sign in sign up
<<
Home , Ahor, Bhadrajun, Bhinmal, Jalore, Jalore district, Jaswantpura

District Survey report of District 1.0 Introduction

The district derives its name from the town of Jalore, which is the headquarters of the district administration. District is located between latitudes 24º 37’ 00” to 25º 49’ 00” and longitudes 71º 11’00” to 73º 05’00” with an area of 10,640 Sq. kms (3.11% of the State). The district is part of Division. The district is composed of five sub-divisions viz. Jalore, Ahore, , , which cover seven tehsils viz: Jalore, Ahore, Bhinmal, Sanchore, Raniwara, Sayala, Bagora and seven blocks viz: Jalore, Ahore, Bhinmal, Sanchore, Raniwara, Sayala & . Total number of in the district is 802 and it also has 3 urban towns. Total population of the district as per Census 2011 is 1828730 with male and female population of 936634 and 892096 respectively. Administrative divisions of are depicted in the index map (Fig. 1). 2.0 Rainfall & Climate

Average annual rainfall (1971-2012) of the district is 445.4 mm. However normal rainfall for the period 1901 to 1970 is 400.6 mm. The annual rainfall gradually decreases from southeastern part to northwestern part.

Climate of the district is dry except during SW season. The cold season is from December to February and is followed by summer from March to June. Period from mid of September to end of November constitutes post monsoon season.

The district experiences either mild or normal drought once in two years. Severe type of drought has been recorded at Ahore block. Most severe type of drought has been recorded at Bhinmal, Sanchore & Jaswantpura blocks.

3.0 Geomorphology, Drainage & Soil type

The district is characterized by landscape of alluvial plains of hill ranges, and isolated hillocks. Jalore district has almost an even topography in its western section, the lowest point being around 17.0 meter above mean sea level and is marked by sand dunes. The sand dunes trend NE-SW, indicating prevalent wind direction in the area. The eastern section is dominantly hilly, forming the flank of range and the highest point is 991 m above mean sea level (amsl). The elevation of the area ranges from more than 600 m amsl in the east to 75m amsl in the west at the confluence of the Luni and Jawai-Sukri Rivers. Generally the terrain slopes westwards. The valley floor has an area elevation ranging from 60m amsl to 215m amsl. The hill tops are normally shaped by weathering phenomena, which have caused tors and boulders of various shapes and sizes. These features are well developed in the eastern part of the area. In the mid eastern and western parts, sand dunes are a common topographic feature. Jalore district is often called “Delta of West ” and all the principal rivers of western Rajasthan flow through this district.

The review of the geomorphological study carried out by the Central Arid Zone Research Institute (CAZRI) 1966 has shown that the whole of the Luni drainage system can be classified into 7 geomorphological divisions viz. dissected plateau, Jalor-Israna- Rewara granite rhyolite Inter-fluve with intervening plains, The Khari-Bandi-Sagi river plains, North and North-east alluvial plains, Pachbhadra salt basin, Western plains with dunes, Flood plains of the Luni and Jawai-Sukri drainage systems.

Geomorphologically, the alluvial valley floor belongs to mature landscape system and present landform units are the products of the past meandering courses and wide flood plains. Additionally, there are innumerable old channels buried under wind blown sand. 3.1 Drainage Jalore district falls in parts of Luni basin (82.8%), Other Nallahs (16.9%) and Outside Basin(0.3%). Tehsil wise distribution of basin area is given in Table Table: Tehsil wise distribution of basins

Sl.No Name of Tehsil Area in Sq. Km. Luni Other Nallahs Out side

1 Ahore 1536.4 - -Basin 2 Bhinmal 2653.6 - 4.1 3 Jalore 2277.2 - - 4 Raniwara 494.9 - 513.8 5 Sanchore 1857.9 33.9 1286.8 The Jalore district forms a part of the Central Luni Basin and is drained by the Luni drainage system, which passes only through the southwestern tip of the district near Sanchore before shedding its load into Runn of Kutch, originating from the Aravalli hill ranges. The main rivers in the district are Jawai, Sukri, Khari, Bandi and Sagi, which are tributaries of the and form a trellis pattern of drainage flowing due northwest. All rivers are ephemeral with graded and meandering courses and wide flood plains.

3.2 Soils & Irrigation Practices

Soils are shallow with deep gravel encrusted with CaCO3. The texture of the soils in general varies from sandy to sandy loam but in deltaic areas of the Luni River south to southwest of Sanchore, the soils are loamy alluvium. The pH value ranges from 7.0 to 9.0 and in general, the soils have a higher pH. The of the soils can be broadly described as fine-sorted sand on the dunes and coarse to medium textured soils on the plains with a tendency for increase in fine particles. The soils in the eastern part of the district are shallow, covering partly weathered rocks and calcareous gravelly material. Soils along the hill slopes are also mostly shallow consisting of weathered rock and calcareous gravelly materials. The fertility status of the soils in general is low and the proportion of organic matter varies from 0.2 to 1.0 per cent.

Geology

Only 5 to 10% of the district reveals exposures of different rock types and the remaining area is covered by a thick blanket of sand and alluvium. The metasedimentary rocks such as phyllite, schists, and quartzite belonging to the Super Group (1,400 to 1,650 million years old) occur only as inclusions within the dominant granites and rhyolites. The pink Jalore granite occurring near Jalore town is the most common type of granite in the district. The older grey granite is rare. The Malani rhyolite and the associated agglomerate, volcanic ash, felsite etc. occupy west of Roja Bhaker and Lakawas and also in the, north eastern parts of the district. These rocks represent a large scale ancient volcanic activity on the Indian sub continent and have been estimated as about 745 million years old. Dykes and veins of dolerite, granite porphyry, applite etc.. also occur at places.

The rock types found in the district are given as below:

Recent to Sand, alluvium etc. sub recent Malani rhyolite Intrusives Post-Delhi- and Jalor granite extrusives. Erinpura granite Mineral Resources

The following are the rocks and mineral resources of Jalore district:

Fluorspar

Fluorspar is an important industrial mineral valued for its calcium fluorite (CaF2) content, and is the only major source of fluorine. It is chiefly used in the manufacture of hydrofluoric acid and other fluorine chemicals, as a flux in steel making and as an opecifier and flux in the ceramic industry. Fluorspar is an essential raw material for manufacture of aluminium fluoride (AlF3) and artificial cryolite (Na3 AlF6 ), which are used as flux and electrolyte in the production of primary aluminium.

The state department of Mines & Geology has discovered a fairly large deposits of fluorspar near Karada of Tehsil Bhinmal, during the field season of 1974-75. Fluorspar and Baryte-occurrences have been discovered for the first time in Malani volcanic suit of rocks which were known to be barren so far.

Mineralisation occurs in an area of 21 sq. km. (confined in 17 small hillocks) in Malani volcanics represented by agglomerates, rhyolites, trachytes and basalts, in the form of massive to thin veins and stringers as fracture and joint filling. As a result of detailed investigation (by trenching and pitting) done by the State Department of Mines & Geology, the total reserves of fluorspar are estimated to be 0.173 million tonnes of 51.9% CaF2 grade out of which about 70,000 tonnes are 80-95% CaF2 content. Veins of baryte and calcite also occur along with fluorite in Karada area. The area is leased out to RSMDC. The main activities of mining are located at Krisna hill, Rekha hill & Santoshi hills. The production during 98-99 was approx. 10 tonnes.

Granite

The granite rocks which have, rather become the economic assets of the district, belong to the Malani System of rocks. The Siwana and Jalor granites provides rocks of high fassinating colours ranging from flesh to pink and light colours. Pink and grey granite capable of taking good polish is found in abundance in the district. Details of the important areas of granite in Jalore & its quality is discreted in the table no.1. A granite polishing factory for making polished slabs was set up by the Rajasthan Government at Jalor which was transferred to R.S.M.D.C in 1970.

Beside R.S.M.D.C., there are number of areas and more than 153 leases of granite in private sector.

List of Granite mines in Jalore District: S.No Near Village No. of Mines 1. Nabi 6 2. Mahaliwas 8 3. Bhetala 6 4. Barlawas 4 5. Dhavla 7 6. Kalaghata 3 7. Devda 1 8. Safada 1 9. Keshwana 4 10. Pijopura 3 11. Muri 5 12. Birbalsar 4 13. Ledermer - 14. Tavab 5 15. Raniwara Khurd 8 16. Lal Ji-Ki-Dungri 1 17. Desu 1 18. Ratanpura 2 19. Khambi 16 20. Kavala 19 21. Tavab (A) 7 22. Tavab (B) 19 23. Kot Kasta 1 24. Bala 10 25. Borta 6 26. Leta 1 27. Namawas 1 28. Nosra 1

Besides above, building stones and masonary stones, Bajri etc. have been produced in the District for local use.

Clay

Clay occurrence has bee reported near village about 48 Km. north east of Jalore town. Another occurrence of clay deposit is reported at Pal.

Bhadrajun clay is found in Rhyolite of Malani volcanic soil. It is white in colour and gritty in nature. The chemical analysis indicates 70% free silica with 14-15% alumina. In the area 0.2 million tonne reserves were assessed.

Saltpetre

Village Kanwla in Tehsil has deposits of saltpetre within an area of about 1.9 . The area was previously leased on fixed royalty basis. Local persons were employed there for crude refining of saltpetre which is used for local pottery and fire works and ammunitions industry.

Gypsum

Gypsum deposits are located near , chawarda in Ahor Tehsil and at number of places in Sanchore Tehsil. Ramsin and Sayar-ka- Kasita area is already leased out to M/s R.S.M.D.C. Other small deposits are located near Vediya, Chittarwana, Sewada, Hemagura and Haryali area.

Besides above, building stones and masonary stones, Bajri etc. have been produced in the district for local use since long back. Small granules of the grey and brown rhyolites are widely used in mosaic flooring.

Serpentinised dolomitic marble is known to occur near village Rupi, 9.5 Kms. south west of Bhinmal. Minor occurrences of graphite and feldspar has also been found in the east of Bhinmal town.