Jammu Landslide, Rock Slope classification

A note on  assessment of Rock Slope stability in the field based on SMR,  a case study at Ramban to Banihal highway poject Km 164+800, Jammu and Kashmir

 1. Introduction and Geology: The existing Jammu to Srinagar highway connect Srinagar to Jammu and India which play a crucial role in the field of land transportation. It is a very critical stretch having steep and rugged terrain. Granitic gneiss rock at the above said stretch belongs to Salkhala formation of Precambrian age. Grey to dark grey granitic gneiss is well exposed along the existing road with intercalation of quartzite and thinly layered mica schist. Medium to coarse grained granitic gneiss is well compacted, massive and partially weathered on surface with normally dry to wet water condition. Rock slope at this location is having an angle 60 to 80 degree, facing towards N 265-280 degree. 

2.   Rock Mass Rating (RMR):Rock mass classification (RMR) system is introduced by Bieniwaski in 1976 in details to classify the rock class based on  geo-mechnical characters in the field. This system is refined latter in 1989 to estimate the strength of the rock mass. The following six parameters are used to classify a rock mass based on values and rating (0 to 100): 

a. Uniaxial compressive strength of rock material. b. Rock Quality Designation (RQD). c. Spacing of discontinuities. d. Condition of discontinuities. e. Groundwater conditions. f. Orientation of discontinuities. The field data have been collected from sites which are as follows:

     

    Granitic gneiss consisting three sets of joints including one sets of random joint. Most prominent foliation joint is directed toward NE with moderate dip angle. 2^nd set of joint is directed opposite to foliation joint with moderate to high dip angle. Third joint set directed perpendicular (SE and NWW) to foliation with high dip angle. Sometime it is almost vertical. Joint planes are partiality weathered, plane rough and open at surface. Persistence of joint sets is moderate to high. Based of field data, granitic gneiss is classify as below at this location.

Jobs in Geology, What can i do after degree to get a Jobs

In the field of Geology there is no more option to get a job in geological field after graduation but if you can go for master degree o higher study than there is many job options like government job as well as in private field. you can apply like GSI, ONGC, UPSc, academic field in government sector and there are many private organization too which have selected geologist, mineralogist, Geophysicists, engineering geologist every year.

Major Challenges in Indian agriculture these days

Major Challenges in Indian agriculture these days:

As we have knows that around 70% of Indian population is depend on our agriculture. But our government spend only less than 10%  of total budget. So the government have not taken correct initiative which directly affect the actual ground. In the other hand the Minimum support price is also not as per ground reality. Indian farmers literacy rate is very low which is major concern to Indian agriculture. The banks are not providing KCC loan to the farmer without hidden service charge which may be up to 10% of loan amount. We must treat a farmer as a businessmen and convert the agriculture as a business. Farmer will be free to decide his product MRP cost based on input price. If the government make proper policy for farming sector it can contribute more 30% in our GDP. 

Construction process after Piling work

Ans. Construction process after Piling work: If you are completed piling work than fist of all pile load test will be conducted on the piles to check the desired SBC. Then the raft work will be carried out on pile for construction activity. Further the other construction activity will be carried out.

Coal Mine in Mangolia

Coal mine in Mangolia:

Mangolian has 8- 10% of the world"s coal reserves. Five hill coal reserved in Mongolia is the largest coal deposit in the world which is yet to be exploited, belong to southern Mangolia. Currently Tavan Tolgoi is the largest mine where the production is going on. The coal grade of this mine belongs near to the anthracite. Oyu Tolgoi, Khushuut and Nuurst Khotgoe are another famous coal mine in Mangolia.

A Geological overview of Ramban to Banihal Highway, Jammu and Kashir

Report on a Geological Overview of Ramban to Banihal Highway Project, Jammu and Kashmir

1.       Introduction:

Ramban to Banihal highway project is a most difficult part of NH-1A (NH-44) due to very rough topography with a steepest terrain on Jammu to Srinagar highway, this is vital for providing connectivity between Ramban to Banihal. The Geological condition is very complex in this section due to past tectonic activity. The total length of the project is 36 km from Km 151+000 and ended at Km 187+000, including 06 major bridges, 21 minor bridges and 6 Tunnels.

2.       Geology of the Project area:

During the field work it has been observed, from Ramban to Banihal metamorphic rocks are exposed along the project highway. These exposed rocks have undergone moderate to high temperature and pressure condition due to Murree thrust, Makarkote thrust and Panjal thrust. At some places, intrusion of granitic rock have been observed near Panthal and khuninallah area. Two local thrusts have been encountered named as Digdole and Magarkote thrust, at Digdole and north of Ramsu respectively. From Ramban to Banihal, there are numerous Shear zone/seams are present which generate rockfalls and slides along the highway on steep hill slopes in the project area. The area from where project highway starts km.151+000 is highly sheared and fractured.

Stratigraphic sequence of the project area (Bhat, et al.,1999)

 The rocks of Salkhala group are exposed along the highway, comprises foliated slate, phyllite, quartzitic phyllite dolomite form 151+00 to up to km. 169+00. Salkhala group is divided to salkhala formation, Ramban formation, sinchua formation and Baila-Gamir formation. Ramban formation comprises slate, phyllite, dolomite and quartzite, highly jointed and sheared at some places (At T1 and T2 tunnel) due to effect of Panjal thrust as well as Muree thrust. Muree thrust separates murree group of rocks to metamorphic rock near Ramban  which is parallel to the Chenab river. Ramban formation is tectonically overlain by salkhala formation near Digdole. The Granitic rocks are exposed near Khuni nallah next to Digdole ut to Magarkote. Further next to Magarkote km.169+000, the rocks of Ramsu formation are exposed along the highway comprise a highly compressed unit of phyllite and phyllitic slates, quartzite. Ramsu formation is separated tectonically from salkhala formation by Makarkote thrust at km. 170+000.  It is recorded unfossiliferous till date. The rocks of Ramsu formation are exposed between Makarkote to Sherbibi along the project highway. Ramsu formation has micro folds due to thrusting activity over salkhala formation. Further from Km. 181+000 to up to end of the project 187+000, the rocks of Chamalwas formation are exposed which comprises greenish grey slate, quartzite, metasandstone and metasiltstone which is uncomfortably overlain by syringotheris limestone. The Chamalwas formation is also unfossiliferous like Ramsu formation.

Lothological Strip Chart along Highway

1.       Structures, Bridge, Retaining walls foundation and Tunnels:

As we have know this area falls under the youngest mountain chain of the world and most difficult zone of Jammu to Srinagar highway due to its geomorphology and geological complexity. The lithology of the project area is metamorphic sequence which is fresh to highly weathered in nature shows intense shearing, fracturing and folding at at some locations (Ramban, Digdol and Ramsu, Nachilana area).

Mom Passi, Highly Steep Terrain with Complex Geology

 There is need to design and execute the foundation work of structure carefully.  During execution of shallow open cast foundation of bridges, geological logging of the foundation area needs to be carried out properly and if found any shear zone/seams should be treated by dental treatment as per the standard (IS:11973, 12070). At some places the nature of rock strata is noticed as poor to very poor rock (Class C, highly jointed, weathered with open joint). Such foundation location should be noticed carefully and foundation improvement to be carried out before laying the PCC by fully grouted anchoring or cyclic grouting method, if required as per IRC or IS standard (from Seri to Battery Chasma MNB at km.153+900,156+070 and 157+970, MJB 161+300).

The foundation which will be cast over a steep slope, the edge distance, frustum of bearing etc. should be checked as per IS 1904,13063 and IRC 78-2000. Excavation for open foundations should be done after taking necessary safety measures for which guidance may be taken from IS: 3764.The foundation protection work related to structures on a steep hill slope noticed carefully at the time of design and execution and kinematic analysis and further modeling needs to be carried out to check the stability of foundation as per the site condition and codal provision. The area from Maroge to Makarkote is the steepest area of the project so special attention needs to be required in this area (Bridge at 153+900,160+300 and 169+060).

At Tunnel 1, 2 and 6 the rock mass is noted as highly jointed and moderate to high weathered slate/phyllite/schist rock including Dolomite. Which belongs near to class C as per the rock mass classification, so proper attention is to be required to design the portal face and tunnel support system based on assumed and field parameters. 

Highly Jointed and Sheared Granitic Schist at Panthal Tunnel Portal

The rock strata at Tunnel 3, 4 and 5 is better with compare to tunnel l, 2 and 6 known as granite/ granitic gneiss (eccept few meter sheared zone at panthal). The Rock strata of this stretch belongs to class A-B of the rock mass classification, moderately jointed and fresh in nature except Panthal bridge location where poor quality of rock mass is observed up to few meters along the tunnel axis both side from center of nallah. At this location weathering and shearing effect have been observed on right bank of panthal nallah up to few meters inside the hill slope. During excavation of tunnel a detail geological mapping including 3-D face logging should be carried out after every cycle of excavation on a scale 1:100 or 200 and if found any deviation in designed data to be communicated to designer to improve the support system and value engineering. The over breaking should be noticed carefully and blast design updated accordingly. Blast design is exercised properly in each type of rock mass for tunneling work as well as for cut slope excavation works.

2.       Road Cut Slope Stability Or Slope Protection works:

As the terrain of the project is through the mountainous region, various protection works, such as revetment walls, rock net and special slide protection works to be required to stabilize the slope. The slope protection works will be mainly soil slope, soil-rock slope and rock catch type. 

Highly Steep Cut Slop required correct Protection measures

For a soil slope, soil nailing, revetment wall (180+000 to 184+000) or stone masonry walls can be used to protect the slope including bioengineering method such as hydro seeding to control surface erosion by quick vegetation development. For highly fractured rock mass, the revetment wall can be applied to protect the slope as per the site condition, if the height of the wall is more than 6 meters the strength parameters to be carried out for the wall foundation (Ramban formation, Ramsu formation and soil strata). Where the slope is stable but surface instability is occurred  due to shooting stone with deferent size of rock pieces, rock net and rock catch fence to be installed as per site condition and contract agreement (Battery chasma to panthal nallah, khuni nallah and magarkot area). In the special protection works such as planer, wedge and toppling failure (Km.170+000 to 178+000 and Km.186+000 to 187+000 ), we can stitched the jointed rock mass by  fully grouted rock anchoring, dowelling with or without shotcrete as per site condition but detail  kinematic slope stability analysis (day lighting case)  should be carried out to check the failure mechanism and FOS. Further we can confirm these results with continuum and discontinuum modeling in details if required. (Digdole,khuni nallah,panthal, Magarkot, Sherbibi and 186+000 location).

The Slope geometry, rock type and shear strength parameters should be checked properly in the field with design and drawing before executing the work of cut slope and if found any deviation in rock type, class and cut slope angle, protection measures must be updated accordingly.  During the cut slope activity at km183+600 to 184+600 and 177+300 (SB), mass movement (creep movement) has been observed due to excessive cut height, toe cutting of the slope, needs to be protected.

3.       Major Landslide at Highway:

Several landslides have been encountered at Ramban to Banihal project highway, named and chanaige as follows:

·         Seri Landslide                                       Km.151+300

·         Landslide at Khuni nallah               Km.162+800

·         LandSlide at Panthal Bridge        Km. 168+600

·         Ramsu landslide                            Km. 172+600

·         Landslide at  Ratanbas               Km. 176+100        

                                                                                               

Landslides are natural phenomena and occurred due to natural forces as well as manmade activity like improper excaation. As we know this area exists in zone IV on earthquake zonation map of India. The topography of this area is very roughed and geologically very complex in nature. When the degree of weathering (physical, chemical and biochemical) is increased and strength parameter of rock mass is decreased as the time passes away. When the shear strength parameters of the rock mass are reached at peak value due to natural or manmade forces, slope fails in continuum or discontinuum materials. Most of landslides of the project area are governed by discontinuities except Seri landslide. The material at Seri Slide is highly crushed and seems to continuum in nature. A brief description of major slides along the alignment and  location view is being presented below:

·         Seri Landslide:   landslide is encountered at Km 151.050 and occurred in sheared and highly crushed rock mass (slate and phyllite) which is continuum in nature.The rock mass fails during monsoon seasons due to decrease in shear strength parameters of rock mass while pore water pressure increased (saturated condition).

Seri Landslide

Deep seated failure has not been observed but it is a large slide. For the protection measure we can used gabion wall or reinforced wire mess grid at this location with bioengineering method such as seeding root mat or hydro seeding as per the site condition.  Location of all current slide https://www.google.com/maps/d/edit?hl=en&mid=1kG4dcr-_JQQmJybqIu45ttv3rmrH942Z

https://www.google.com/maps/d/edit?mid=1kG4dcr-_JQQmJybqIu45ttv3rmrH942Z&usp=sharing

·         Khuni nallah Landslide:  Khuni nallah landslide is located at Km 166+200 just before the bridge. This landslide is governed by discontinuity. It is occurred due to road widening/toe cutting with a combination of planar, wedge failure within the rock mass.

Landslide near Khuni Nallah

The rock type of this area noted as phylitic, granite dipping towards the highway (daylight at some location). For control measures of this landslide we can use rock catch fence with rock net. As we have observed, this landslide produces different size of rock boulders so that the rock catch fence to be design after knowing the trajectory path and kinetic energy of the detached boulders. 

·         Panthal Nallah  Landslide: 

This landslide is located just after the Panthal  bridge at km 168+700. The area is noted as moderately jointed granitic gneiss with steep slope. The nature of this slide is governed by kinematic mechanism and required slope

Landslide at Panthal Nallah

 protection as trimming of the slope, rock netting with rock bolting. The stone masonry wall, revetment wall can be used at the bottom of the slope. Before finalizing the rock net kinematic analysis should be carried out to know the mode of failure and protection works to be decided and executed accordingly.

·         Ramsu Landslide:   This landslide is located at km 172+600. It is most prominent landslide in the project area and occurred due to widening of existing road and complex mechanism of failure due to Magarkote thrust. The rock type of this area is noted as highly compress sequence of Phyllite, carbonaceous slate, dolomitic and siliceous limestone including quartzite of Ramsu formation. 

Ramsoo Landslide

This area is highly sheared, fractured and folding to Makarkote thrust. For the control measure of this landslide we can use reinforced gabion wire mesh grid at the bottom of the slope. Loose rock pieces/rock boulders must be removed by trimming and rock net to be used with geo-mat from top of the slope (crown) up to the gabion wall top. The rock bolting can be used to improve the shear parameters of the rock mass but before finalizing special protection a detail kinematic analysis of the slope, slope 2-D face logging, and subsurface parameter of rock mass needs to be carried out.

·         Landslide at Ratanbas:   This landslide is located at Km. 181+400 near Ratanbas area. It is occurred due to planar and wedge failure in carbonaceous slate and phyllite. Rock mass is moderately weathered.  

Landslide at Ratanbas area

Slope failure is occurred along closely spaced and steeply dipping joints as a planar and wedge mechanism due to the intersection of adversely-oriented joint planes. For control measure of this landslide first we can need to redesign the slope face geometry and remove all loose materials from rock slope then we can use rock bolting with rock net and shotcreting. A detail analysis should be carried out before finalizing special protection measures as 2-D slope face logging, subsurface parameter of rock mass.

1.      Conclusion:

As we have noted that the topography of this section is extremely rugged including steep hill slope. The area is witnessed two major thrusts known as Digdole and Makarkote which is tectonically active till date. It is also noticed mostly length of the project covered by slate, phyllite and schistose rock mass wherever these rocks are highly weathered and jointed at places may leads to problems in both cases, slope protection as well as structures foundation stability. Special attention is to be required during execution of cut slope excavation, tunnel portal face as well as foundation excavation. At Seri,Ramsoo and Ratanbas  landslide locations, we can also go for square half tunnel with inclined roof top but the applicability of this type of structure is a matter of technical and financial discussion. These types of structures are successfully adopted in the country for highway protection from unexpected fall, avalanche landslide on highway. At the location of Maroge, Digdole and Makarkote bridge, foundation will be on a steep slope, an excessive excavation will be required to layout the foundation on steep slope, is not good for foundation stability. So we can go for pile foundation in rock on steep slope, if required. The tunnel 3,4 and 5 will be executed as rock type seems fair to good but special attention will be required for execution of Tunnel 1,2 and 6.    

  

How to identify Rocks in Field

1. Identification Of Rock in the Field: 

Broadly we have categorized the rocks in the field in two classes for identification point of view: 

i) The rocks which give Fizzes with acid  like limestone and Marble

ii) The rocks which don"t fizz with acid

Rock Classification in the Field

First we identify the rock above said parameters and if the rock dont fizz with acid then further devided in three parameters which dont fizz with acid as below-

a) Rocks made of very fine grains rock which are soft and crumbly-  (SHALE or MUDSTONE)

b) Rock made of Rounded grains- if small rounded sand like grains (SANDSTONE)
                                                    - if rock have large rounded pebbles (CONGLOMERATE)

c)Rocks made of Crystal grains which are tightly held together in close filling pattern- this is further decided in two class - 1.Grains are not arrange in layers: Pale colour with large crystals (GRANITE)
                                                                       Dark colour with small crystals (BASALT)
           
                                      2. Grains are arrange in layers: * White colour very hard rock, drived due to                                                                                                            metamorphism of  sandstone(QUARTZITE)
                                                                                           * Grey or purple colour very hard brittle in nature                                                                                                     and splits in to thin sheets drived due to                                                                                                              metamorphism of shale/mudstone(SLATE)
                                                                                          * Silver colour with flaky grains (Schist)
                                                                                        *Rock having alternate dark and light bands (GNEISS)

Hope you will broadly identified the rock in the field based on these parameters.

         

The word ‘GURU’ has its roots in the Sanskrit language, where ‘gu’ means darkness and ‘ru’ stands for the removal of darkness. This day first time comes in word when the Lord SHIVA or First YOGI introduced Saptarishis, the seven celebrated sages. 

GURU PURNIMA_ Lord Shiva and Maharishi VYASH

Day fifteen of Ashadh Sukla is called GURU Purnima. On this occasion we have worship of our Guru who provide us the knowledge about this mighty world and who truly introduce us to our self. This day is celebrated on the name of Maharishi Vayas who wrote the Mahabharata. He was also wrote our all four Vedas. Guru Purnima is in honour of the guru in the form of yogis and sage who help an individual connect on a spiritual level.  On this Guru Purnima the largest Moon ellipse is also can be seen which can be observed in night on 27.07.2018.

Our all Garanthas told us about the importance of GURU. Our life can not be successful without a True GURU. We can differ in views and opinion about God but not to Guru. In India all religion accepts the importance of GURU. So wish to all of you, a Happy Guru Purnima. 

GIS based spatial data analysis for landslide susceptibility mapping in Indian Himalaya
https://www.researchgate.net/publication/225909360_GIS_based_spatial_data_analysis_for_landslide_susceptibility_mapping

Road subsidence at km. 104 Kud-Patnitop, Jammu and Kashmir,

Road subsidence at km. 104 Near Kud-Patnitop, Jammu and Kashmir, Prepared by Pushpendra Kumar, Deputy Manager, Geology,  Rodic consultants Private  Limited, RAMBAN-BANIHAL

Disclaimer: Any part of this report should not be used, updated in any form without the prior permission of the Author.

This report included the following CONTENTS

1. Introduction 

2. General Geology of the Site

3. Visually Inspection of Site and Problem observed

4. Proposal for Stabilization Measures

5. Conclusion

1.Introduction: Cheneni to Patnitop highway passes through rough and steep terrain of lower Himalayas. The kud land slide location falls at 33°05´ 15.04”N and 75° 18´ 8.6”E at km 104 on Cheneni to Patnitop highway. Geologically the area falls under Muree structural belt of Lower Himalayas which is named on Muree, located in Pakistan. The area is tectonically very sensitive due to Muree and Panjal Thrust and very prone to slope failure during snow time and rainy season.

Subsidence at Jammu to Patnitop Highway, Lower Himalaya

2.General Geology: General Geology of the area belongs to rocks of Lower Muree formation comprises a sequence of interbedded sandstone and siltstone/claystone layers, Lower tertiary in age. The tectonic domain of this area is bounded by main frontal thrust (MFT) in south and main boundary thrust in north (MBT). Along the nallah, red clay stone is exposed which is highly weathered on surface and much fined grained. The Rock exposures along the nallah have dipped towards NE direction. The strike of rock unit is sub-parallel to the nallah and road at this location.

Sequence of interbedded sandstone and siltstone/claystone 

This the Arial view of the site which is prepared with the help of google map. The map shows the existing protection works related to old slide. The main causes of this subsidence exactly decided after details Geo technical investigation but at the site it seems that it is triggered due to toe cutting of the slope by flooded water during monsoon.

Arial view of Site from Google Map

3.Visually Inspection of Site and Problem observed: The site have been visited on June 26,2018. It have been observed that the area is under slope instability from long time and some protection measure already adopted at this location as concrete retaining wall and Gabion Wiremesh structure. The current subsidence is occurred due to Toe erosion/Scouring of bed level in the nallah during rain. Due to toe erosion of side slope of the nallah, the creep movement is triggered. Tilted tree at the slope is an indication of slow mass movement at this location. It is also define the lateral boundary of creeping area.

Rain Cut Below  foundation Of RCC cladding wall

Above photograph shows the toe cutting of existing wall due to flood water on bed level. It should be repaired immediately to avoid further damage to the road.

Second problem is observed at existing Culvert and culvert return wall which are damaged badly due to erosion of exposed clay stone. Some cracks are already noticed at floor and side wall of the existing culvert. So it is immediately needs to be repaired without further delay.

Damaged Culvert and Guard wall

     Photograph shows the cracks which are developed at floor and side wall of the culvert.

Cracks developed on the floor and wall

4.Proposal for Stabilization Measures: There is two action are required immediately at site to escape further damage of road and Culvert. First the culvert foundation needs to be repaired immediately including supporting wall next to return wall. And second are the bed rock investigation to know the exact sub surface strata and depth of failure plane within creeping area.

After decided the creeping plane we can installed micro pile to stop the creep movement within the existing strata.

On the other hand we should remove all loose materials. The eroded bed level of nallah should be filled by boulders/Pebbles with help of gabion wire mesh up to desired level and plug its top with lean concrete to support the eroded  toe of the slope at creeping area. As well as toe of retaining wall should also be repaired. The top of the gabion structure or boulder layer must be plug perfectly with lean concrete to prevent the seepage/ingress of water within the bedding strata. The Side wall throughout the nallah must be constructed to proper channelize the water flow in desired direction.

5.Conclusion: It is concluded that the subsidence on road is occurred due to toe cutting of the slope by rain. The following measures should be required at this location-

1. First the Cracks of culvert and retaining wall must be repaired without further delay.
2. Cracks on the road should be filled with lean concrete without further delay.
3. A Bore hole should be conducted at failure slope to know about subsurface strata and creeping plane.
4.  The eroded bed level should be retained up to desired level to support the slope base and toe of retaining wall.
5. Side wall within the nallah should be constructed to proper channelized of water flow.
6. Loose materials on the slope should be removed and geometry of the slope should be updated.

References:

                     •         IRC:78-2000, Standard Specification and code of practice for road bridges

                 •        IRC:SP:48-1998, Hill Road manuals

                     •        Duncan C. Wyllie & Christopher W. Mah, Rock Slope Engineering

                 •        https://www.google.com/maps               

                 

                   

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Subsidence on Highway

https://youtu.be/fG-2r2910mw

*श्री कृष्ण -राधा जी और रुक्मणी

एक दिन रुक्मणी ने भोजन के बाद श्री कृष्ण को दूध पीने को दिया।

दूध ज्यदा गरम होने के कारण श्री कृष्ण के हृदय में लगा और उनके

श्रीमुख से निकला- " हे राधे ! "

यह सुनते ही रुक्मणी बोली- प्रभु !

ऐसा क्या है राधा जी में, जो आपकी हर साँस पर उनका ही नाम होता है ?

मैं भी तो आपसे अपार प्रेम करती हूँ,

फिर भी, आप हमें नहीं पुकारते !

श्री कृष्ण ने कहा -देवी , आप कभी राधा से मिली हैं ?

और मंद मंद मुस्काने लगे..

अगले दिन रुक्मणी, राधा जी से मिलने उनके महल में पहुंची ।

राधा जी के कक्ष के बाहर एक अत्यंत खूबसूरत स्त्री को देखा.

उसके मुख पर तेज होने कारण उसने सोचा कि ये ही राधा जी है

और उनके चरण छुने लगी !

तभी वो बोली -आप कौन हैं ? रुक्मणी ने अपना परिचय दिया

और आने का कारण बताया.

तब वो बोली-

मैं तो राधा जी की दासी हूँ।

राधा जी तो सात द्वार के बाद आपको मिलेंगी !

रुक्मणी ने सातो द्वार पार किये और,हर द्वार पर एक से एक सुन्दर

और तेजवान दासी को देख सोच रही थी क़ि अगर उनकी दासियाँ इतनी

रूपवान हैं, तो राधारानी स्वयं कैसी होंगी ?

यह सोचते हुए राधाजी के कक्ष में पहुंची, कक्ष में राधा जी को देखा-

अत्यंत रूपवान तेजस्वी जिसका मुख सूर्य से भी तेज चमक रहा था।

रुक्मणी सहसा ही उनके चरणों में गिर पड़ी...

पर,ये क्या राधा जी के पुरे शरीर पर तो छाले पड़े हुए है !

रुक्मणी ने पूछा- देवी आपके  शरीर पे ये छाले कैसे ?

तब राधा जी ने कहा- देवी !

कल आपने कृष्णजी को जो दूध दिया था,

वो ज्यदा गरम था !

जिससे उनके ह्रदय पर छाले पड गए..

और, उनके ह्रदय में तो सदैव मेरा ही वास होता है.

इसलिए कहा जाता है बसना हो तो...

'ह्रदय' में बसो किसी के,

दिमाग' में तो..

लोग खुद ही बसा लेते है..!