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Why are tilted blocks of rock common along mid-ocean ridges?
Tilted blocks of rock along mid-ocean ridges are caused by the process of seafloor spreading. As new oceanic crust forms at the ridge axis, it pushes older crust away, creating faults and fractures that result in the tilting of blocks of rock. This tilting is a result of the spreading and rifting of the crust as it moves away from the ridge axis.
What holes are formed by huge blocks of glacier that have been burrowed into the ground?
kettles
What are small asteroid like bodies that formed the building blocks of the planet?
they are called planetesimals
After the last ice age stranded ice blocks left behind by the continental glacier melted and formed what?
As the ice blocks left behind by the continental glacier melted after the last ice age, they formed bodies of water known as kettle lakes. These kettle lakes are depressions in the landscape caused by the melting of the ice blocks, which were then filled with water from the melted ice.
Which fibers have ester units as their building blocks?
Polyester and polyamide fibers have ester units as their building blocks. Polyesters are formed by the condensation reaction of diols with dicarboxylic acids, while polyamides are formed by the condensation reaction of diamines with dicarboxylic acids.
What are tilted blocks?
Blocks that are veering to one side.
What Mountains made of huge tilted blocks of rocks surrounding faults?
the faul-block mountains are made of huge tilted blocks of rock that are separated from surrounding rock by fault
Where are tilted blocks of rock commonly found?
Tilted blocks of rock are commonly found in areas where tectonic forces have caused the Earth's crust to be uplifted and deformed, such as in mountain ranges, along fault lines, or in areas of intense volcanic activity. These tilted blocks can provide valuable information about the geological history and processes that have shaped the landscape.
Fault block mountains are formed when large blocks of crust are and tilted along normal faults?
Yes, fault block mountains are formed by the uplift of large blocks of crust due to movement along normal faults. As the blocks move up or down along the fault lines, they create steep mountain ranges and valleys. This type of mountain formation is common in regions with tectonic activity and significant faulting.
How many images will be formed when two plane mirror are tilted at an angle of 60 degree?
When two plane mirrors are tilted at an angle of 60 degrees, there are 5 images will be formed.
Mountains formed by blocks of crust moving along a fault?
what are mountains formed by blocks of crust moving along a fault
What characteristics are in Fault-block mountains and how are they formed?
Fault-block mountains are characterized by steep, rugged slopes and a block-like appearance. They are formed when tectonic forces cause the Earth's crust to break along faults, resulting in blocks of crust being uplifted and tilted. Over time, erosion exposes the faulted blocks, creating distinct mountain ranges.
What would you look for if you wanted to know if a mountain was formed by compression?
Tilted and folded rock formations.
How many images will be formed when two plane mirror are tilted at an angle of 120 degree?
2 images
Why are tilted blocks of rock common along mid-ocean ridges?
Tilted blocks of rock along mid-ocean ridges are caused by the process of seafloor spreading. As new oceanic crust forms at the ridge axis, it pushes older crust away, creating faults and fractures that result in the tilting of blocks of rock. This tilting is a result of the spreading and rifting of the crust as it moves away from the ridge axis.
What are holes formed by blocks of glacier that have been burrowed into the ground?
kettles
What kind of stress that produce on fault block?
Fault block mountains are formed when large blocks of Earth's crust move up or down along faults. The stress that produces fault block mountains typically comes from the tectonic forces pushing or pulling on the Earth's crust, causing the blocks to move vertically relative to each other. This movement can create a tilted or lifted landscape with steep scarps and flat valleys.
