yhh pj nu oil do eh dhili hoyi aa :hello: :hello: :hello:

3.lado rani jis tym marji dekh laoooooooo fight fight karna esi da kam hai but god mera naal esi ne fight nhi kiti kade viiiiii n he rahe lado to rabb he bache

 :sad: :sad: haww ma kad kise naal fight kiti  :sad: :sad:

vase jattie ah topic ma phyla hi banya c uthe update kar dinde  :candies: :candies: :candies:

3rd is nyc  :okk: :okk: :okk: kudrat da posts dekh ka sonnen da posts cheta aa janda

ana gana na suna bola ho jana tuci

well pata nhi yar ih roz da kam a ya nhi ..dis is da reason main chat ch nhi jandi.....ell oh kudi ta gaye so hun ki hona a

la kise toh kada darna je koi 1 kadda gal tuci 4 kad dayo  :he: :he:

nackchadu ah ta roj da kam c itha

chal vadia chat te hun jaya na karii

A roll cloud -  These rare long clouds may form near advancing cold fronts. In particular, a downdraft from an advancing storm front can cause moist warm air to rise, cool below its dew point, and so form a cloud. When this happens uniformly along an extended front, a roll cloud may form. Roll clouds may actually have air circulating along the long horizontal axis of the cloud. A roll cloud is not thought to be able to morph into a tornado. Unlike a similar shelf cloud, a roll cloud, a type of Arcus cloud, is completely detached from their parent cumulonimbus cloud. Pictured above, a roll cloud extends far into the distance in 2009 January above Las Olas Beach in Maldonado, Uruguay.

woww nycc view bt its weird

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bandro tenu ta chadya v naii  :angry: :angry: :angry: