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Hipervinculo Geología
The formation of stalagmites and stalactites happens through the capillary action between porous rocks and water rich in minerals. The rocks attract the water and the moisture accumulates until gravit ...
Hipervinculo Geología
Water has power! It has the power to shape the surface of the Earth. Water can change one landform by washing away sediment and then depositing it somewhere else to create a new landform. How are new ...
Hipervinculo Geología
Rocks are ever changing.They can be smoothed by water, broken off by wind, and cracked by ice.If you found a rock in your backyard then traveled back in time 1,000 years, that rock would look totally ...
By applying more and more pressure to a piece of aluminum foil “clay,” we can discover, stage by stage, how heat and pressure turn clay into slate, phyllite, and finally schist.It is an educational co ...
Hipervinculo Geología
Create your own miniature salt flats at home.It is an educational content by education.com.By clicking on the title of this resource, you will be redirected to the content. If you want to download the ...
Hipervinculo Geología
This project shows one way that sedimentary layers are formed as sediments (mud and silt, sand, pebbles and rocks, other ) settle over time.How do sedimentary layers form?It is an educational content ...
Hipervinculo Geología
You can’t always tell what mineral you’ve got by its color; lots of them look alike. How can you tell them apart?It is an educational content by education.com.By clicking on the title of this resource ...
Hipervinculo Geología
Density is the mass of an object divided by its volume. A rock and a piece of foam might be the same size, but they will weigh very different amounts. Density tells you how tightly packed the molecule ...
Hipervinculo Geología
The difference between quartz monzonite and gneiss is a lot of pressure. In this experiment, we'll learn how pressure can make the minerals in a rock line up in the same direction and form bands and f ...
Some minerals are harder than others because of how strongly their atoms are bound together at the molecular level. How do we find out which minerals are harder and which are softer?It is an education ...
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