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Nilanjan Bhowmick AIR 3, CSIR NET (Earth Science)
Rahul kumar Best Answer
Cross beds are sedimentary structures form as a result of ripple propagation. Sediments are carried along the stream and due to reduced flow velocity in Lee side, they got deposited over that. Repeating the same process again and again leads to the formation of cross beds. For better clarification you can look at the attached figure. Figure shows the formation of cross stratification clearly. Feel free to ask if you have any doubt.
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sir in my question. it shows cross bedding of sandstone. how it is
Cross bedding is most common feature in sandstones. Sands are transported all the way from stoss side to Lee side and due to reduced flow velocity along lee side, they got deposited as a cross laminate of the ripple, which in turn upon preservation lead to the generation of cross beds.
okok ty sir
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sir can we say... except this pattrn....any other patterns of deposition will be considered as cross bedding?
Cross bedding form always at an angle to the bounding surfaces. For your reference, I have attached a figure which contains different types of cross beddings.
ty sir.