Khandwa

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Author: Laxman Burdak IFS (R)
For another villages of same name see - Khandwa Niwai/Khandwa Churu/Khandwa Sehore
Map of Khandwa & Burhanpur district
Khandwa-Abna River-Sukta River-Jaswadi in Khandwa, MP
Khandwa-Titgaon-Bhakarada in Khandwa, MP

Khandwa (खंडवा) is a city and district in Madhya Pradesh. Formerly it was called East Nimar. It is located on Abna River. Burhanpur District was created on August 15, 2003, from the southern portion of Khandwa District.

Variants

Origin of name

  • The name of the city is derived from Khandavavana (खांडववन), which literally means Khandav Forests.
  • To trace the origin of the name of the present District it is necessary first to find out the origin of the name Prant Nimar from which obviously most of the present District is carved. Nothing definite is known about the latter but it may be guessed that the old Prant Nimar was so called, because a place called Nimawar on the Narmada (now in Dewas District), was the capital of Prant Nimar. Nimawar is also mentioned by the famous Arab writer Alberuni, as Namavur[1]. The name Nimar happens to be spelt in certain books as Nimaur.[2] In course of time and by stages Nimawar, Namavur or Nimaur may have assumed the simple form, Nimar. As most of the territorial divisions derive their names from some one place of importance in the region, and as Nimawar was such a place of religion and administrative importance in the region,[3] the old Prant Nimar was called after that name, and the present Nimar District carved out of it retained the same.[4]
  • The name is supposed to be derived from nim, half, as Nimar was supposed to be half-way down the course of the Narmada, but in reality it is much nearer the mouth than the source of the river.[5]
  • Another derivation suggested is from the nim tree which is noticeably common in the District” [6] . [7]

Location

Khandwa is a major railway junction; the Malwa line connecting Indore with the Deccan meets the main east–west line from Mumbai to Kolkata.

The Town Khandwa has the proud to be the Head Quarter of District East Nimar. Due to its location on the map of India, it has been enjoying visits of great Indians. In the past (age of British Government), this was a place alone connecting northern, eastern, southern and western rail routes. Delhi (North) and Bombay (South) and Baroda (West) was directly connected whereas Calcutta was accessible through [[Bhusawal Junction.

Swami Dayananda Saraswati, Swami Vivekananda, Mahatma Gandhi, Lokmanya Tilak and many more great personalities visited the place during there all India visit. The Location, easy availability of resources and other socio-economic factors are in favour of making the place a very good Industrial region.The place has several ancient kunds., English architecture and religious places.

The place is located at Bombay-Delhi central line and north of Burhanpur. The place has been the district Head quarter since 1864. The place has four historic kunds in its four direction namely Suraj kunda, Padma kund, Bhima kunda, Rameshwar kund. The buildings of Collector office, Girls Degree College, Ghantaghar are Among the ancient monuments. Dada Dhuni wale ki samadhi, Turja Bhavani Temple, Nav-chandi Devi Dham are the places of faith & worship of Hindus.

Source - https://khandwa.nic.in/en/tourist-place/khandwa-town/

Geography

Khandwa District lies in the Nimar region, which includes the lower valley of the Narmada River. The Narmada forms part of the northern boundary of the district, and the Satpura Range form the southern boundary of the district. Burhanpur District, to the south, lies in the basin of the Tapti River. The pass through the Satpuras connecting Khandwa and Burhanpur is one of the main routes connecting northern and southern India, and the fortress of Asirgarh, which commands the pass, is known as the "Key to the Deccan". Betul and Harda districts lie to the east, Dewas District to the north, and Khargone District to the west.

Rivers

Jat Gotras

Jat Gotras Namesake

  • Asi (असि) (Jat clan) → Asinder = Narmada Nagar. Narmada Nagar is a small town, established in around 1985, by Narmada Valley Development Authority and afterwards by Narmada Hydroelectric Development Corporation. It was earlier known as Asinder, after the king of Punasa, a neighboring town.

Tahsils in Khandwa District

Villages in Khandwa tahsil

Town :1. Khandwa

Villages:

1 Ahmadpur, 2 Ajanti, 3 Amalpura, 4 Ambapat, 5 Amlani, 6 Amoda, 7 Atoot Bhikari, 8 Attar, 9 Awaliya Vithal, 10 Badgaon Bhila, 11 Badgaon Gujar, 12 Badgaon Mal, 13 Badgaon Mali, 14 Badgaon Piplod, 15 Badiya Tula, 16 Baidiya Khurd, 17 Baidiyaw, 18 Baldua Dongri, 19 Baliyapura, 20 Balkhand Sura, 21 Balwada, 22 Bamanda Ryt, 23 Bamangaon, 24 Bamangaon Bhila, 25 Bamjhar, 26 Banjari, 27 Barar, 28 Barud, 29 Bawadiyakajee, 30 Benpura Kurwada, 31 Bhagaiyapur, 32 Bhagwanpura, 33 Bhaisawan, 34 Bhakarada, 35 Bhamgarh Nazul, 36 Bhandariya, 37 Bhawsinghpura, 38 Bhelkhedi, 39 Bhigawan Nankari, 40 Bhil Khedi Murar, 41 Bhilai Kheda, 42 Bhojakhedi, 43 Bhuifal, 44 Bhutni Ryt, 45 Bihar, 46 Bijora Bhil, 47 Bilan Kheda, 48 Birpur Kundeshwar, 49 Bisrampur Ryt, 50 Bodul, 51 Borgaon Khurd, 52 Borkheda Kalan, 53 Borkheda Khurd Ryt, 54 Chandpur Ryt, 55 Charkheda, 56 Chhaigaon Devi, 57 Chhaigaon Makhan, 58 Chhanera, 59 Chhirbel, 60 Chhirwan Ryt, 61 Chich Kheda, 62 Chichgohan, 63 Chichli Buzurg, 64 Dagadiya, 65 Deepla, 66 Dehariya, 67 Delgaon, 68 Deola Mafi, 69 Deshgaon, 70 Dewla Mafi, 71 Dhangaon, 72 Dhangaon, 73 Dhanora, 74 Dharampuri, 75 Dhodwada, 76 Dhorani, 77 Digarish, 78 Dodwada, 79 Domwada, 80 Dongargaon, 81 Dugwada, 82 Fatepur Mundi, 83 Fathehpur, 84 Fulgaon, 85 Gajwada, 86 Gandhwa, 87 Garangaon, 88 Gohlari, 89 Gokulgaon, 90 Golkheda Ryt, 91 Gondwadi, 92 Gondwadi Ryt, 93 Gudikheda Ryt, 94 Gujrikheda Ryt, 95 Haidarpur, 96 Handiakheda Ryt, 97 Hapla, 98 Haraswada, 99 Heerapur, 100 Hirapur Ryt, 101 Itwa Ryt, 102 Itwamal, 103 Jagatpura, 104 Jalkuwa, 105 Jamli Mundi, 106 Jamli Sayad, 107 Jamniya, 108 Jaswadi, 109 Jawar, 110 Jheeraniya, 111 Jinwaniya, 112 Jirwan, 113 Kahalari, 114 Kaldakhedi, 115 Kalmukhi, 116 Kalpat, 117 Kamaliya, 118 Kankariya, 119 Kanwani, 120 Karpur Ryt, 121 Kaweshwar, 122 Kedarkhedi, 123 Kesoon, 124 Khajuri, 125 Kharkali, 126 Khedi Kitta, 127 Khidgaon, 128 Khutpal, 129 Kirgaon, 130 Kithiya Joshi, 131 Kohadad, 132 Kolgaon, 133 Korgala, 134 Kotwada, 135 Kumtha, 136 Lachhora Khurd, 137 Lachhorakalan, 138 Ladanpur, 139 Lakhangaon, 140 Lalwada, 141 Lohari, 142 Lunhar Ryt, 143 Machhoundi Ryt, 144 Malgaon, 145 Manpura, 146 Mathani Buzurg, 147 Mathani Khurd Ryt, 148 Mathela, 149 Matpur, 150 Moghat, 151 Mordad, 152 Mundwada, 153 Nagchoon, 154 Nahalda, 155 Nahar Mal, 156 Nandiya, 157 Nawali, 158 Pachhaha, 159 Padlya, 160 Palasi, 161 Palkana, 162 Panchbedi Ryt, 163 Pangra, 164 Panjhariya, 165 Parethi, 166 Pipalkota, 167 Piplod Khas, 168 Piplya Kalan, 169 Piplya Khurd Ryt, 170 Piplya Punasa, 171 Piplya Tahar, 172 Piplyafool, 173 Pokhar Kalan, 174 Puranpura Mal, 175 Puranpura Ryt, 176 Rahemapur, 177 Raikhutwal, 178 Rajgarh, 179 Rampurakalan, 180 Rampuri Ryt, 181 Rangaon, 182 Ranjani Ryt, 183 Rewada, 184 Rijgaon, 185 Rohani, 186 Rohnai, 187 Roshiya, 188 Roshnai, 189 Rudhy, 190 Sahejala, 191 Sahejalakhandwa, 192 Sali Ryt, 193 Sarai, 194 Saray, 195 Satwada, 196 Sawkheda, 197 Semalya Ryt, 198 Sihada, 199 Singot, 200 Sirpur, 201 Sirra, 202 Sirsod, 203 Siwana, 204 Sonud, 205 Sulyakhedi, 206 Sunderbel, 207 Surgaon Banjari, 208 Surgaon Joshi, 209 Surgaon Nipani, 210 Surgaon Rathor, 211 Sutarkheda Ryt, 212 Takali Mori, 213 Takalkheda Ryt, 214 Talwadiya, 215 Talwadiya, 216 Teerandajpur, 217 Tembhikalan, 218 Tighariya, 219 Titgaon, 220 Tokar Kheda, 221 Torani,

Source - https://www.census2011.co.in/data/subdistrict/3716-khandwa-east-nimar-madhya-pradesh.html

Archaeology

Source - East Nimar District Gazeteer by P N Shrivastav, 1969, p.37

Recent explorations in the beds of the Agni, Kundala, Machikunda, Chhota Tawa, Samdeni, Ruprel and Ghorapachhar, all tributaries of the Narmada, have revealed traces of the Palaeolithic men in East Nimar District.1 Palaeolithic tools have been discovered at Bijalpur, Barakund, Mahalkheri, Matupur and other places in Harsud tahsil. Microliths, consisting of blades, lunates, crescents and scrapers, and fluted cores have also been discovered in the above mentioned river valleys at Punaghat-Kala, Borkheda-Khurd, Peeplya-Bawli, Roshini and a large number of other villages in Harsud tahsil and at Dehgaon, Hutiya, Atud Khasa, Ratanpur, Nandh-kheda and other places, in Khandwa tahsil.2 Further explorations in East Nimar and adjoining district confirm the three-cycle hypothesis of De Terra and Patterson, the sequence of deposits being: Large-sized pebble-gravel, red sandy clay and the midium-sized pebble-gravel containing Middle Stone Age tools with fossils; finer gravel with thin flake-blade and scraper industry; and alluvium. 3

Lately, a proto-historic site, situated on the Tapti, 5 miles south-west of Burhanpur, has, in addition to microliths, yielded red-ware with black painting, black and red and red-slipped wares, grey-ware with light-cream slip and dull grey ware.

1. Indian Archaeology—A Review, 1958-59, p. 28; 1959-60, p. 69; 1960-61, p. 61.

2. Ibid.

3. Ibid, 1962-63, p. 10.

History

Ancient history: Recent explorations in the beds/tributaries of Narmada have revealed traces of the Paleolithic men in the East Nimar district. Omkar Mandhata, a rocky island on the bank of the Narmada river, about 47 miles north-west of Khandwa, is said to have been conquered by the Haihaya king Mahishmant, who had named the same as Mahishmati.[8]

During the rise of Buddhism, the East Nimar region was included in the Avanti Kingdom under Chandapradyota Mahesana, which was later added to the growing empire of Magadha by Shishunaga.

From the early 2nd century BCE to late 15th century CE, the Nimar Region (earlier a part of Khandesh) was ruled by many dynasties, which include Mauryas, Shungas, Early Satvahanas, Kardamakas, and Abhiras (Ahir Gavli).[9] Vakatakas, Imperial Guptas, Kalachuris,[10] Vardhanas (of Harsha Vardhana fame), Chalukyas, Rashtrakutas, Paramaras, Faruki Dynasty.[11]

Modern History

Source - East Nimar District Gazeteer by P N Shrivastav, 1969, p.i

East Nimar is one of the most important districts of Madhya Pradesh. It has a rich historical past. The District bears traces of Palaeolithic man and microlithic objects. Omkar Mandhata is a place repeatedly figuring in the Puranic lore. Situated on a picturesque site, it is one of the 12 jyotirlingas in the country. The Hindu and Jain temples at Omkar Mandhata add to the beauty and the sanctity of the place. Burhanpur was among the important cities of Medieval India.

It was the seat of the Faruqis and also of an important subah under the Mughals, where heir-apparents or more efficient Princes like Daniyal and Parviz were posted. It was here that Khushrav lost his life, Khurram lost his beloved spouse Mumtaz Mahal in whose memory the grandest mausoleum was built at Agra, and Alamgir held the office of the Viceroy of Deccan for almost a decade.

Commanding the view of a rich landscape, this town was once famous for its handicrafts, textiles and decorative arts. Asirgarh, one of the most impregnable forts in the country, controlled in medieval times the one and the only western gateway to South. Owing to its strategic position, it was a scene of many momentous battles fought for domination by the Rajputs, Muslims, Marathas and the British. In recent times, Nepanagar with its Newsprint Mill has found a place in the industrial map of modern India.

Several personalities, associated with East Nimar, have left their impress on the life and thought of the people. It was Asa Aheer who built the historic fort of Asirgarh. Saint Burhanuddin of Daulatabad rests in a tomb at Burhanpur. King Adil Khan II laid the foundation for the industrial prosperity of the region by encouraging arts and craft. Pindaris like Chitu and Dulla ravaged the District for many years till their extinction. Singaji, the Sixteenth Century saint and a popular Nimadi poet, was an outstanding holy figure. Tantiya Bhil, the Robin Hood of the region, was a figure inspiring awe and respect both, in his role of a persecutor of the unjust and the friend of the poor.

Coming to the post-World War II period, one notices the finest political journalism in Hindi which owed its inception and flowering to the efforts of Makhanlal Chaturvedi, Affectionately called Dada, Makhanlal Chaturvedi was the doyen of Khandwa in the field of political, literary and public life of the town. The cine-loving proletariat proudly asserts that the stellar luminary Ashok Kumar hails from their District. In brief, East Nimar has a tradition rich in its versatility, range and quality.

Introductory:

Source - East Nimar District Gazeteer by P N Shrivastav, 1969, p.1

[p.1]: Most of East Nimar District formed a part of Lire old administrative subdivision called Prant Nimar. The southern part of the District was included in the old territorial division of Talner, later known as Khandesh. The Prant Nimar is said to have comprised a sizeable portion of the Narmada Valley from the Ganjal river on the east to Hiranphal or the Deer’s Leap on the west, at both of which places the Vindhya and the Satpura ranges come very close to each other and over look the Narmada.

In 1778 Peshwa divided the territory among Holkar, Pawar and Sindhia and retained only the small tracts of Kasrawad, Kanapur and Beria for himself. Later on the possessions of Peshwa and Sindhia came into the British possession and formed parts of this District.

Origin of the Name:

To trace the origin of the name of the present District it is necessary first to find out the origin of the name Prant Nimar from which obviously most of the present District is carved. Nothing definite is known about the latter but it may be guessed that the old Prant Nimar was so called, because a place called Nimawar on the Narmada (now in Dewas District), was the capital of Prant Nimar. Nimawar is also mentioned by the famous Arab writer Alberuni, as Namavur1. The name Nimar happens to be spelt in certain books as Nimaur.2 In course of time and by stages Nimawar, Namavur or Nimaur may have assumed the simple form, Nimar. As most of the territorial divisions derive their names from some one place of importance in the region, and as Nimawar was such a place of religion and administrative importance in the region,3 the old Prant Nimar was called after that name, and the present Nimar District carved out of it retained the same.

The author in this connection mentioned that “The name is supposed to be derived from nim, half, as Nimar was supposed to be half-way down the course of the Nerbudda, but in reality it is much nearer the mouth than the source of the river. Another derivation suggested by the Deputy Commis-

1. E. C. Sachau, Albemni’s India, p. 203.

2. C. P. Administration Report, 1863-64, p. 9.

3. Nimar District Gazetteer, 1908, p. 20.

[p.2]: sioner is from the nim tree which is noticeably common in the District” 1 . All these are conjectures about the derivation of the name of the District and for want of any other ascertainable material on the topic, it remains a subject-matter for conjectures only.

The present District of East Nimar includes only a small portion of the old Prant Nimar, which had nearly 9,000 sq. miles 3 (23,310 Sq. km.) of area. Prior to the States Reorganisation, i.e., on 1st November 1956, the district was officially known as Nimar District and formed part of the Mahakosal region of the erst-while Madhya Pradesh. The western part of the old Prant Nimar originally held by the Holkar, became a part of Madhya Bharat, when that State was formed in the year 1948. As on the reorganisation of States, Madhya Bharat region was merged in Madhya Pradesh, the western part of old Prant Nimar eventually became a part of Madhya Pradesh. This tract with its headquarters at Khargone, also happened to retain its old name of Nimar, and being to the west of the District of former Nimar of Mahakosal region, was named as Nimar (West) or West Nimar, while this District was officially renamed as Nimar (East) or East Nimar from 1st November, 1956.

Topography

Natural Divisions

Source - East Nimar District Gazeteer by P N Shrivastav, 1969, p.4-8

[p.4]: The District lies, for the most part, on the uplands between the valleys of the two major rivers, the Narmada and the Tapti flowing parallel to each other from east to west through the District. The Hatti hill range borders and overlooks the Tapti valley in the south throughout its length in the District. The major natural divisions of the District correspond to the four distinct physiographic divisions, viz., (1) The Narmada valley (2) The Tapti valley (3) The main Satpura ranges and (4) The Hatti range or the southern flank of the Satpuras south of river Tapti.

The general height of the country in Nimar (East) is about 1,000 Ft. (304.8 metres) above Mean Sea Level but the elevations range from 618 Ft. (188.4 metres) in the bed of the Narmada in the extreme north-west to 3,010 Ft. (917.5 metres) at Pipardol peak of the Hatti range,

Narmada Valley: The Narmada flows through the northern part of the District, roughly in an east-west direction. It forms about one-third of the northern boundary of the District. The two small tracts of Chandgarh and Selani are to the north of the river, on which side the District is bordered by the high cliffs of basalt, intersected by numerous deep and dark ravines and alternated by precipitous wooded hills, mostly alineated in a north-south direction.

Among the streams joining the Narmada within the District from the north are Khari and Kanar (Lohar). These are the only perennial streams in the tract. The hills in the Chandgarh and Selani tracts rise conspicuously from 220' to 500' (61 to 152 metres) above the adjacent plains. The general height of Selani tract is about 750' (228 metres) and that of Chandgarh is about 850' (258 metres). The north-south chain of hills in Chandgarh and Selani tracts continue across the Narmada in the south. The most

[p.5]: conspicuous of these is a sand-stone hill. It occupies the elbow formed at the junction of the Chhota Tawa and the Narmada and which rises about 500' (152.4 metres) above the surrounding country.

The southern tributaries of the Narmada flow towards north or north-west revealing the general slope of that part of Narmada Valley which lies within the District. The average height in the eastern part of the valley is about 900' (274 metres) above Mean Sea Level, while in the western part it is about 800' (243 metres). The plain country in the extreme west, below Mandhata, lies at a level of about 700' (213.4 metres) above Mean Sea Level. The catchment area of the Chhota Tawa is at about 1,000' (304.8 metres) above Mean Sea Level.

About 25 miles (40 km.) south of the Narmada near Barur, a low range of foot-hills, commencing on the western boundary of the District, traverses the District towards the north-east until it abuts on the Narmada near the confluence of the Chhota Tawa river. The north-eastern part of this range divides the Narmada valley into two halves, viz., the western and the eastern. This range marks the southern limits of the low-lying valley of the Kaveri River, a tributary of the Narmada in the west and the north-western limits of the Khandwa gap which, though undulating, lies at a higher altitude. The range also forms the watershed between the upstream of the Kaveri flowing north-east and the tributaries of the Chhota Tawa river, both of which ultimately empty their waters into the river Narmada.

The country lying north-west of this range, drained by the Kaveri river is mostly uneven and forested. The forests abound in the belts along the Narmada in the north and along the hill slopes in the south and south-east of the Kaveri valley. There is an open area in the central part of the valley.

The eastern part of the Narmada valley, in the District, is largely drained by one of its important left bank tributaries, the Chhota Tawa which is so called below the confluence near Bhamgarh of the three streams, viz., Abna, Sukta and Bham. River Machak and the Samdeni flow into the Narmada in the extreme north-eastern part of the District. The Chhota Tawa basin occupies the northern slopes of the Satpuras. The western half of the upper Chhota Tawa valley around Khandwa is a plain country with most fertile soil. Once the stream leaves the chain of hills fringing in the south, west and north, it passes through an open country without any significant hill or a forest block, though the surface is undulating. Minor rivers with banks covered with vegetation alternate with broad divides in this part. Some of the narrow valleys are comparatively fertile, where others are bare and stony.

The eastern half of the upper Chhota Tawa valley is bordered by the Satpuras in the south-east which in this part range roughly in the direction from south-west to north-east. This country south and east of Chhanera up to the foot-hills is hilly and much cut-up by the channels of the meandering rivers and streams. Spurs of the Satpuras extend towards the north-west and gradually lose height

[p.6]: as they advance between the streams. The area is mostly rocky with thin soil in the depressions. The thick forests cover the slopes of the Satpuras, the foot-hills and the lower valley of the Agni. Forests with lesser economic value abound throughout the area. Some patches in the forests have been cleared for cultivation and have given rise to interspersed villages.

The lower Chhota Tawa valley is not a level plain throughout since spurs and low out-crops of the Satpuras appear right upto the Narmada in the north. Considerable areas are covered with forests, the clearings of which support numerous small villages with arable land. The hills and forests abound in most of the western bank of the Chhota Tawa river. The forested tract of Khandwa Tahsil south of the Narmada extends further east into Harsud Tahsil. East of the Chhota Tawa river the country around Harsud and Kasrawad is undulating and is covered with black soil of uneven thickness. Stretches of deep soil deposits in the depressions make good wheat lands. As one proceeds from here towards the Hoshangabad District boundary in the east, the relief becomes sharper and accentuated and the soils poorer and lighter.

Tapti Valley: The Tapti flows in a narrow valley between two parallel ranges of the Satpura in the southern parts of the District. It stretches for about 50 miles (80 km.) from east-north to west-south-west. The eastern half of the valley in the Manjrod and Nawtha tracts, is hardly 10 miles (16 km.) wide. The upper portion of Manjrod and Nawtha tracts was once fertile and well cultivated but now mostly covered with forests. The valley opens west of Samardeo Hill towards Burhanpur where it is about 20 miles (32.2 km.) wide. Here the soil is deeper and richer and form the most cultivated and densest populated area of Burhanpur tahsil.

Satpura Ranges: The Satpura (literally ‘seven folds’) is the name given collectively to a complex system of ranges and high lands about 600 miles (966 km.) long and 100 miles (161 km.) wide which lie to the south of the Narmada from the western coast of India to the Amarkantak hills in the east. This system includes ranges as far south as the Southern Maikal range or Saletakri hills. The various hill ranges, of which it is composed, are highly dessected by the erosive action of rivers and streams, and run approximately parallel to each other in an east-west direction. They are known by different local names. Earlier the name Satpura was applied to the hills which separate the Narmada and the Tapti valleys in East Nimar, east of Asirgarh hill and was styled as Satpura or seven sons of the Vindhyan mountains.

It was only during the early British regime that the whole series of hill ranges, about 600 miles (966 km.) long and, in their greatest depth exceeding a hundred miles (161 km.) from north to south, was known after the Satpura range of East Nimar.

[p.7]: The Satpuras, in this District, are bifurcated into two parallel ridges on either side of the Tapti valley. The main one, i.e., the northern branch of the Satpura, extends through the south-eastern part of Harsud Tahsil and more or less along the boundary between Khandwa and Burhanpur tahsils. It is only in the western extremity that this boundary passes through the northern foot-hills of the Satpuras, Asirgarh and other conspicuous peaks falling in Burhanpur, the southern Tahsil. The hill range west of Asirgarh hill is known as Rajpipla hills which extends up to the Western-Ghats in the west. The hills in the eastern extremity of the District belong to the Kalibhit range which in most of its parts falls in Betul District. Joining these two parts, is the water-parting line of low hills which may be called the Satpura proper, by which name the whole scries of hills south of the Narmada came to be known and which provided the lowest and convenient pass-way between northern and the southern parts of India.

The Rajpipla in East Nimar is about 24 miles (38.6 km.) wide from north to south and above 1,250 Ft. (381 metres) from the Mean Sea Level. The line of more prominent hills rising up to 2,000' (609.6 metres) from the Mean Sea Level extends like the two sides of a triangle with its apex in the Amba reserved forest, the western most limit of the District. A hill at this nodal point attains a height of 2,543 Ft. (775.1 metres) which is the highest elevation of the Satpuras in the District, north of the Tapti river. Other peaks rising to notable heights are the hills north of Amba, 2,244 Ft. (684 metres), the hill south-west of Itaria, 2,324 Ft., (708 metres), Gaira Barla hill, 2,338 Ft., (712.6 metres), Pipalphata, 2,183 Ft. (665.4 metres) and Asirgarh, 2,189 Ft. (667.2 metres). The waters of Sukta river have corroded and lowered the central part along its deep channels between the two prominent lines of Rajpipla hills. The width of the hilly area along the water parting line of the Satpura proper is about 11 miles at their base but in height they are above 1,250 Ft. (381 metres) from the Mean Sea Level. Hilly area is not continuous and there are several cols, through one of which the Bombay-Delhi railway line passes from south to north. After entering Harsud Tahsil, beyond Kulhardeo hill, 1,600 Ft. (487.7 metres), the Satpuras gradually gain height and form a continuous chain of rugged and much dissected hills which are nowhere less than 1,500 Ft. (457.2 metres) from the Mean Sea Level. There are several hills rising above 2,000 Ft. (609.6 metres) from Mean Sea Level in the Kalibhit range of which the notable points are Kalibhit, 2,225 Ft. (678.2 metres), Kelipahar, 2,476 Ft. (754.7 metres), Phepri, 2,137 Ft. (651.3 metres) and the hill 2,296 Ft. (699.8 metres) high east of Karwani village. Practically all the hills from Amba Reserved forest in the west to Genjal nullah in the east are covered with forests which are Government reserves and form a large belt occupying the northern part of Burhanpur Tahsil and the south-eastern part of Harsud Tahsil.

Hatti Range: The southern branch of the Satpuras, divided from the main range by the Tapti valley runs close to the southern boundary of the District. It is locally

[p.8]: known as Hatti range, as it was formerly divided into four hattis or estates held by predatory Bhil chiefs. The boundary lies chiefly along the outer border of the range so that all of it except a few spurs, belongs to Nimar (East). The name Hatti is probably derived from Hathi, an elephant. The configuration of the range presents a series of long narrow valleys on the northern face, the watershed lying generally within a mile or two of the Maharashtra (Berar region) boundary. The declivities on that side are more precipitous. The valleys are flanked by eminences having generally flat tops, with narrow strips of culturable soil. The general elevation is about 2,000 Ft, (609.6 metres) above Mean Sea Level or about 1,200 Ft. (365.8 metres) above the plains of Berar in the south and the Tapti in the north. A few peaks on the extreme east reach the height of 3,000 Ft. (914.4 metres) which are the highest points in the district. Among the heights recorded are Pipardol, 3,010 Ft. (917.4 metres), Baingarh, 2,717 Ft. (828 metres), Sitoli, 2,479 Ft. (755.6 metres), Bhingar, 2,477 Ft., (755 metres) and Jitgarh, 1,959 Ft. (597 metres). The elevation of the range falls regularly towards the west, and at last it vanishes completely near the south-western boundary of East Nimar and East Khandesh District of Maharashtra State in the Tapti valley. The whole of the Hatti range is covered with thick forests nearly all of which are under Government reserves.

The Samardeo hill is a continuation of Hatti range, and detatched from it. It is more or less identical to Hatti range in respect of its east-west expansion with a steeper slope on the southern edge than on the northern face. The vegetative cover is equally good and similar in nature.

River System and Water Resources

Source - East Nimar District Gazeteer by P N Shrivastav, 1969, p.8-13

Drainage

[p.8]: The drainage of the District falls under the Narmada and the Tapti river systems. The water-parting line between the two river-systems runs along the crest of the northern range of the Satpuras. The major portion of the District, north of this line, except the low tracts of Chandgarh and Selani, drains towards the north into the Narmada through the Chhota Tawa and the Kaveri rivers and a large number of small streams, The tracts north of the Narmada slope towards the south and the drainage is represented by the rills and rivulets joining the Narmada to the south. The area between the northern and the southern forks of the Satpuras in the District, mostly falling in Burhanpur Tahsil, is drained by a large number of streams descending into a hollow country (cyncline) 1 occupied by the Tapti. As the southern boundary of the district lies chiefly along the crest of the Hatti range, the southern slopes of the range drain into the Poorna, a left bank tributary of the Tapti river in East Khandesh District of the Maharashtra State.

1. As suggested by Prof. S. M. Ali of the University of Saugar the valleys of the Tapti and Narmada may be Synclinal valleys.

[p.9]: The two rivers, the Narmada and the Tapti contrary to all other principal rivers of the South Indian plateau flow towards the west, their courses being in the fault or rift-valleys 1 in the hard and compact mass of the Deccan plateau. The drainage of the major rivers in the District therefore, is typical to the rift valley drainage. The narrow and straight alluvial valleys, the closely bordering ranges, the deep river-beds and numerous small tributary rills joining the major rivers more or less at right angles are all the characteristics of the Narmada and the Tapti river systems after these rivers have entered the rift-valleys.

The drainage in the denuded parts of the Satpuras and in the river valleys resting on it as in the Chhota Tawa valley, shows a dendritic pattern. This may be the result of a gradual water erosion for long time on a trap-country. The small plateau south-west of Mundi village is drained radially. The radial type of drainage is also represented by relatively high elevated area of Punasa which slopes around and from where the streams flow in all directions.

The volume of water in the streams and rivers depends upon their size which in turn corresponds to their catchment areas. The seasonal variation is great. The river-beds are mostly studded with rocks which due to difference in their hardness have helped in formation of water-pools behind the stretches of hardness. Falls and rapids have developed due to the removal of the relatively softer material after a line of hard rocks. The rocks have also caused, at places, the bifurcations or multiplication of the river channel. Mandhata, a river island between the two channels of the Narmada is well-known as a Hindu pilgrimage centre. There are other river islands, though of little importance. All these characteristics of the rivers have acted to the disadvantage in their economic utilisation. There is no line of navigation in the District except the ferry boats across the rivers at the terminus of thorough fares and the pilgrim centres. The deep channels, the high steeply rising banks and the fluctuating volume of water make it difficult to construct a dam across the river or to irrigate the country through the channels. There is an important water-fall in the District at Punasa, where the Narmada falls from a height of about 40' (12.2 Metres). It may be said that this fall is exactly equal to the fall on the Narmada at Mandhar 25 miles (40.2 Km.) below Handia.

The Narmada

The Narmada is one of the seven most sacred rivers referred to in religious books, excluding the Rig Veda and the Sutras of Panini. This river was known to Ptolemy and the author of the Periplus as the Nommados or Nammadius, but not noticed by Magasthenes. The Reva Khand of the Skanda Puran has a chapter devoted to the story of the birth of the Narmada and of which it relates many legends. The river is stated to have emerged from the body of Lord Shiva, after the performance of great penance in the Riksha Mountain (a part of the Vindhyachal), whence it acquired its great virtues. There is also a mention that the river was created in the form of a lovely damsel whose beauty captivated the gods and

1. E. H. Pasco, Manual, Geology of India, p. 22.

[p.10]: brought them all to her feat. Shiva laughed when he saw the enamoured gods and named her Narmada, or delight-giving in consequence. In Central India, the Narmada is held to be far more sacred than any other river. Even the Ganga is obliged to come and dip in once a year. She comes in the form of a coal-black cow and returns home pure white free from all sins. A mere sight of the Narmada is equivalent to a bath in the Ganga, and such are its virtues that all sins of the person who sees or dips into its water are removed.

Religious fairs are held among other places, at Bheraghat, Gwarighat, Burmanghat, Omkareshwar, along its banks. The Narmada rises from the western flank of the Amarkantak plateau at about 22° 40' North and 81° 46' East in Shahdol District and enters the sea without forming a delta, below Broach, after a course of 801 miles.

Down the Amarkantak hills the river passes through Mandla and Jabalpur Districts and further forms the boundaries between the Districts of Narsimhapur and Hoshangabad in the south and Raisen, Sehore and Dewas Districts in the north. It enters Nimar (East) District after its confluence with Machak river at Panghat. After passing the western part of Chandgarh pargana of Harsud tahsil it is joined by the Chhota Tawa river from the south. Further it flows along the northern boundary of Khandwa tahsil except where it leaves Selani pargana north of its course. For about 40 miles (64.4 Km.) after entering the District the Narmada flows between high alluvial banks, closely bordered by high cliff's of basalt and wooded hills on the north and a wild broken country on the south. The banks are intersected by numerous deep and dark ravines, the favourite resorts of tigers in the hot season. A sandstone hill about 500 Ft. (152.4 metres) high from surrounding country, occupies the angle at the junction of the Chhota Tawa and the Narmada. Throughout this distance the stream is much contracted and forms in the dry season a chain of pools alternating with rapid shallows. Opposite a place called Pemgarh is a curious back-water known as Kutra Kund, formed by a diagonal ledge of hard basalt and filled only when the river is in flood. Waste timber brought down by the current is whirled into this basin and stranded on sloping sand-banks at its head. At Dhairi opposite Punasa, the river tumbles through and partly over a broken ledge of hard basalt about 40 Ft. (12.2 metres) high; and then boils deep and sullen through a gorge of the same rock not more than 50 Ft. (15.2 metres) in breadth. Below the falls again, down to the island of Mandhata, the channel is tolerably open with a minimum of four feet (1.2 metres) of water at the deepest part in the hot weather. Immediately above Mandhata, the Narmada is joined by the small stream of the Kaveri from the south. Below Mandhata the hills and rugged ground recede and an open alluvial basin begins, upwards of a hundred miles (160. 9 km.) long which formed the kernel of old Prant Nimar. The banks in this part consist of sandy alluviam and are 60 Ft. to 70 Ft. (18 to 21 metres) high. Below Mandhata the hills and the rugged ground that have up to this point environed the river recede, the Satpuras being 40 miles (64.4 Km.) to the south and the Vindhyas about 16 miles (25.7 km.) to the north.

The Tapti

The Tapti is also one of the sacred rivers o India. Amongst its various

[p.11]: names Tapti, Payoshni, Tapi, and Tapni, are more commonly known. All these names cannote one and the same meaning- the cooler of the Tap, meaning heat. It is said to have been created by the Sun to protect himself from his own warmth. It is believed to have risen from the sacred tank to Multai (multapi, the source of the Tapti), on the Satpura plateau, but its real source is two miles distant (78° 15'E: 21° 48'N). It flows in a westerly direction through the Betul District, at first traversing an open and partially cultivated plain, and then ploughing into a rocky gorge of the Satpura hills between the Kalibhit range in Hoshangabad and East Nimar and Chikalda in Berar. Its bed here is rocky, overhung by steep banks, and bordered by forests. It enters East Nimar at a distance of 120 mile (193 km.) from its source and is still confined, for about 30 miles (48.3 km.) in a comparatively narrow valley. There are some small basins of exceedingly rich soil but they are mostly forested. The valley opens out a few miles above Burhanpur, the Satpura hills receding north and south. The towns of Burhanpur and Zainabad are located on either side of the river in the centre of the 20 miles (32.2 km.) wide rich alluvial basin. About nine miles (14.5 Km.) down the town of Burhanpur, the Tapti enters Khandesh where, it is joined by the Purna on its left bank from the hills of Berar. The river falls into the Arabian sea near Surat with an estuarine mouth like that of the Narmada.

The general direction of the river in Nimar (East) is from north-east to south-west. Its banks are too high, 30 Ft. to 60 Ft. (48 to 97 metres) for irrigation, and the bed is crossed at several places by ridges of rocks; hence, the river is not navigable except for about 20 miles (32 Km.) near its estuary. The Tapti runs so near the foot of the Satpuras that its tributaries on the right bank are small but on the left bank the streams are of larger size. Among the tributaries Mona, Utaoli and Umraoti are the feeder streams of some size in the District which flow for some distance rapidly through the hills and valleys, and when they reach the open plain, cut deep channels through the sandy alluvial sub-soil.

The Chhota Tawa

This river is formed by the confluence of the three streams of Abna, Sukta and Bham near Bhamgarh, and joins after a course of 32 miles (51.5 Km.), flowing south to north through the Harsud Tahsil. It is called the Chhota Tawa to distinguish it from the more important river, Tawa in Betul and Hoshangabad Districts. Tawa signifies the flat bed of the river. The tributaries of the river are the Agni, the Piprar, the Gangapat and the Kala Machak on the right bank and Khurkhuri and another Piprar on the left bank. It is crossed by the Central Railway near Bilod.

The Abna

Abna rises in the south-west of the Khandwa Tahsil near Rajpura. It flows in an easterly direction through the Khandwa Tahsil, passing within a mile (1.6 Km.) of Khandwa, and joins the Sukta near the village of Kupasthal (Jaswadi) about six miles (9.6 Km.) further on. The length of the river is about 33 miles (53.1 Km.) It is crossed by the line of Central Railway near Khandwa.

[p.12]:

The Sukta

Sukta rises in the East Khandesh District and enters the Burhanpur Tahsil at its north-western boundary. After traversing it for about 15 miles (24.1 Km.) it enters the Khandwa Tahsil near Kalana, and returns to the north. It is joined by the Abna near Kupasthal, and thence flowing north-east falls into the Chhota Tawa near Selda. The name is probably a corruption of Sukh Tawa ‘The dry Bed’. The river is crossed by the railway near Behar, ten miles (16.1 Km.) south of Khandwa. Its length in the District is about 50 miles (80.5 Km.). At Sukta on the border of Khandwa and Burhanpur tahsils is a, spring known as Bhimkund, near the river’s bank.

The Kaveri

The Kaveri rises from the ridge diagonally traversing Khandwa tahsil. It is one of the sacred streams. It runs into the Narmada some little way above the island of Mandhata. Local belief is that the waters of Kaveri here at its real confluence do not mix with the waters of the Narmada, but flow across them and round the north side of the island, and mix with the waters of the Narmada below the island. The belief has thus attributed greater sanctity to this confluence than the real one and pious devotees take dip here and not at the real confluence.

Tanks

Lakes as such in the District are none, but a few tanks exist of which one at Mohghat situated at a distance of four miles (6.4 Km.) north-west of Khandwa town deserves mention. The tank covers an area of about 500 acres (202.3 hectares). This was formed by damming up a stream. Later on its catchment area was enlarged to nearly nine square miles (23.3 Sq. km.) by the construction of a canal four miles (6.4 Sq. km.) long to Ajainti. It is one of the water-supplying sources of the Khandwa town. The water is usually carried from it to the town by gravitation but when the Mohghat reservoir runs low, the water is pumped. The pumping station was constructed in the year 1887. The tank for last few years is being utilised as one of the fish-breeding centres of the district. Another tank of Punasa covers an area of 200 acres (80.9 hectares).

Springs

At Sukta on the boundary of the Burhanpur and Khandwa tahsils is a small water spring popularly known as Bhimkund. It is situated near the bank of the river Sukta. On the occasion of Vasant Panchmi festival a small fair is held near this Kunda (spring). People attending the fair carry with them the water of this spring to sprinkle it on the standing crops of their fields in the belief that the water has some resisting power for rust in wheat and smut in jowar.

Another spring takes its source in Harsud Tahsil of the District. It is called the Gomukh and is located at Gaurbrigiri. This spring flows all the year round and its water is utilised for the purpose of irrigation. It irrigates about 60 acres (24.3 hectares) of land in the vicinity.

[p.13]: There are other springs in the vicinity of Burhanpur town. These are among the eight subterranean conduits of the Mughal water works engineered between 1618 and 1650. Two of these underground springs, viz,, Khuni Bhandara and Chintavaran carry ample fresh water all the year round to the municipal water works of Burhanpur and its suburbs, Lalbagh and Bahadurpur.

Places of interest

  • Ganguli House, the ancestral home of Ashok Kumar and Kishore Kumar. Also named Gauri Kunj, after their mother.[12]
  • Samadhi of Kishore Kumar.[13]
  • Four Kunds located in four directions of the city, called Padam Kund, Bheem Kund, Suraj Kund and Rameshwar Kund.[14]
  • Dada Darbar, popularly known as Shri Dadaji Dhuniwale.
  • Shree Vitthal Mandir Khandwa the temple was founded by shree swami sacchidanand swami maharj in 1850, temple is made up of sheesham and sagvan wood. Great example of architecture.
  • Turja Bhavani Temple
  • Nav-chandi Devi Dham

खण्डवा परिचय

खण्डवा भारत के मध्य प्रदेश राज्य के खण्डवा ज़िले में स्थित एक नगर है। यह ज़िले का मुख्यालय भी है। खंडवा (पूर्वी निमाड़) जिला मुख्य रूप से हिंदुओं और जैनियों के धार्मिक पर्यटन स्थल के लिए जाना जाता है। 12 ज्योतिर्लिंगों में से एक ओंकार ममलेश्वर ओंकारेश्वर शहर में पवित्र नदी नर्मदा ("माँ नर्मदा" के रूप में सम्मानित) के तट पर स्थित है। दादा धूनीवाले का समाधि स्थल खंडवा शहर में स्थित है। ब्रह्मगीर महाराज का समाधि स्थल खंडवा शहर के पास स्थित है। निमाड़ के कबीर का समाधि स्थल सिंगाजी मुंडी कस्बे के पास पिपलिया सिंगाजी में स्थित है। बुखारदास बाबा का समाधि स्थल नया हरसूद, छनेरा के पास है।

हनुवंतिया में साहसिक पर्यटन उपलब्ध है, जिसे इंदिरा सागर पर्यटक परिसर, हनुवंतिया के नाम से जाना जाता है। सैलानी ओंकारेश्वर के पास साहसिक पर्यटन के लिए द्वीप विकसित कर रहा है।

खण्डवा समुद्र तल से 900 मीटर की ऊंचाई पर है। यह जिला नर्मदा और ताप्‍ती नदी घाटी के मध्य बसा है। 6200 वर्ग किलोमीटर के क्षेत्र में फैले खण्डवा की सीमाएं बेतूल, होशंगाबाद, बुरहानपुर, खरगोन और देवास से मिलती हैं।

ओमकारेश्‍वर यहां का लोकप्रिय और पवित्र दर्शनीय स्‍थल है। इसे भारत के 12 ज्योतिर्लिगों में शुमार किया जाता है। इसके अलावा घण्टाघर, दादा धुनीवाले दरबार, हरसुद, मूँदी, सिद्धनाथ मन्दिर, पूर्णेश्वर धाम पुनासा और वीरखाला रूक यहां के अन्य लोकप्रिय पर्यटन स्थल हैं।

वीरखाला रूक ओंकारेश्वर पहाड़ियों के पूर्वी किनारे पर स्थित एक प्राचीन मंदिर है, जहाँ पहले भैरव को प्रसन्न करने के लिए नरबलि दी जाती थी, जिसे ब्रिटिश काल में बंद कर दिया गया था। पहाड़ी के पास कुंती माता का मंदिर भी है.

इतिहास : प्राचीन मान्यताओं के अनुसार खण्डवा शहर का प्राचीन नाम खाण्डववन था जो मुगलों और अंग्रेजो के आने से बोलचाल में धीरे धीरे खण्डवा हो गया।

मान्यतानुसार श्रीरामजी के वनवास के समय यहाँ सीता माता को प्यास लगी थी तथा रामजी ने यहाँ तीर मारकर एक कुआ बना दिया और उस कुए को रामेश्वर कुए के नाम से जाना जाता है जो खण्डवा के रामेश्वर नगर में नवचण्डी माता मन्दिर के पास स्थित है अतः खण्डवा मान्यता अनुसार हजारों वर्ष पुराना है जिसका आधुनिक रूप वर्तमान खण्डवा है।

12वीं शताब्दी में यह नगर न मत का महत्त्वपूर्ण स्थान था। यह नगर पुरातन नगर है, यहाँ पाये जाने वाले अवशेषों से यह सिद्ध होता है, इसके चारों ओर चार विशाल तालाब, नक़्क़ाशीदार स्तम्भ और जैन मन्दिरों के छज्जे स्थित हैं। खण्डवा जिले से ही बुरहानपुर जिला बना है।

आधुनिक नगर: 1864 से यह नगर मध्य प्रदेश के नवगठित निमाड़ ज़िले का मुख्यालय रहा। 1867 में इसे नगरपालिका बना दिया गया। भारत के मध्य प्रदेश राज्य में स्थित खण्डवा एक प्रमुख शहर है। 6200 वर्ग किलोमीटर के विस्तार वाले खण्डवा की सीमा बेतूल, होशंगाबाद, बुरहानपुर, खरगोन और देवास से मिली हुई हैं। ओंकारेश्‍वर यहाँ का बहुत ही लोकप्रिय प्रसिद्ध और पवित्र धार्मिक स्थल है। ओंकारेश्‍वर भारत के 12 ज्योतिर्लिंगों में से एक है।

प्रमुख पर्यटन स्थल

माँ तुलजा भवानी माता मन्दिर: खण्डवा का प्रसिद्ध भवानी माता मन्दिर धूनीवाले दादाजी के दरबार के पास स्थित है। यह मन्दिर माता तुलजा भवानी को समर्पित है। यह मन्दिर खण्डवा, मध्य प्रदेश में स्थित है। यह खण्डवा का प्राचीन मन्दिर है जहा प्रतिदिन भक्तो की भीड़ लगी रहती है कहते हैं भगवान राम अपने वनवास के दौरान इस स्थान पर आए थे और यहाँ उन्होंने नौ दिनों तक तपस्या की थी। नवरात्र में यहाँ नौ दिनों तक मेला लगता है, जिसे देखने और माता के दर्शन करने के लिए प्रतिवर्ष हजारों लोग यहाँ आते हैं। ऐसी मान्यता है की माँ भवानी के दर से हर मुराद पूरी होती है।

दादाजी धूनीवाले: दादाजी धूनीवाले (श्री केशवानान्दजी महाराज) भारत के एक महान सन्त थे ज़िनेः दादाजी डण्डे वाले के नाम से भी जाना जाता था। उन्होने 19वी और 20वी शताब्दी मे भारत, ख़ास कर मध्य भारत में, यात्राएँ की। दुनिया भर मे उनके लाखों भक्त उन्हे शिव भगवान का रूप मानते हैं। दादाजी महाराज हमेशा अपने साथ एक डण्डा रखा करते थे और जहाँ भी विराजमान होते वहाँ धूनी रमाते थे। जन कल्याण करने का दादाजी का बहुत ही विचित्र तरीका था, वे भक्तों को गाली देते व डण्डा मारते। हर तरह के लोग, अमीर से अमीर और ग़रीब से ग़रीब दादाजी के आशीर्वाद के लिए आते। इन्ही महान सन्त जिन्हें दादाजी धुनी वाले के नाम से पुकारा जाता है की समाधि खण्डवा में है जहा निरन्तर धुनी जलती रहती है जिसे धुनी मैया कहते है तथा दादाजी की समाधि दर्सन और धुनी मैया की भभूती का प्रसाद लेने दूर दूर से भक्त्त आते हैं।

माँ नवचण्डी देविधाम मन्दिर: यह मन्दिर खण्डवा खण्डवा रामेश्वर छेत्र में स्थापति नवीनतम मन्दिर है जो माँ नवचण्डी माता को समर्पित है जहा माता के मन्दिर के साथ ही भगवान शिव का मन्दिर कालीमाता मन्दिर स्थापित है यह एक मनोहर धार्मिक मन्दिर है जो रेलवे स्टेशन से लगभग 3 किलोमीटर की दुरी पर स्थापित है जहा महाशिवरात्रि पर विशाल मेले का भी आयोजन किया जाता है

गौरी कुंज ऑडिटोरियम: यह ऑडिटोरियम संगीत का सांस्कृतिक हॉल है, जो खण्डवा रेलवे स्टेशन से 1 किलोमीटर की दूरी पर है। यह ऑडिटोरियम जाने माने गायक किशोर कुमार गांगुली की याद में बनवाया गया था। शहर के प्रमुख सांस्कृतिक कार्यक्रम यहीं आयोजित किए जाते हैं। देवी नव चण्डी धाम और तुरजा भवानी माता मन्दिर रेलवे स्टेशन के निकट ही स्थित हैं।

नागचून तालाब: नागचून गांव में बना तालाब यहां का जाना माना पिकनिक स्थल है। तालाब खंडवा से लगभग 5 किलोमीटर दूर है। यह बान्ध खण्डवा की सिचाईं का प्रमुख स्रोत है। इसके चारों ओर की हरियाली तालाब को और आकर्षक बना देती है।

ओमकारेश्‍वर का गुरूद्वारा: इस गुरूद्वारे को नानकदेव के ओमकारेश्‍वर आने के पश्चात् बनवाया गया था। नानकदेव के प्रति सम्मान प्रकट करने के लिए बना यह गुरूद्वारा सिख और हिन्दू धर्म के अनुयायियों से भरा रहता है। ओमकारेश्‍वर रेलवे स्टेशन यहां का निकटतम रेलवे स्टेशन है।

सिगांजी धाम: सिगांजी धाम एक धार्मिक एवं दर्शनिक स्थल है। खण्डवा जिले के मूँदी नगर से 16 कि.मी की दूरी पर इन्दिरा सागर परियोजना के बैकवाटर में स्थित है। चारों और से पानी में घिरे इस समाधी स्थल का सौन्दर्य अति सुन्दर है।

मान्धाता हिल: यह पवित्र पहाड़ी नर्मदा नदी के तट पर स्थित है। यह पहाड़ी धार्मिक दृष्टि से जिले का महत्वपूर्ण स्थल है। देश में 12 शिव ज्योतिर्लिगों में एक यहीं स्थित है। ओमकारेश्‍वर और ममलेश्वर यहां के प्रमुख मन्दिर हैं। पहाड़ी के चारों ओर से बहती हुई नर्मदा नदी इसे ओम के आकार का बनाती है। यह पहाड़ी खण्डवा से करीब 75 किलोमीटर दूर है।

भगवान सम्भवनाथ मन्दिर: सिद्धवरकूट स्थित भगवान सम्भवनाथ का यह मन्दिर बारा मन्दिर के नाम से भी जाना जाता है। माना जाता है कि जैन धर्म के तीसरे र्तींथकर का यह मन्दिर भूमि को खोदकर निकाला गया था। मुख्य मन्दिर के अलावा यहां चार अन्य मन्दिर भी देखे जा सकते हैं जिसमें भगवान चन्द्रप्रभु, अजीतनाथ, पार्श्‍वनाथ और सम्भवनाथ की मूर्तियां स्थापित हैं।

घण्टाघर: खण्डवा रेलवे स्टेशन से 1 किलोमीटर की दूरी पर घण्टाघर एक स्थल है। सूरजकुण्ड, पद्मकुण्ड, भीमाकुण्ड और रामेश्वर यहां के चार पवित्र कुण्ड हैं। दादा धुनी वाले की समाधि, तुरजा भवानी मन्दिर और नव चण्डी देवी घाम भी यहां के लोकप्रिय पवित्र स्थल हैं।

वीरखाला रूक: ओमकारेश्‍वर की पहाड़ियों की पूर्वी दिशा में स्थित वीरखाला एक प्राचीन मन्दिर है। माना जाता है कि प्राचीन काल से ही यहां शिव के अवतार भैरव को प्रसन्न करने के लिए मानव बलि दी जाती थी जिसे ब्रिटिश काल में समाप्त किया गया था। पहाड़ी के निकट ही कुन्ती माता का मन्दिर है।

काजल रानी गुफा: ओमकारेश्‍वर से लगभग 9 किलोमीटर दूर यह एक खूबसूरत पिकनिक स्थल है। यहां से आसपास के क्षेत्र का सुन्दर नजारा देखा जा सकता हैं। काजल रानी गुफा के निकट ही सतमत्रिका गुफा स्थित है। जुलाई से मार्च की अवधि यहां आने के लिए सबसे उपयुक्त मानी जाती है।

देवझिरी भूतेश्वर महादेव मन्दिर: खण्डवा से लगभग 15 किलोमीटर दूरी पर भोजाखेडी गाँव के पास पहाड़ी छेत्र में स्थित एक प्राचीन शिवलिंग है जिसपर प्राकृतिक रूप से निरन्तर जलधारा प्रवाहित होती रहती है

सूरजकुण्ड, पदमकुण्ड, रामेश्वर कुण्ड और प्रसिद्ध भीमकुण्ड: प्राचीन काल में खाण्डववन के नाम से प्रचलित शहर के चारों दिशाओं में चार कुण्डों ऐतिहासिक धरोहर के रूप में विराजमान है। पूर्व में सूरजकुण्ड, पश्चिम में पद्मकुण्ड, उत्तर में रामेश्वर कुण्ड और दक्षिण में प्रसिद्ध भीमकुण्ड स्थापित है। यहां पर भोले बाबा विराजित हैं।

इंदिरा सागर पर्यटक संकुल, हनुवंतिया, खण्‍डवा

Indira Sagar Tourist Complex, Hanuvantiya- District Khandwa

हनुमंतिया द्वीप मध्य प्रदेश पर्यटन में एक उभरता जल पर्यटन स्थल है। यह पश्चिमी मध्य प्रदेश में खंडवा शहर के करीब है। यह मध्य प्रदेश पर्यटन विकास निगम द्वारा विकसित और संचालित है। “हनुमंतिया” नाम के स्थानीय गाँव के नाम पर है जो मध्य प्रदेश में खंडवा जिले की पुनासा तहसील में स्थित है। राज्य पर्यटन विभाग ने इस क्षेत्र को जल पर्यटन गतिविधि के लिए उपयुक्त पाया, इसलिए इसे विकसित करने का निर्णय लिया, जिसमें उन्होंने बोट-क्लब, आवास सुविधा, सड़क संपर्क सुनिश्चित किया है ।

इंदिरा सागर परियोजना के बारे में: इंदिरा सागर बांध मध्य भारत में मध्य प्रदेश में एक बहुउद्देशीय बांध परियोजना है। यह नर्मदा नदी पर बनाया गया था जो मध्य भारत से पश्चिमी भारत तक बहती थी। परियोजना की आधारशिला वर्ष 1984 में भारत के प्रधान मंत्री द्वारा रखी गई थी लेकिन कई वर्षों बाद मुख्य बांध का निर्माण वर्ष 1992 में शुरू हुआ था और वर्ष 2003 में पूरा हुआ । इसका जलाशय भारत के सबसे बड़े जलाशयों में गिना जाता है, जिसकी क्षमता 12.22 बिलियन घन मीटर है।

पर्यटन: इंदिरा सागर बांध का बैकवाटर एक विशाल झील है, जिसमें पर्यटन विकास की अपार संभावनाएं हैं। इस क्षेत्र में पर्यटन विकास के लिए इस बांध के पानी के दोहन के लिए हनुमंतिया का विकास किया गया है। इस तथ्य को महसूस करते हुए, मध्य प्रदेश पर्यटन विभाग ने इस साइट को विकसित करने और पर्यटकों के लिए एक नया स्‍थान बनानें की पहल की। यह बैकवाटर पर आवास, रेस्तरां और नौका विहार, क्रूज की सवारी की सुविधा प्रदान करता है। आवास के लिए, केवल एक होटल “हनुवंतिया पर्यटक परिसर” उपलब्ध है, जो एमपीएसटीडीसी का है। बांध के आसपास का क्षेत्र प्राकृतिक पर्यटन के लिए भी अच्छा है जिसमें बर्डवॉचिंग, स्तनधारियों को देखना शामिल है। इंदौर टूरिस्ट सर्किट का दौरा करते समय, कोई इस जल पर्यटन स्थल को भी शामिल कर सकता है। यह महेश्वर से सिर्फ 140 किमी और ओंकारेश्वर से 95 किलोमीटर दूर है ।

Source - https://khandwa.nic.in/en/tourist-place/indira-sagar-tourist-complex-hanuvantiya/

Notable persons

  • Late B L Dhaka - Mob:9926013854
  • Ajit Singh Patel- Thana Prabhari Mundi, Dist: Khandwa, Mob: 9425086166
  • Hisalal Nathu ji jat- 9407455411
  • Ramchandra Jat-milk dairy 6266548483
  • Ashok Jat , milk dairy -- 9617680051
  • Banshi lal Jat, milk dairy - 8959692764
  • Moti Lal Jat , milk dairy- 8770509341

Gallery

  • Shri Hisalal Nathu ji jat Khandwa.

    Shri Hisalal Nathu ji jat Khandwa.

External links

Source

See also

References

  1. ↑ E. C. Sachau, Albemni’s India, p. 203.
  2. ↑ C. P. Administration Report, 1863-64, p. 9.
  3. ↑ Nimar District Gazetteer, 1908, p. 20.
  4. ↑ East Nimar District Gazeteer by P N Shrivastav, 1969, p.1
  5. ↑ East Nimar District Gazeteer by P N Shrivastav, 1969, p.1
  6. ↑ Ibid, p.1
  7. ↑ East Nimar District Gazeteer by P N Shrivastav, 1969, p.2
  8. ↑ Subodh Kapoor (2002). Encyclopaedia of Ancient Indian Geography, Volume 2. Genesis Publishing Pvt Ltd. p. 435. ISBN 9788177552997.
  9. ↑ B.H. Mehta (1984). Gonds of the Central Indian Highlands Vol II. Concept Publishing Company. p. 569.
  10. ↑ "Kalachuris of Mahismati". CoinIndia.
  11. ↑ Charles Eckford Luard, Ram Prasad Dube (1908). Indore State Gazetteer. Superintendent government printing, India, Original from University of Minnesota. p. 221.
  12. ↑ Santoshi, Neeraj (4 August 2014). "Kishore Da's house lives in neglect in Khandwa". Hindustan Times.
  13. ↑ "Curfew drowns music riot on Kishore b'day". The Times of India. 3 August 2014.
  14. ↑ https://www.khandwa.nic.in/tourism.htm
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