingly, the state of Bihar Comprehensively revised its State Rules namely the

“Bihar Minors Minerals Concession, Stocking, Transportation of Minerals and Prevention

of illegal Mining Rule, 2014” repealing the Prevailing Rules namely Bihar Minors

Minerals concession Rules 1972”.

iv) The Mineral concession in the Bihar are being Granted in the form of “Mining Contract”

or Mining Lease” through competitive bidding process. In district Lakhisarai minerals

concessions are granted in the form of mining contact for the period up to 31.12.12019.

The contracts are been granted through open auction mode. The Mineral concession are

being granted subject to condition that actual mining operation shall be allowed only after

Environment Clearance is/are obtained from the competent authority as per requirement of

EIA Notification dated 14.09.2006 of the MoEF&CC, GoI.

v) The Mineral concession holder are required to prepare detailed “ Mining Plan” for their

specific project through Registered Qualified Person and get in approved from authorized

officer of Mines and Geology Department of the State Government. The exhaustive

mining plan are prepared by RQP giving details of minerals reserves, method of mining,

Progressive closure plan, extent of proposed mining and other related details. These are

the project specific details are based on these details itself the project proponents/minerals

concession holder obtains environmental clearances.

Method of Mining and Condition in Which Mining in River Bed Areas is to be allowed

i. The river bed area apart from other related condition for mining are allowed to excavate

minerals (sand) to ensure safety of river bed structures and the adjoining area on the

following specific conditions:

a. No mining would be permissible in a river bed up to a distance of five times of the span

of a bridge on upstream side and ten times the span of such bridge on down-stream side,

subject to a minimum of 250 meters on the downstream side:

b. There shall be maintained an un-mined block of 150 meter width after every block of 1000

meters over which mining in undertaken or at such distance as may be directed by the

Director or any officer authorized by him.

c. The Maximum depth of mining in the river-bed shall not exceed three meters measured

form the un-mined bed level at any point in time with proper bench formation.

d. Mining shall be restricted within the central 3/4th width of the river rivulet:


e. Note: The above said conditions have been decided after detailed discussions and

recommendations of the concerned Department, Government of Bihar.

ii. As the mining river bed remains restricted in the in the central 3/4th part of the river bed,

the area left on both on side of the river bank not only ensures the safety of banks (bank

cutting due to water stream) but also ensures that in the central part of river, water stream

flows smoothly during rains and process of river and process of river meandering does not

occur.

iii. The light weight excavator/JCBs are being deployed to remove mineral form river bed up

to maximum depth of 03 meter layer form general level of the bed. The mining in the river

bed are undertaken in mechanized manner. At times the RQPs do refers the excavation in

river bed mining through excavators as “Semi Mechanized Mining”.

iv. The mineral excavated is directly loaded in the vehicles/dumpers and the vehicles owners

and driver take away the minerals directly to the stone crushers or screening plants or

consumers. In certain cases minerals concession holder stacks mineral on the river bank in

case are not able to sell the material on actual mining itself.

Method of Mining in Areas outside River Bed Areas:

i. As the mineral (sand) are around river beds area also to ensure that mining from outside

do not effect river. No mining is being permitted in an area up to a width of 500 meters

form the active edges of embankments in case of river 250 meter in case of bridge and 100

meter on either side of all other rivers/rivulets.

ii. The mineral from outside area river bed is being permitted subject to condition a safety

margin of two meter (2m) shall be maintained above the ground water table while

undertaking mining operation shall be permissible below this level unless a specific

permission is obtained from the competent authority in this behalf further the depth of

excavation of minerals shall not exceed nine meter (9m) at any point of time.

iii. The method of excavation is such that the mining contractors deploys earth moving

machineries and after removing the top layer of original soil, varying between 1 to 1.5

meter stacks the same separately. Thereafter removes the minor minerals deposits. After

undertaking the mining i.e. removing of minerals layer up to a maximum depth of 09

meter, the top stacked soil is again spread back into the pit. The mined out area/land in put

to reuse for cultivation after spreading the top soil. The landowners/farmers give their land


to the contractors for mining after getting compensation, mutually settled between the

landowner and the mining contractor.

Method of Mining in river bed area (semi mechanized/or manual)

i. The Hon’ble NGT with regards to rivers bed mining has specifically desired to examine

the mode of mining- shall the same be semi mechanized/mechanized or manual.

ii. There is no specific definition of Semi- Mechanized Mining. The team Semi-mechanized

mining in general is used were method of working in general are undertaken

mechanically. However, some operation are also undertaken manually.Therefore the semi

mechanized mining or mechanized mining is the method of working sometime

mechanized mining with light machines are also referred as semi –mechanized mining.

The term semi mechanized mining is being used in general parlance where in the very

same mining area in part area as per requirement manual mining is also under taken along

with mechanized mining of sand/river bed mining.

iii. Where Manual mining operation are undertaken using conventional hand tools only like

chisel, hammer and crowbar etc.and operation are only labour intensive. As per

requirement manual lifting of sand and directly loading intensive, as per requirement

manual lifting of sand and directly loading the sand in tractor trolleys etc. through labours

itself.

iv. The Mechanized mining operations in respect of sand mining are undertaken with help of

excavator-cum–loaders. In this process sand is lifted/excavated from the river bed through

excavator-cum loader and directly loaded in dumpers or other mode of transport. The

vehicles carrying the minerals form mines to site of use/site of construction or sale stocks

outside lease hold area (an independent business than that of mining).

v. In the current scenario it is impractical to undertake manual mining because:-

i. The labour are not easily available.

ii. Manual mining cannot be under taken in systematic and scientific manner as compared to

mechanical mining which can be undertaken systematic/scientific and controlled mining.

iii. In case of manual mining to achieve desired level of production more number of

manpower would be required meaning thereby human interface within river bed area

would increase and more ecological damage would be caused.

vi. The method of mining even otherwise can be uniform even for same area and all the

methods have their own pros and cons,however,considering the current scenario wherever


feasible mechanized (semi-Mechanized or mechanized is same thing) mining should be

preferred over manual method.

General Regulation relating to Mining

I. As per prevailing state rules the mineral concession holder are required to get a mining

plan for the area prepared form a “Registered Qualified Person’. The mining plan includes

the area specific details along with the mine closure plan (progressive & Final ) taking into

consideration the details of the geology and lithology of the area including the estimated

mineral reserve of the area. Proposed method of mining/development of mines, use of

explosives and blasting operation. If any stacking and disposal of minerals, mine-drainage

pattern, handing of the overburden, location of weight bridge and minerals processing ,if

any .The extant of manual mining or mining with the use of machinery and mechanical

device along level of production (production form year-to year for a period of five

years),Mechanization, Type of Machinery to be used, nature and extent of the minerals

body/spot or spots where the mining operation area proposed to be undertaken, natural

water occurs, limits of minerals reserve and other forest area and density of trees, if any

assessment of impact of mining activity on land environment management plans, In

addition to this mining plan also suggests the details of area of restoration/rehabilitation of

the area through afforestation, land reclamation, use of pollution control devices and such

other measure as may be directed by the state Government from time to time.

II. The Mining plan area to be got approved form the authorized officer of the state

Government, Based on mining plan prior environment clearance from the competent

authority as per provisions of EIA Notification dated 14.09.2006 of MoEF&CC, Gol.

III. After obtaining the Environment clearance as Further, to comply with requirement of Air

Act, 1981, the consent to establish and consent to operate from State pollution Control

Board are also obtained before actual mining.

IV. The above said provision mainly related to mineral conservation and environmental

protection with regard to provisions related to safety in mines and welfare of labours

provisions under mines acts 1952 are ensured by the Directorate General Mines Safety De

Ministry of Labour, Government of India.


Area Selected for Mining in District Lakhisarai:

I. As per rough estimate total area of river beds (Ganga, Kiul, Harohar and

tributaries/rivulets) passing through district Lakhisarai is about 39.55 Sq.km. Area

outside river bed is also having mineral deposits. A large part of which is

otherwise under various uses including agriculture. As regards selection of area for

mining it may be pointed out that:-

i. Earlier,(about 16-18 years back) mineral concession /mining contracts were being

granted on revenue estate basis (without giving any specific details of areas)subject

to various restrictions. The minerals concession holder used to undertake mining in

area after living restricted area.

ii. Needless to state that such material concession area use to have even the area

having no mineral deposit, the area otherwise not permissible for mining. The

Mineral concession holders were under obligation to undertake mining only in the

area free from all restriction and as per prevailing all rules and regulation. Mineral

Concession for minor Mineral prior to 14.09.2006 were not required to obtain

environmental clearance.

iii. The EIA notification dated 14.09.2006 became applicable for fresh contacts/ leases

and in the year 2008 for grant of mineral concessions in respect of other area in the

state fresh auction was notified subject to condition that will be allowed to be

undertaken only after prior environment clearance to obtained as per requirement

of EIA notification dated 14.09.2006 of MoEF&CC, Gol. However, said condition

was challenged by some prospective bidders on the plea that the notification date

14.09.2006 was not applicable for mining minerals.


CHAPTER - 3 List of Mining Leases in the District with location, area and period of validity

List of Mining Leases in the District with location, area and period of validity is attached as-

Sl. No.

Mining Unit Block Location Area (In Hect.)

Period (In Yrs) Name of Minor

Minerals

1 Village- Sharma,

Panchayat- Sharma,

Block- Lakhisarai

24.9 Up to 31st December, 2019

Sand

2 Village- Ramal Bigha,

Panchayat- Bhalui,

Block- Chanan


Sand

3 Village- Raota,

Panchayat- Kundar,

Block- Chanan


Sand

4 Village- Dumrahi,

Panchayat- Dumrahi,

Block- Chanan


Sand

5 Village- Rampur,

Panchayat- Iton,

Block- Chanan


Sand

6 Village- Moliya,

Panchayat- Moliya,

Block- Chanan


Sand

7 Village- Nagardar,

Panchayat- Iton,

Block- Chanan


Sand

8 Village- Jhinora,

Panchayat- Mahisauna,

Block- Lakhisarai


Sand

9 Village- Kishanpur,

Panchayat- Rampur,

Block- Suryagarha


Sand

Note: List of identified sand ghats in the district is attached as annexure-I


CHAPTER - 4

Details of Royalty or Revenue received from Sand or minor minerals in last three years

Sr. Year Revenue (In Lakh Rs.)

1 2014-15 2364.49

2 2015-16 1589.31

3 2016-17 822.17

Total 4775.97

CHAPTER - 5 Details of production of Sand or Bajri or Minor Mineral in Last three

There was no EC approved gaht in Lakhisarai district before year 2018. Hence the production

details of sand minerals is NIL


CHAPTER - 6

Process of Deposition of Sediments in the rivers of the District Process- Sediment is a naturally occurring material that is broken down by processes of

weathering and erosion, and is subsequently transported by the action of wind, water and/or by

the force of gravity acting on the particles. Sediments are most often transported by water.

Sediment is transported based on the strength of the flow that carries it and its own size, volume,

density, and shape. Stronger flows will increase the lift and drag on the particle, causing it to rise,

while larger or denser particles will be more likely to fall through the flow.

Deposition is the processes where

material being transported by a

river is deposited. Deposition

occurs when a river loses energy.

This can be when a river enters a

shallow area (this could be when it

floods and comes into contact with

the flood plain) or towards its

mouth where it meets another body

of water.

Rivers flood on a regular basis. The area over which they flood is known as the floodplain and

this often coincides with regions where meanders form. Meanders support the formation of flood

plains through lateral erosion.

When rivers flood the velocity of water slows. As the result of this the river's capacity to transport

material is reduced and deposition occurs. This deposition leaves a layer of sediment across the

whole floodplain. After a series of floods layers of sediment form along the flood plain.

Larger material and the majority of deposition occurs next to the river channel. This is the result

of increased friction (with the flood plain) causing the velocity of the river to slow and therefore


rapidly reduce its ability to transport material. This leaves a ridge of higher material next to the

river channel on both banks of the river known as a levee.

If the upwards velocity approximately equal to the settling velocity, sediment will be transported

Downstream entirely as suspended load. If the upwards velocity is much less than the settling

velocity, but still high enough for the sediment to move, it will move along the bed as bed load by

rolling, sliding, and saltating (jumping up into the flow, being transported a short distance then

settling again). If the upwards velocity is higher than the settling velocity, the sediment will be

transported high in the flow as wash load.

As there are generally a range of different particle sizes in the flow, it is common for material of

different sizes to move through all areas of the flow for given stream conditions.

The various factors governing the occurrence and deposition of sand is country rock i.e.

geological disposition, climate, and rainfall, water load physical parameters of river and velocity

of water current. 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 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.

Capacity & Competence Rivers can only carry so many loads depending on their energy. The

maximum volume of load that a river can carry at a specific point in its course is called the age

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.

A river system can be divided into three subsystems:

Collecting system (branches) -- consisting of a network of tributaries in the headwater

region, collects and funnels water and sediment to the main stream.

Transporting system (trunk) -- the main trunk stream, which functions as a channel way

through which water and sediment move from the collecting area toward the ocean.

(Erosion and deposition also occur in a river's transporting system)

Dispersing system (roots) -- consists of a network of distributaries at the mouth of a river

(delta), where sediment and water are dispersed into an ocean, a lake, or a dry basin


Removal of washed in Silt Load

Geologically, the district from part of the vast Indo-Gangetic alluvial tract. The origin of the Indo

-Gangetic tract as a whole is now attributed to the sag in the earth crust formed in the upper

Eocene times between Gondwana land and the raising of Himalaya belt. The economic minerals

found in the district are Sand, Soil and Stone.

The sand deposits being an integral part of the dynamic river system to which it belongs.

Therefore, as a part of natural cycle, the monsoon flow of every river carries with it replenishment

of silt and washed out soil and clay from upstream areas in the catchment. This silt shall be

removed during the sieving of sand before it is loaded into truck/tipper/trailer to carry to the

consumers.

Sand mining is critical to infrastructure development around the globe. Sand is an essential minor

mineral used extensively across the country as a useful construction constituent and variety of

other uses in sports, agriculture, glass making (a form of sand with high silica content) etc. The

rivers are the most important source of Sand. It acts as source of transportation and deposition of

sand etc.


CHPATER-7

General Profile of the District

Lakhisarai district was a carved out of erstwhile Munger district on 3rd July 1994. Earlier it was a

sub-division within Munger District. It is located in southern part of Bihar state and extends from

250 01’ to 250 22’ North Latitude and 850 50’ to 860 17’ East Longitudes with a geographical

area of 1301 sq km. The district is bounded on the north by Patna and Begusarai districts, on the

west by Nalanda and Sheikhpura, on the east by Munger, while on the south it is bounded by

Jamui district. Lakhisarai district is a part of Munger division. It has 06 developmental blocks

(Fig.-1) comprising 476 villages with its headquarters at Lakhisarai. The total population of the

district is 4476043 as per census year 2011 with a Rural: 4311466 & Urban 164577 population.

District profile is as presented below in table.

Sl. No. Particular Year Unit Statistics 1 Geographical features

(A) Geographical Data i) Latitude 250 to 25025’N ii) Longitude 85055’ E to86025’E iii) Geographical Area Acre 317787.77

(B) Administrative Units Sub divisions 01 Tehsils 06 Nagar Palika 01 Gram Panchayats 80 Revenue villages 460 Assembly Area 02

2. Population

(A) Sex-wise Male 2001 417672 Female 2001 384553

(B) Rural Population 2001 561205 3. Agriculture A. Land utilization

Total Area 2010-11 Acre 317787.77 Forest cover 2010-11 “ 33225.26 Non Agriculture Land 2010-11 “ 7513.82 Cultivable Barren land 2010-11 “ 1871.25

4. Forest (i) Forest 2010-11 Ha. 33225.26


CHPATER-8

Land Utilization Pattern in the district: Forest, Agriculture, Horticulture, Mining

Forest

Lakhisarai district has got the forest area coverage of 33225.26 acres in which no dense forest is present. The forest area of district has presence of Teak Wood, Seesam, Paisar, Kendu, Amla, Mahua, Mango, Neem and Gamhar Tree. The District has forest coverage in only 10.46 percent area of the total geographical area and so industrial and commercial exploitation of the forest is very less.

Crop

The agroclimatic condition of the district favours the plantation of various crops. Paddy, Wheat, Maize are the main cereal crops of the district. Different cropping patterns are adopted by the cultivators in different areas. In Taal area pulses like Gram and Masoor occupy maximum area, while in Ganga region Wheat, Maize, Mustard, Pea, Green Vegetables are the main crops. In Hilly area and other parts of the district Paddy is the main crop. In few areas Potato and Onion are also cultivated. The yeild rate (Quintal/hect.) of different crops are as follows:- Wheat,(In irrigated area 30-35, in Non irrigated area 15-20) Paddy(35-40) Gram(20-22), Maize(Rabi 60-62, Khariff 40-45), Pea(15-20) Masoor (18-20) Arhar (20-25) Mustard(10-12) Flood affected Tall and Ganga regions mostly in rainy season and in this region Rabi is the main crop . The cropping pattern in the district is (a) Paddy- Wheat (b) Paddy- Potato-Onion (c) Maize-Wheat-Green vegetable (d) Gram- Sarso.There is a good scope for scientific and rotation of crops for higher yeild.

Irrigation

The main natural water resources are rivers, fountains, Canals and rain fall. Planned irrigational. Facilities within the district are not sufficient. There are only two irrigation systems, Kiul minor irrigation and Shringi Rishi Dam which irrigate less than 10 percent of the total cultivable land area of district. Farmers depend either upon nature or private irrigational systems i.e Hand Pump, Boring, Local water storage or on Ponds for irrigation of their fields.

Horticultural

The district- wise analysis of the area and production of horticultural crops (fruits, vegetables, and flowers) reveals a substantial spread of horticultural production across the district. The horticultural development in the district has is very low and placed among twelve districts namely Lakhisrai, Jamui, Banka, Purnia, Sitamarhi, Gaya, Katihar, Jehanabad, Bhojpur, Kaimur, Buxar and Supaul.


Mineral resources

Sand is major mineral of Lakhisarai district of Bihar. Yellow sand in Kiul river is major source of revenue collection in district as well as soil / clay is actively mined for bricks and pottery industry. In the financial year, huge amount of clay was produced for these purposes. It is also used as a decorative material in landscaping. Specific types of sand are used in the manufacture of glass and as a molding material for metal casting. Wide flood plains and high banks are the common features in the course of the Ganga and the Kiul along with silt and clay deposits. Stone is also a source of minor mineral in Lakhisarai district of Bihar. Land utilization patter is presented as below-

A. Land utilization

i) Total Area 2010-11 Acre 317787.77

ii) Forest cover 2010-11 “ 33225.26

iii) Non Agriculture Land 2010-11 “ 7513.82

v) cultivable Barren land 2010-11 “ 1871.25

B. Forest

(i) Forest 2010-11 Ha. 33225.26


CHPATER-9 Physiography of the District

Hydrogeology

Hydro-geologically, the district is divided into two parts (a) hard rock/ fissured formation (b)

unconsolidated / porous formations (Fig.-5))

a) The hard rock / fissured formation: It comprises rocks of Chotanagpur gneissic

Complex (CGC) and Kharagpur formation. They are composed mainly of granite

gneisses, quartzite’s and phyllites. In general, these rocks possess poor aquifers until or

unless they have developed secondary porosities by means of weathering and/or

fracturing. The drainage pattern of the terrain indicates that the basement rocks have

undergone poly-tectonic deformations giving rise to deep seated tensile and shear

fractures. These fractures appear on the surface in the form of lineaments. The lineaments

are potential areas for ground water exploration and recharge. Weathered residuum,

saprolite zone and fractures within 15 - 35m depths constitute shallow aquifers. In

Lakhisarai district, two bore

wells have been drilled and

the maximum depth drilled is

135m at Gunsagar village in

Halsi block. Ground water

occurs generally under semi-

confined condition in these

areas.

b) Porous Formation: The

Quaternary alluvium

constitutes this hydro

geological unit. Its thickness

is maximum in the northern

and western parts of district,

while in eastern and southern

part reduces to as low as 5m.

The variation in thickness of the alluvium is mainly due to uneven bedrock topography


and proximity of hill ranges. The alluvium comprises clay, silt and sand of various

thickness. Aquifers in this formation occur under unconfined to semi-confined conditions.

CGWB has drilled 04 tube wells in this formation and maximum thickness of alluvium is

123 m at Ashokdham village of Lakhisarai block. In general the alluvial thickness varies

from 60 to over 120m. Details of exploratory bore wells drilled are given in table1.

There are four hydrographs network station (HNS) in the district. These HNS are being

monitored four times in a year since 1975 by CGWB. The pre-monsoon 2011, water level in the

district ranges between 7.58 to 9.8 and in post-monsoon 2011, its ranges between 1.28 to 6.09 m

bgl. Long-term water level data (2002-2011) indicate no significant declining in water levels.

Ground Water Resources:

Dynamic ground water resources of the district were estimated (GEC-1997, norm) in the year

2009 by adopting groundwater estimation methodology 1997, Govt. of India. There are wide

variations in the ground water potential of various hydrogeological units identified in the district.

The net annual replenishable ground water resource of the district is 27941 ha m. The gross draft

for all uses is 11719 ha m and allocation for domestic and industrial requirement supply by next

25 years is 2100 ha m. The present stage of ground water development of the district is 41.9% and

hence all the six blocks of district fall under safe category for ground water development. At

present, maximum ground water development has taken place in Ramgarh Chowk Block (65.3%),

while minimum in Barahia block (24.5%).

Geomorphology

The district has a diverse landscape ranging from hills to flood plains. The major geomorphic

units are rocky upland, Pedi plain, alluvial plain and flood plains The Rocky Upland area

comprises series of Kachhua and Kajra hills. These hill tracts constitute elevated and rugged

landmasses surrounded by alluvial plains. The altitude of hills varies from 250 to 500m amsl. It

comprises mainly quartzite, phyllite and schist of Kharagpur formation. The rocks of Kharagpur

formation have undergone tectonic deformation giving rise to variety of deformational structures.

The rocky uplands are limited mainly in Surajgarha block.

a) Pedi plain is represented by an area formed through coalescence of pediments and thus

forms rolling topography and comprises residual soil overlain by mixture of sheet wash

deposits. It extends all along the Kharagpur hills.


b) Older Alluvial Plain forms a major part of the district. It comprises sediments deposited by

Ganga River and also the sediments derived from the denudation of Chota Nagpur plateau

and Kharagpur hills. This is also known as marginal alluvial plain due to its limited

thickness. Although the thickness of this alluvium at Ashok dham village is about 123m but

reduces considerably in the southeastern parts ranging from 15 to 20m.

c) Younger Alluvial Plain forms the northern parts of the district and stretches few km to the

south of Ganga rive. Almost all of Pipariya and some part of Barahiya blocks are

considered as flood prone area. These areas remain inundated in rainy season. Locally, this

is called “Tal” area. Diara area is level to gently undulating ground. The mighty Ganga

meanders in this parts and usually remains flooded from middle of July to the end of

September. The relief of this plain varies on an average from 25 to 65m above mean sea

level.

Soils

The Lakhisarai district consists mainly of Inceptisols, Entisols and Alfisols group of soils

generated under different lithological and pedogenic conditions. Calcareous alluvial soil of

Inceptisols group occurs on the southern bank of Ganga, particularly in Barahiya and Pipariya

blocks. Younger alluvial soil of Entisols group occurs in major part of the district. It is deficient in

nitrogen, phosphoric acid and humus. Texturally these soils are sandy to loamy and the pH value

is on the alkaline side. Older alluvial soil of Alfisols group is developed mainly in the marginal

areas along the foothills


CHPATER-10 Rainfall: Month-wise

Climograph / Weather by month Lakhisarai

Lakhisarai's climate is classified as warm and temperate. The summers here have a good deal of rainfall, while the winters have very little. This location is classified as Cwa by Köppen and Geiger. The average annual temperature is 26.3 °C in Lakhisarai. The rainfall here averages 919 mm.

The least amount of rainfall occurs in November. The average in this month is 1 mm. Most of

the precipitation here falls in July, averaging 235 mm.


Average temperatures Lakhisarai

The temperatures are highest on average in May, at around 32.9 °C. January is the coldest month,

with temperatures averaging 17.6 °C.

Lakhisarai Weather by month / Weather Averages

January February March April May June July August September October November December

Avg. Temperature

(°C) 17.6 20.5 26.1 30.7 32.9 32.1 29.7 29.3 28.9 27.1 22.1 18.6

Min. Temperature

(°C) 10.9 13.3 18.6 23.5 26.4 27.3 26.5 26.3 25.7 22.5 15.3 11.5

Max. Temperature

(°C) 24.3 27.7 33.6 38 39.5 36.9 32.9 32.4 32.2 31.7 29 25.7

Avg. Temperature

(°F) 63.7 68.9 79.0 87.3 91.2 89.8 85.5 84.7 84.0 80.8 71.8 65.5

Min. Temperature

(°F) 51.6 55.9 65.5 74.3 79.5 81.1 79.7 79.3 78.3 72.5 59.5 52.7

Max. Temperature

(°F) 75.7 81.9 92.5 100.4 103.1 98.4 91.2 90.3 90.0 89.1 84.2 78.3

Precipitation / Rainfall (mm) 13 6 10 8 28 115 235 233 191 78 1 1

The variation in the precipitation between the driest and wettest months is 234 mm. throughout

the year, temperatures vary by 15.3 °C.

Source: CLIMATE –DATA.ORG https://en.climate-data.org/location/24598/


CHPATER-11

Geology and Mineral Wealth

(i) Regional Geology

Geologically, it represents nearly two third of Bihar is under cover of Ganga basin composed of alluvium and masks the nature of basement rocks.

Geological succession and their occurrences distribution

Age Geology Occurrences

Quaternary Alluvial Deposits(sand, clay, silt, Fragments)

North Bihar Plain & Central Bihar Plain

Tertiary Sand Stones& Clay Stones North Champaran Hills

Gondwana Coal Measures, Forming a series of small outlier basins

Banka District

Vindhyans Sandstones, shales, Limestones etc. Parts of Bahbhua and Rohtas Disricts

Satpura Schist, Phyllite, Quartzite Part of Aurangabad, Gaya, Nawada, Nalanda, Sheikhpura and Munger District

Proterozoic Schist, amphibolites, quartzite, granites, dolerites and pegmatites

Nawada, Jamui and Banka

Archaean Gneisses, Granites, Schists, Phyllites, quartzites, amphibolites & intrusive all metamorphosed sedimentary and

igneous rocks

Part of Aurangabad ,Gaya, Nawada ,Jamui, Banka and Bhagalpur

(ii) Local Geology of the area

The river sand exposed in the river beds of Kiul, Ganga and surrounding areas is the product of

the deposition of the sediments brought and deposited in the flood plains of River Ganga. These

sediments are of recent geological formation. The litho-units exposed within the river and

surrounding areas have formed as water borne sediments brought by flood water during rainy

season every year and deposited in river bed. The litho units encountered in the river bed and

surrounding areas belongs to the Shiwalik super groups. The size of the sediments towards the


source i.e. host rock is course and at the tail end of the river the grain size is reduced to smaller

sizes resulted in the formation of clay beds. The following sequences have been observed in the

area, i.e. Top soil/ Alluvium followed by sand deposition.

Sand and silt are deposited in the middle of the river whereas fine sand and soil are deposited at

the fringe of the riverbanks. Soil/ alluvium varying in thickness from 0.20m to 0.60m constitute

the top horizons in the area suitable for agriculture. River Ganga meanders through the area

exposing the alluvium and soil at the banks. Sand is found in the river bed up to a depth of more

than 3.0 m. The major part of bed remains dry as water flows in a single stream during the non-

monsoon seasons. Only during rainy seasons the entire flood plain has water, when there will be

no mining done.

(a) Details of river or stream and other sand source of the district

Sand is major mineral of Lakhisarai district of Bihar. Yellow sand in Kiul River is major sand

source and source of revenue collection in district. As well as soil / clay is actively mined for

bricks and pottery industry. In the financial year, huge amount of clay was produced for these

purposes. It is also used as a decorative material in landscaping. Specific types of sand are used in

the manufacture of glass and as a molding material for metal casting. Wide flood plains and high

banks are the common features in the course of the Ganga and the Kiul along with silt and clay

deposits. Stone is also a source of minor mineral in Lakhisarai district of Bihar.

The rivers of the district bring out the sediment as bed load and suspended load during the

monsoon period and post monsoon when the carrying capacity of river decreases it deposit the

sediment as braided deposit, point bars, etc. these are the main source of sand in the district.

(b) Availability of Sand or gravel or aggregate resources

Kiul River is major sand source and in district. The rivers of the district bring out the sediment as bed load and suspended load during the monsoon period and post monsoon when the carrying capacity of river decreases it deposit the sediment as braided deposit, point bars, etc. these are the main source of sand in the district. There is gravel or boulder or bajari is not found is the district.

(c) Existing Mining Lease of sand and aggregates

Refer to Chater-3


Drainage System with description of main rivers in

Total area of Lakhisarai district: 1301 sq.km.

Total area of drainage system with main rivers: 39.55sq.km.

S. No. Name of the River Area drained (Sq. Km) % Area drained in the District

1. Ganga 16 1.23% 2. Kiul River 18.5 1.42%

3. Bandar River 0.30 0.02%

4. Garkhe River 1.0 0.07%

5. Harohar River 3 0.23%

6. Some River 0.75 0.06%

Total 39.55 3.03%

Salient Features of Important Rivers and Streams

Total Area of Rivers in Lakhisarai District: -39.55 Sq.km.

S. No. Name of the River Total Length in the District

(in km)

Place of origin Altitude at

Origin

1. Ganga 4.5 km Jaitpur 41 m

2. Kiul River 59 km Kumadar 72 m

3. Bandar Nadi 4.7 km Chak Indupur 42 m

4. Garkhe Nadi 16.75 km Bherha 42 m

5. Harohar Nadi 35 km Pali 43m

6. Sone River 76.5 km Ballopur 53 m


River of Stream

Portion of the river or stream recommended for mineral concession ( in Sq. Km)

Length of area recommended for mineral concession (in Kilometer)

Average width of area recommended for mineral concession in meter)

Area recommended for mineral concession (In Square Meter)

Mineable Mineral Potential (In Metric Tonne) 60% of total Mineral

Ganga 16 Sq. Km 4.5 km 3555 m 159.97 Lakh Sq. m 440.57 Lakh MT

Kiul River 18.5 Sq. Km 59 km 314 m 185.26 Lakh Sq. m 510.20 Lakh MT

Bandar River 0.30 Sq. Km 4.7 km 63 m 2.96 Lakh Sq. m 8.15 Lakh MT

Garkhe River 1.0 Sq. Km 16.75 km 60 m 10.05 Lakh Sq. m 27.68 Lakh MT

Harohar River 3 Sq. Km 35 km 86 m 30.10 Lakh Sq. m 82.89 Lakh MT

Some River 0.75 Sq. Km 76.5 km 10 m 7.65 Lakh Sq. m 21.06 Lakh MT

TOTAL 196.45 Km 681 m. (Average)

395.99 Lakh Sq. m 1090.55 Lakh MT

Mineral Potential

Boulder (MT) Bajari (MT) Sand (MT) Total Minable Mineral

Potential (MT)

Not available Not available ~ 1091 Lakh MT ~ 1091 Lakh MT

Annual deposition

Annual deposition is calculated as 30 percent of total Minable Mineral potential in the district.

Details are as below-

Boulder (MT) Bajari (MT) Sand (MT) Total Minable Mineral

Potential (MT)

Not applicable Not applicable ~ 327 Lakh MT ~ 327 Lakh MT

Methodology Adopted for Calculating of Mineral Potential

The mineral potential is calculated based on field investigation and geology of the catchment area

of the river/ streams. As per the policy of the State and location, depth of minable mineral is

defined. The area for removal of mineral in a river or stream can be decided depending on geo-

morphology and other factors, it can be 50% to 60% of the area of a particular river/stream, e.g. in


river mineral constituents like sand up to a depth of three meters considered as resource mineral.

Other constituents like clay and silt are excluded as waste while calculating the mineral potential

of particular river/ stream.

The specific gravity of each mineral constituent is different. While calculating the mineral

potential, the average specific gravity is taken as 2.25. The percent of mineral constituent like

sand also varies for different river and streams. While calculating the mineral potential the

percentage of each mineral constituent is taken as Sand 25-30% and 5-10% for silt and clay.

The quantum of deposition varies from stream to stream depending upon factors like catchment

lithology, discharge, river profile and geomorphology of the river course. There are certaingeo-

morphological features developed in the river beds such as channel bar, point bar etc. where

annual deposition is more even two to three meters.


Chapter-12

BRICK KILNS IN BIHAR

The state of Bihar is developing rapidly. In the five year period from 2004 to 2009 Bihar’s Gross

Domestic Product (GDP) has grown by 11.03% and between 2001 and 2011 there has been a

significant increase in urbanization with the number of towns increasing from 120 to 213

according to the latest census. This has been possible through investment in various sectors,

especially the construction sector. If this growth rate needs to be sustained, the demand for quality

building materials will increase manifold. In rural areas too, Bihar faces challenges with the need

for over 7.5 billion bricks over the next five years to meet the rural housing gap. A field study was

conducted in 5 districts on Bihar to understand the present scenario of the brick industry and to

assess the market potential and barriers for introducing energy efficient technologies for walling

materials. The major brick producing districts of Bihar is Patna, Nalanda, Siwan, Muzaffarpur,

Sitamarhi, East and West Champaran, Darbhanga, Samastipur and Madhubani. With over 5,700

authorized brick kilns the state produces around 17 billion bricks per year. The brick sector in

Bihar is growing at a rate of 9%, however it continues to be dominated by traditional technology -

the Fixed Chimney Bulls Trench Kiln (FCBTK). Unlike the rest of India (except Punjab,

Haryana, Uttar Pradesh and West Bengal) the state of Bihar is the only state which has

transformed the brick firing technology from movable to fixed chimney.

Lists of Bricks Earth are attached -Annexure –II

Status of Brick Earth in Lakhisarai District

S No No of operational Units of Brick Earth in Lakhisarai

districts during Financial Year (2016-17)

No of Units of Brick Earth in Lakhisarai

district Identified by IEED

1 63 69


References

1. Singh, U,(1965):“Ditribution and Character of Cities of The Ganga Plain.”National

Geographical Journal of India,Vol.XI P.37

2. Optimum Utilisation of Surface Water and Ground Water Potential Using Fuzzy

Approach National Systems Conference, NSC 2008, 17–19 December 2008

3. http://www.censusindia.gov.in/2011-prov results/Census2011Bihar.pdf

4. Census of India 2011- Provisional Population Totals - Bihar - Data Sheet" (PDF).

Government of India, Ministry of Home Affairs, Vital Statistics Division. Office

of the Registrar General & Census Commissioner, India. 2011. pp. 1 & 2.

Retrieved 16 August 2012.

5. www.cgwb.gov.in/District_Profile/Bihar/Lakhisarai.pdf

6. cgwb.gov.in/gw profiles/st_Bihar.htm

7. www.cgwb.gov.in/Regions/GW-year.../GWYB%20MER%20(Bihar)%202015-

16.pdf

8. www.census2011.co.in › Bihar

9. http://www.cwc.nic.in

10. http://www.ecobrick.in

11. CLIMATE –DATA.ORG https://en.climate-data.org/location/24598/

***


Annexure-I SAND GHAT STATUS OF LAKHISARAI DISTRICT

SL. No.

Name of

River

Name of Sand Ghat

Area in Hect

s.

No. of Blocks

GPS Coordinates A B C D

1 KIUL Kishanpur Sand Ghat

23 Block - 1 25°11'55.99" 86°7'35.99"

25°11'47.94" 86°7'41.52"

25°11'34.78" 86°7'19.15"

25°11'42.71" 86°7'13.28"

2 KIUL Garhi Bishanpur Sand Ghat

24 Block - 1 25°11'19.89" 86°6'34.63

25°11'10.28" 86°6'41.09"

25°10'59.65" 86°6'19.34"

25°11'8.82" 86°6'12.90"

3 KIUL Birdaban Sand Ghat

18 Block - 1 25°10'4.80" 86°5'48.51"

25°10'7.74" 86°6'1.09"

25°9'54.42" 86°6'8.27"

25°9'49.69" 86°5'57.86"

4 KIUL Gurdih Sand Ghat

18.50

Block - 1 25°9'36.87" 86°6'10.67"

25°9'41.07" 86°6'18.22"

25°9'20.29" 86°6'33.05"

25°9'17.15" 86°6'24.30"

5 KIUL Ghosi Kundi Sand Ghat

22 Block - 1 25°9'2.04" 86°6'30.86"

25°9'3.97" 86°6'40.21"

25°8'35.72" 86°6'38.29"

25°8'35.00" 86°6'29.27"

6 KIUL Khairi Sand Ghat

21 Block - 1 25°8'17.16" 86°6'24.99"

25°8'19.01" 86°6'35.94"

25°8'6.19" 86°6'49.52"

25°7'57.33" 86°6'43.97"

7 KIUL Mahisona Sand Ghat

23 Block - 1 25°7'49.14" 86°7'0.63"

25°7'57.73" 86°7'5.20"

25°7'39.39" 86°7'32.95"

25°7'33.77" 86°7'27.83"

8 KIUL Khutupar & Banshipur sand Ghat

235 Block - 1 25°7'21.51" 86°7'42.85"

25°7'24.55" 86°7'47.57"

25°6'57.88" 86°8'15.84"

25°6'52.71" 86°8'9.27"

9 KIUL Jhinaura Sand Ghat

20 Block - 1 25°6'39.89" 86°8'22.96"

25°6'44.21" 86°8'30.13"

25°6'21.34" 86°8'40.20"

25°6'20.43" 86°8'27.56"

10 KIUL Maliya Sand Ghat

24.50

Block - 1 25°5'32.94" 86°8'15.23"

25°5'28.88" 86°8'24.54"

25°5'5.08" 86°8'10.86"

25°5'10.13" 86°8'1.44"

11 KIUL Sharma Sand Ghat

22 Block - 1 25°5'34.10" 86°7'38.37"

25°5'31.03" 86°7'52.07"

25°5'15.19" 86°7'37.97"

25°5'19.86" 86°7'25.23"

12 KIUL Tetarhat Sand Ghat

21.50

Block - 1 25°4'56.34" 86°7'30.98"

25°4'59.36" 86°7'45.94"

25°4'44.84" 86°7'53.34"

25°4'41.69" 86°7'37.91"

13 KIUL Nagardar Sand Ghat

23.50

Block - 1 25°4'39.35" 86°8'20.13"

25°4'46.77" 86°8'24.34"

25°4'38.50" 86°8'49.37"

25°4'29.60" 86°8'42.12"

14 KIUL Rampur Sand Ghat

23.50

Block - 1 25°4'14.47" 86°8'52.79"

25°4'17.63" 86°9'0.40"

25°4'2.66" 86°9'18.22"

25°3'56.56" 86°9'1.71"

15 KIUL Nongarh Sand Ghat

23.50

Block - 1 25°3'25.33" 86°9'2.45"

25°3'30.83" 86°9'8.16"

25°3'15.37" 86°9'32.68"

25°3'7.01" 86°9'24.64"

16 KIUL Kumadar Sand Ghat

22 Block - 1 25°2'49.53" 86°9'31.93"

25°3'8.49" 86°9'52.18"

25°2'43.80" 86°9'39.10"

25°3'3.05" 86°9'59.71"

17 KIUL Moliya Sand Ghat

2 Block - 1 25°5'9.921" 86°7'46.689"

25°5'12.708" 86°7'46.807"

25°5'12.509" 86°7'51.871"

25°5'7.965" 86°7'52.920"

18 KIUL Nagardar 1 Sand Ghat

4.22 Block - 1 25°04'25.35" 86°08'54.15"

25°04'28.02" 86°09'00.08"

25°04'34.84" 86°08'53.74"

25°04'30.01" 86°08'49.64"


19 KIUL Rampur - 1 Sand Ghat

2.43 Block - 1 25°04'22.90" 86°08'53.56"

25°04'18.54" 86°08'56.32"

25°04'20.69" 86°08'00.15"

25°04'25.98" 86°08'59.68"

20 KIUL Dumrahi Sand Ghat

4 Block - 1 25°5'41.864" 86°8'12.188"

25°5'47.685" 86°8'23.566"

25°5'40.610" 86°8'21.709"

25°5'38.536" 86°8'16.124"

21 KIUL Takari Mountain Sand Ghat

3 Block - 1 25°2'8.441" 86°10'34.939"

25°2'10.108" 86°10'37.106"

25°2'2.556" 86°10'45.667"

25°2'0.172" 86°10'43.248"

22 KIUL Takari Lakhapur Sand Ghat

24.9 Block - 1 25°1'39.600" 86°11'37.658"

25°1'34.200" 86°11'34.872"

25°1'48.518" 86°10'56.792"

25°1'54.470" 86°11'2.043"

23 KIUL Sharma Sand Ghat

24.9 Block - 1 25°6'7.543" 86°8'30.831"

25°6'9.298" 86°8'43.739"

25°5'48.618" 86°8'19.025"

25°5'44.959" 86°8'31.952"

24 KIUL Jhinaura 1 Sand Ghat

4.74 Block - 1 25°6'16.467" 86°8'24.693"

25°6'17.091" 86°8'40.871

25°6'13.689" 86°8'40.900"

25°6'12.883" 86°8'24.732"

25 KIUL Kishanpur 1 Sand Ghat

3.88 Block - 1 25°11'28.881" 86°6'55.810"

25°11'33.554" 86°6'56.609"

25°11'26.040" 86°7'5.424"

25°11'23.813" 86°7'0.953"

Annexure-II List of Bricks Kilns Under Lakhisarai District

S. N

Name of M/s Name of Proprietor Running or close

Address /close / Mauja Mark / Grade

Khata& Khesra

No.of soil cutting

area

Khata &Khesra

No. of bricks kline area

Latitude (N)

Longitude (E)

1 M/s Shiva Bricks

Mr. Sunil Singh Running Mauja:- Govind Bigha Vill:- Govind Bigha Block:- Lakhisarai Dist:- Lakhisarai Mo:-7870321611

555/A Khata No: Khata No: 25.199085 86.092351 25.199312 86.092426 25.199335 86.092241

ESTD.YEAR- 2013

Khesra No: Khesra No:

25.198881 86.092157 25.198827 86.092357

2 M/s Bajrangbali Bricks

Mr. Panveshvar Sah Running Mauja:- Govind Bigha Vill:- Balgudar Block:- Lakhisarai Dist:- Lakhisarai Mo:-8292485684

BBM/A Khata No: Khata No: 25.200203 86.089918 25.200002 86.090037 25.200093 86.090152

ESTD.YEAR- 1990


25.200440 86.089940 25.200374 86.089787

3 M/s ABP Bricks Mr. Satendra Dev+BaBlu kumar

Running Mauja:- Balgudar Vill:- Balgudar Block:- Lakhisarai Dist:- Lakhisarai Mo:-9504180568

ABP/A Khata No: Khata No: 25.202832 86.088544 25.202946 86.088726 25.202766 86.088751

ESTD.YEAR- 2013


25.202782 86.088296 25.202932 86.088271

4 M/s BMP Bricks Mr. Niwas Singh Running Mauja:-Kashva Vill:- Balgudar Block:- Lakhisarai Dist:- Lakhisarai Mo:-8271517684

BMP/A Khata No: Khata No: 25.205268 86.087795 25.205477 86.087770 25.205487 86.087628

ESTD.YEAR-1995


25.205045 86.087673 25.205056 86.087854

5 M/s Tata Bricks Mr. Om Prakash Singh

Running Mauja:-Balgudar Vill:- Balgudar Block:- Lakhisarai Dist:- Lakhisarai

TATA/C Khata No: Khata No: 25.209909 86.085292 25.210074 86.085349 25.210129 86.085221

ESTD.YEAR- Khesra No: Khesra 25.209730 86.085127

District Survey Report - Lakhisarai

2012 Mo:-7301180082 No:6 M/s Pawan

Bricks Mr. Mani Kant Singh Running Mauja:- Jaitpur

Vill:- Barhiya Block:- Lakhisarai Dist:- Lakhisarai Mo:-9570528188

PAWAN/C

Khata No: Khata No: 288

ESTD.YEAR-2010

Khesra No: 2119,2120

7 M/s Shivam Bricks

Mr. Bablu Singh Running Mauja:- Jaitpur Vill:- Jaitpur Block:- Lakhisarai Dist:-Lakhisarai Mo:-9631017957

SHIVAM/C

Khata No: 18,12

ESTD.YEAR- 2010

Khesra No: 130,133,132,134

8 M/s Sagar Bricks

Mr. Surendra Singh Close/ 2017

Mauja:- Tirasi Vill:-Barhiya Block:- Barhiya Dist:-Lakhisarai Mo:-

SAGAR Khata No: Khata No:

ESTD.YEAR- Khesra No: Khesra No:

9 M/s JMG Bricks Mr. Radheshyam Singh New-Navin kumar

Running Mauja:- Gangasarai Vill:- Gangasarai Block:- Barhiya Dist:- Lakhisarai Mo:-8877612221

JMG/C Khata No: Khata No:

ESTD.YEAR-2013


10 M/s KBI Bricks Mr. Raushan kumar Running Mauja:- Barhiya Vill:- Barhiya Block:- Barhiya Dist:- Lakhisarai Mo:-9204449439

RBI/C Khata No: Khata No:

ESTD.YEAR- 2012


11 M/s BBC Bricks Mr. Ranjit kumar Running Mauja:- Govind Bigha Vill:- Govind Bigha Block:- Lakhisarai Dist:-Lakhisarai Mo:-9135599370

BBC/C Khata No: Khata No:

ESTD.YEAR- 2014


12 M/s Shiva Bricks

Mr. Sanjay Singh Close/ 2017

Mauja:- Lakhsmipur Vill:- Lakhsmipur Block:- Lakhisarai Dist:- Lakhisarai

SHIVA/C

Khata No: Khata No:

ESTD.YEAR- Khesra No: Khesra


Mo:- No:13 M/s ABC Bricks Mr. Sanjay kumar Running Mauja:- Gadh

Vill:- Lakhsmipur Block:- Lakhisarai Dist:- Lakhisarai Mo:-

ABC/C Khata No: Khata No:


14 M/s A to Z Bricks

Mr. Vijay Singh Running Mauja:-Khurha Vill:- Barhiya Block:- Lakhisarai Dist:- Lakhisarai Mo:-9525180972

A to Z/C Khata No: Khata No:834,4048

ESTD.YEAR- 2017


15 M/s JMG Bricks Mr. Kanhaiya Singh Close/2014

Mauja:- Malpur Vill:- Barhiya Block:- Lakhisarai Dist:-Lakhisarai Mo:-9472166272

JMB/C Khata No: Khata No:

ESTD.YEAR- 2014


16 M/s Maa Bricks Mr. Shashi Shekhar Singh

Close this Year No

Start again

Mauja:- Nandnana Vill:-Ramgadh Block:-Ramgadh Dist:-Lakhisarai Mo:-9939590719

MAA/C Khata No: Khata No:

ESTD.YEAR- 2000


17 M/s ABC Bricks Mr. kamal Kishor Singh

Close/2014

Mauja:- Nandnana Vill:-Ramgadh Block:-Ramgadh Dist:- Lakhisarai Mo:-

ABC Khata No: Khata No:


18 M/s Kishan Bricks

Mr. Ram Prakash Singh

Running Mauja:- Nandnana Vill:-Ramgadh Block:-Ramgadh Dist:- Lakhisarai Mo:-8294206552

KISHAN/C

Khata No: Khata No:

ESTD.YEAR- 2008



19 M/s Ganga Bricks

Mr. Chandan Singh Close/2 Years

Mauja:- Nandnana Vill:- Ramgadh Block:- Ramgadh Chand Dist:- Lakhisarai Mo:-

GANGA/C

Khata No: Khata No:


20 M/s LPS Bricks Mr. Anjani kumar Singh

Close/10 years

Mauja:- Sondhi Vill:- Ramgadh Chand Block:- Rangadh Dist:-Lakhisarai Mo:-

LPS Khata No: Khata No:


21 M/s JBS Bricks Mr. 4 Patner Close /dead

Mauja:- Sharmar Vill:- Ramgadh Block:- Ramgadh Dist:-Lakhisarai Mo:-

JBS Khata No: Khata No:

ESTD.YEAR- 2016


22 M/s Taj Bricks Mr. Nilesh kumar Running Mauja:- Sharma Vill:- Sharma Block:-Ramgadh Dist:- Lakhisarai Mo:-

TAJ/C Khata No: Khata No:

ESTD.YEAR- 2013


23 M/s BTS Bricks Mr. Randhir kumar Running Mauja:- Sharma Vill:- Sharma Block:- Ramgadh Dist:- Lakhisarai Mo:-7250808159

BTS/C Khata No: Khata No:

ESTD.YEAR- 2012


24 M/s JDM Bricks Mr. Rajesh Yadav Running Mauja:- Tetarhar Vill:- Halasi Block:-Ramgadh Dist:- Lakhisarai Mo:-9771929939

JDM/C Khata No: Khata No:

ESTD.YEAR-2013



25 M/s MBM Bricks

Mr. Samshudhin Ansari

Running Mauja:- Tetarhar Vill:- Halasi Block:-Ramgadh Dist:- Lakhisarai Mo:-9852034957

MBM/C Khata No: Khata No:


26 M/s Milan Bricks

Mr. Sadanand Singh Running Mauja:-Satyabj Vill:- Ramgadh Block:-Ramgadh Dist:- Lakhisarai Mo:-8676045401

MILAN/C

Khata No: Khata No:

ESTD.YEAR-2018


27 M/s Sriram Bricks

Mr. Bulbul Singh Close/5Years

Mauja:- Bahrama Vill:- Halasi Block:- Halasi Dist:-Lakhisarai Mo:-

SHREERAM+APNA/C

Khata No: Khata No:


28 M/s BKS Bricks Mr. Vikas kumar Singh

Running Mauja:- Konaga Vill:- Konaga Block:- Halasi Dist:-Lakhisarai Mo:-9931692300

BKS/C Khata No: Khata No:

ESTD.YEAR- 2018


29 M/s STM Bricks Mr. Rananuj Singh Running Mauja:-Maharat Vill:-Maharat Block:- Halasi Dist:- Lakhisarai Mo:-8521529702

STM/C Khata No: Khata No:44

ESTD.YEAR- 2012

Khesra No: Khesra No:416

30 M/s Satyam Bricks

Mr. Pramod Singh Close/3 year

Mauja:- Maharat Vill:- Halasi Block:-Halasi Dist:- Lakhisarai

STM/ Khata No: Khata No:



2015 Mo:-9771337256 No:

31 M/s BSN Bricks Mr. Vijaykumar Singh

Running Mauja:- Matasi Vill:- Matasi Block:-Halasi Dist:-Lakhisarai Mo:-9934734359

BSN/C Khata No: Khata No:

ESTD.YEAR- 2012


32 M/s Sivendra kumar Singh

Mr. Sivendra kumar Running Mauja:- Pipra Vill:- Pipra Block:- Halasi Dist:- Lakhisarai Mo:-9631580251

SPL/C Khata No: Khata No:

ESTD.YEAR- 2011


33 M/s Shivam Bricks

Mr. Shailendar Singh Close / 5 years

Mauja:- Tarhari Vill:- Tarhari Block:-Halasi Dist:-Lakhisarai Mo:-

SHIVAM/C

Khata No: Khata No:

ESTD.YEAR- 2000


34 M/s Raj Bricks Mr. Bablu Singh Running Mauja:- ouro Vill:- Ramgadh Block:- Ramgadh Dist:- Lakhisarai Mo:-9631017957

RAJ/C Khata No: Khata No:

ESTD.YEAR- 2017


35 M/s Sriram Bricks

Mr. Hari Kant Singh Running Mauja:-ouro Vill:-Ramgadh Block:- Ramgadh Dist:- Lakhisarai Mo:-9973407973

SR/C Khata No: Khata No:


36 M/s Sum Bricks Mr. Pankaj kumar Running Mauja:- Chandanpura Vill:-Chandanpura Block:- Suryagdha

SUM/C Khata No: Khata No:161


ESTD.YEAR- 1998

Dist:- Lakhisarai Mo:-9939659814


37 M/s Om Bricks Mr. Sanjay Yadav Running Mauja:- chandanpura Vill:-chandanpura Block:-Suryagdha Dist:- Lakhisarai Mo:-8936072654

OMB/C Khata No: Khata No:

ESTD.YEAR- 2000


38 M/s HHM Bricks

Mr. Anandi Yadav Running Mauja:- Chananiya Vill:- Chananiya Block:-Suryagdha Dist:-Lakhisarai Mo:-9939417657

HHM/C Khata No: Khata No:

ESTD.YEAR- 2012


39 M/s SSS Bricks Mr. Sudhir kumar Singh

Close/2year

Mauja:-Mahamadpur Vill:- Mahamadpur Block:- Suryagdha Dist:- Lakhisarai Mo:-

SSS/C Khata No: Khata No:

ESTD.YEAR- 2010


40 M/s JMK Bricks Mr. Ramaudan kumar Yadav

Running Mauja:- Ratanupur Vill:-Ratanupur Block:- Suryagdha Dist:- Lakhisarai Mo:-9852757353

JMC/C Khata No: Khata No:

ESTD.YEAR-2013-14


41 M/s JMS Bricks Mr. Manoj kumar Running Mauja:- Aadupur Vill:- Aadupur Block:- Suryagdha Dist:- Lakhisarai Mo:-9852310271

JMS/C Khata No: Khata No:41,74,07,24

ESTD.YEAR- 2016

Khesra No: Khesra No:111,112

42 M/s JBS Bricks Mr. Uday kumar Running Mauja:- Aadupur Vill:- Aadupur

JBS/C Khata No: Khata No:


Block:- Suryagdha Dist:-Lakhisarai Mo:-9939094583


43 M/s JBB Bricks Mr. Nand Kishor Prasad Rai

Running Mauja:-Aadupur Vill:- Aadupur Block:- Suryagdha Dist:- Lakhisarai Mo:-9097013073

JBB/C Khata No: Khata No:

ESTD.YEAR-2012


44 M/s JMB Bricks Mr. Sikendra Yadav Running Mauja:- Aadupur Vill:- Aadupur Block:- Suryagdha Dist:- Lakhisarai Mo:-9934757672


ESTD.YEAR- 2014


45 M/s Aman Bricks

Mr. Kumari Nirupam Running Mauja:- Khemtarni Vill:- Khemtarni Block:-Suryagdha Dist:- Lakhisarai Mo:-9934705997

JMD/C Khata No: Khata No:

ESTD.YEAR- 2000


46 M/s Mohan Bricks

Mr. Mohan Yadav Running Mauja:- Vikrampur Vill:- Vikrampur Block:- Suryagdha Dist:- Lakhisarai Mo:-8084067199

CHK/C Khata No: Khata No:

ESTD.YEAR- 1998


47 M/s SSV Bricks Mr. Anil kumar Verma

Running Mauja:-Chandanpura Vill:- Chandanpura Block:- Suryagdha Dist:- Lakhisarai Mo:-9430237029

SSV/C Khata No: Khata No:

ESTD.YEAR-2015


48 M/s Raj Bricks Mr. Rajiv Nayan Running Mauja:- Sherpur RAJ/C Khata No: Khata No:


Singh Vill:-Sherpur Block:- Suryagdha Dist:- Lakhisarai Mo:-9852468371

ESTD.YEAR- 1999


49 M/s RKS Bricks Mr. Vikram kumar Singh

Running Mauja:- Salempur Vill:- Salempur Block:-Suryagdha Dist:-Lakhisarai Mo:-9934705453

RKS/C Khata No: Khata No:

ESTD.YEAR- 2015


50 M/s JBG Bricks Mr. Mithilesh kumar Singh

Running Mauja:- Avagil Vill:- Avagil Block:- Medani Chouki Dist:- Lakhisarai Mo:-9931091488

JBG/C Khata No: Khata No:

ESTD.YEAR- 2000


51 M/s JBM Bricks Mr. Dinesh Yadav Running Mauja:- Avagil Vill:-Rampur Block:- Medani Chouki Dist:- Sheikhpura Mo:-9931425998


ESTD.YEAR-2010


52 M/s SDJ Bricks Mr. Aswani kumar Jalan

Running Mauja:- Makasampur Vill:- Makasampur Block:- Medani Chouk Dist:- Lakhisarai Mo:-9931696478

SDJ/C Khata No: Khata No:

ESTD.YEAR- 2008


53 M/s BMJ Bricks Mr. Sri Veerendra Running Mauja:-Makasampur Vill:- Makasampur Block:- Medani Chouk Dist:- Lakhisarai Mo:-9852565544

BMJ/C Khata No: Khata No:



54 M/s BPM Bricks Mr. Vijay PD Mahto Running Mauja:- Slarpur Vill:-Slarpur Block:- Medani Chouk Dist:- Lakhisarai Mo:-9534775502

BPM/C Khata No: Khata No:

ESTD.YEAR- 2013


55 M/s NKJ Bricks Mr. Pawan kumar Jalan

Running Mauja:- Nanakpur Vill:- Devgra Block:- Medani Chouk Dist:- Lakhisarai Mo:-9931859937

NKJ/C Khata No: Khata No:

ESTD.YEAR- 2008


56 M/s Raja Bricks Mr. Jyotish kumar Running Mauja:- Nanakpur Vill:- Nanakpur Block:- Medani Chouk Dist:- Lakhisarai Mo:-9006621200

RAJA/C Khata No: Khata No: 522,547,510,50

ESTD.YEAR- 2011

Khesra No: Khesra No: 1026,1039,1053,1052

57 M/s JBGS Bricks

Mr. Prem kumar Gautam

Running Mauja:- Karehar Vill:- Karehar Block:- Suryagadh Dist:- Lakhisarai Mo:-9934696738

JBGS/C Khata No: Khata No:

ESTD.YEAR- 2014


58 M/s JMT Bricks Mr. Munna kumar Running Mauja:- Karehar Vill:- Karehar Block:- Suryagadh Dist:- Lakhisarai Mo:-9031832218

JMT/C Khata No: Khata No:

ESTD.YEAR- 2015


59 M/s JMV Bricks Mr. Sanjay kumar Running Mauja:- Karehar Vill:- Karehar Block:- Suryagadh Dist:- Lakhisarai

JMV/C Khata No: Khata No: 49,130,130,76



2014 Mo:-9931846484 No: 356,357,331,358,331

60 M/s BPR Bricks Mr. Vanvari Prasad Rai

Running Mauja:- Karehar Vill:- Karehar Block:- Suryagadh Dist:- Lakhisarai Mo:-9006590259

BPR/C Khata No: Khata No:

ESTD.YEAR-2014


61 M/s GPR Bricks Mr. Gopal Prasad Rai

Running Mauja:- Patelpur Vill:- Patelpur Block:- Suryagadh Dist:- Lakhisarai Mo:-9931649749

GPR/C Khata No: Khata No: 294,293,209

ESTD.YEAR- 2011

Khesra No: Khesra No:215,214,209

62 M/s JJB Bricks Mr. Sujit kumar Singh

Close/ Start Again

Mauja:- Harpur Vill:Harpur Block:- Suryagadh Dist:- Lakhisarai Mo:-8409864633

JJB/C Khata No: Khata No:

ESTD.YEAR-2011


63 M/s Pawan Bricks

Mr. Arun Singh Running Mauja:- Balipur Vill:- Pipariya Block:-Pipariya Dist:- Lakhisarai Mo:-9473042338

PAWAN/C

Khata No: Khata No:

ESTD.YEAR- 2014


64 M/s Panchamukhi Bricks

Mr. Santosh yadav Running Mauja:- Manpur Vill:- Kharkuaa Block:- Chanan Dist:- Lakhisarai Mo:-7349915040

PMC/B Khata No: Khata No:03

ESTD.YEAR- 2017


65 M/s JKM Bricks Mr. Krishna Murari yadav

Close/1ye

Mauja:- wasubhachak Vill:- wasubhachak

JKM/B Khata No: Khata No:


ars Block:- Chanan Dist:- Lakhisarai Mo:-9006199708

ESTD.YEAR- 2017


66 M/s SVR Bricks Mr. Subodh kumar Running Mauja:- Revta Vill:- Revta Block:- Chanan Dist:- Lakhisarai Mo:-

SVR/C Khata No: Khata No:

ESTD.YEAR-2017


67 M/s IBN Bricks Mr. Indradev Rawat Running Mauja:- Kundar Vill:- Kundar Block:- Chanan Dist:- Lakhisarai Mo:-9939654679

INB/C Khata No: Khata No:

ESTD.YEAR- 2015


68 M/s RKS Bricks Mr. Rabindra kumar Singh

Running Mauja:- Kundar Vill:- Kundar Block:- Chanan Dist:- Lakhisarai Mo:-9939654679

RKS/C Khata No: Khata No:

ESTD.YEAR- 2017


69 M/s SDY Bricks Mr. Dilip Yadav Running Mauja:- Bis Hjari Vill:- Nongadh Block:- Halasi Dist:- Lakhisarai Mo:-9771703171

SDY/C Khata No: Khata No:

ESTD.YEAR- 2012

Khesra No:

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