ScienceIQ.com

Table Salt - It's All In The Ions

All elements are defined by their individual atoms, which are in turn identified by the number of protons in the nucleus of each atom. Since protons are carriers of positive electrical charge, there must then also be an equal number of negative electrical charge carriers in an electrically neutral atom. Sodium atoms in sodium metal and chlorine ...

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TableSaltItsAllInTheIons
Biology

The Journey of the Monarchs

The life of Monarch butterflies is an amazing one. They develop as caterpillars from the roughly 400 eggs each mother lays on the underside of milkweed plant leaves. Then they spend their brief lives ... Continue reading

MonarchButterflies
Engineering

Dress Sizes The Scientific Way

In pre-industrial America, most clothing was crafted at home or by professional tailors or dressmakers from individual measurements taken of each customer. In the early Twentieth Century, the growing ... Continue reading

DressSizesTheScientificWay
Biology

What is Garlic Mustard?

If someone told you that they were going to look for garlic mustard, you would probably think they were making dinner. Garlic Mustard, or Alliaria petiolata, is actually a plant native to Europe. It ... Continue reading

WhatisGarlicMustard
Geology

Is Earth Getting Fatter Around the Belt?

Besides being used for transmission of this email message to you, communication satellites are used for some neat science. By shooting a laser beam onto them and measuring how long it takes for light ... Continue reading

EarthBelt

Sedimentary Rock

SedimentaryRockSedimentary rock is one of three rock types on earth. Rock types are classified according to how the rock is formed. Igneous rock forms as it cools to a solid from molten rock. Metamorphic rock forms when rock is altered by intense heat, pressure, or both. Sedimentary rock is formed from particles derived from other rock through the processes of weathering, erosion, and deposition.

Sediments are eroded by flowing water in streams, by waves or ocean currents, by wind, ice, or gravity. Most erosion is done by flowing water. As eroded sediments move along, they grind against other rocks. This adds to the erosive power of the water, wind, or ice and further erodes the moving sediment. The grains become rounder, smoother, and smaller. The size and shape of the grains in a sedimentary rock give clues to its history. Coarse, angular grains could not have moved far from their source rock. Small, rounded grains must have been rolled along for hundreds of miles. Streams deposit tons of sediment into the oceans every day. In the oceans, sediment may be moved by currents and waves and later be dropped in layers upon the seafloor. Remains of organisms can be preserved as fossils as they drop and are quickly buried in accumulating sediments. Sedimentary rock is the only rock type containing fossils.

As layers of sediment build up, overburden pressure begins to squeeze the grains together. Water between the grains can leave once dissolved minerals behind after it is squeezed out or driven off by heat. These minerals cement the grains together into rock. Heat and pressure at burial depth can also fuse grains together into solid rock. As earth's forces cause the solid crust to move, sedimentary rock formed from sediments on the ocean floor or in valleys can be uplifted to the surface, perhaps reaching mountaintops. Some may become metamorphosed. Once at the surface, the rock is again exposed to weathering and erosion. New sediment forms, and the rock cycle continues. Because all rock at the surface is eroded and eventually forms new deposits, sedimentary rock is the most abundant rock type on earth.