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Science Zip Pouch featuring the photograph Hailstone, 1953 by Science Source

Boundary: Bleed area may not be visible.

The watermark at the lower right corner of the image will not appear on the final product.

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Hailstone, 1953 Zip Pouch

Science Source

by Science Source

$25.00

Size

Bottom Style

Image Size

 
 

Product Details

Dress it up, dress it down, or use it to stay organized while you're on the go.   Our zip pouches can do it all.   They're crafted with 100% poly-poplin fabric, double-stitched at the seams for extra durability, and include a durable metal zipper for securing your valuables.

Our zip pouches are available in three different sizes and with two different bottom styles: regular and t-bottom.

Design Details

This hailstone was four inches in diameter and weighed seven ounces. Washington, D. C. May 26, 1953. Hail is a form of solid precipitation which... more

Care Instructions

Spot clean or dry clean only.

Ships Within

2 - 3 business days

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Hailstone, 1953 Photograph by Science Source

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Zip Pouch Tags

zip pouches atmospheric zip pouches historical zip pouches washington zip pouches science zip pouches phenomenon zip pouches weather zip pouches intense zip pouches storm zip pouches america zip pouches american zip pouches unite state zip pouches usa zip pouches history zip pouches historic zip pouches freeze zip pouches

Photograph Tags

photographs atmospheric photos historical photos washington photos science photos phenomenon photos weather photos intense photos storm photos america photos american photos unite state photos usa photos history photos historic photos freeze photos

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Artist's Description

This hailstone was four inches in diameter and weighed seven ounces. Washington, D. C. May 26, 1953. Hail is a form of solid precipitation which consists of balls or irregular lumps of ice, that are individually called hail stones. Hail stones on Earth consist mostly of water ice and measure between 5 millimeters (0.20 in) and 200 millimeters (7.9 in) in diameter, with the larger stones coming from severe thunderstorms. Hail is possible within most thunderstorms as it is produced by cumulonimbi (thunderclouds) and within 2 nautical miles (3.7 km) of the parent storm. Hail formation requires environments of strong, upward motion of air with the parent thunderstorm (similar to tornadoes) and lowered heights of the freezing level. Hail is most frequently formed in the interior of continents within the mid-latitudes of Earth, with hail generally confined to higher elevations within the tropics.

 

$25.00