the asthenospheres size is 1654
It's your shoe size in the United Kingdom.Because the United States uses the older, outdated imperial system, while the United Kingdom uses the modern, updated metric system, the measurements are different.UK and US shoe size comparisons:UK Size 2 = US Size 4.5UK Size 2.5 = US Size 5UK Size 3 = US Size 5.5UK Size 3.5 = US Size 6UK Size 4 = US Size 6.5UK Size 4.5 = US Size 7UK Size 5 = US Size 7.5UK Size 5.5 = US Size 8UK Size 6 = US Size 8.5UK Size 6.5 = US Size 9UK Size 7 = US Size 9.5UK Size 7.5 = US Size 10UK Size 8 = US Size 10.5
well im from the US and I'm a size 0 here and would be a size 4 in the UK. that means that: US Size 2 = UK Size 6 US Size 4 = UK Size 8 US Size 6 = UK Size 10 US Size 8 = UK Size 12 US Size 10 = UK Size 14 US Size 12 = UK Size 16 - so a UK size 8 would make you a us size 4! ~beelover
European shoe size for Men = size 40 UK size 7 European shoe size for Ladies = size 40.5 UK size 7
Size 13 is a junior size as opposed to a woman's size. I would think a size large.
what is the average shoe size for women in the philipines
womens size 26 in jeans what size is that in mens pant size
a size 6
size 28...one size bigger than size 27
his shoe size is a size 8
Can you convert size 3XL in European size
comprise of tectonic plates which floats to each other it contains more than crust and it is made up/divided into two oceanic crust where it ranges from 50-90km in thinkness and continental ranges from 40-210km and below it is Asthenosphere that contains high viscousity that allow it to move slowly anddoes it transfer heat to lithosphere via convection being responsible as process for the movement of tectonic plate and Asthenospheres ranges from 100-200km and it's depth upto 4020km
The asthenosphere is unusual because it is a semi-fluid layer within the Earth's upper mantle, exhibiting properties of both solid and liquid states. It allows for the slow movement of tectonic plates due to its partially molten nature, which contrasts with the more rigid lithosphere above it. This unique state of matter is crucial for geological processes like plate tectonics and volcanic activity. Its behavior is primarily governed by temperature and pressure conditions, leading to its distinctive flow characteristics.