There are lot of different things that can slide each other for example in science we learn about the plate boundaries and one of them is transform boundaries that grind or slides each other.
transform boundary
When one tectonic plate slides past another, it can create a transform boundary. At this boundary, the plates grind against each other, causing earthquakes due to built-up stress being released. This movement can also lead to the formation of features such as strike-slip faults.
Sentence A describes liquids best, although sentence B also fits the description of liquids.
Tectonic Plates move by trying to push past each other and by trying to slide past each other.
Particles in a liquid can slide past each other but are still packed together.
earthquake
its called a transform boundary
When two plates slide past each other, this is called a transform fault. Earthquakes can occur when the plates scrape by. If the earthquake happens underwater, a tsunami may occur. (Like in Japan)
Tectonic plates slide past each other at transform plate boundaries. This movement can result in earthquakes as the plates grind against each other. Examples of transform plate boundaries include the San Andreas Fault in California and the Alpine Fault in New Zealand.
gliding
transform boundary
When one tectonic plate slides past another, it can create a transform boundary. At this boundary, the plates grind against each other, causing earthquakes due to built-up stress being released. This movement can also lead to the formation of features such as strike-slip faults.
Sentence A describes liquids best, although sentence B also fits the description of liquids.
It is where one plate slides past another plate, rubbing against it. One slides right, the other left. An example would be North America. Your Welcome.
The best way to store microscope slides is in a slide box. A slide box will keep slides from sticking to each other, keeping them intact.
Yes, adjacent slides in PowerPoint are considered contiguous slides. Contiguous slides are those that are next to each other in the presentation, without any gaps in between. This means that if you select a range of slides, the selected slides will be contiguous if they are sequentially arranged in the slide sorter view.
Theny happen in Mountain ranges when slides hit each other.