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What is the difference between overburden layer and spoil in geology?
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What is the overburden soil?
Overburden soil refers to the layer of soil and rock that sits above a mineral deposit or bedrock. It needs to be removed during mining or excavation activities to access the desired materials underneath. The overburden soil is usually of lower economic value compared to the underlying mineral deposits.
What is the liquid layer of earth that lies between the mantle and surrounds the core?
geology
What is different between double layer media and a single layer media?
difference between single layer and double winding
What is the most significant difference between the Layer 4 TCP and the Layer 4 UDP?
the main difference between UDP and TCP is that UDP is not a reliable protocol.
What layer of the heart is the thickest layer of muscle?
Myocardium? why are you asking the geology section?
What is the difference between troposphere and the thermosphere?
The troposphere is the lowest layer of the atmosphere, and the thermosphere is the third (?) layer.
What is difference between datalink layer flow control and transport layer flow control?
The difference between datalink layer flow control and transport layer flow control is the need to keep the different layers of data separate in the flow control option.
What is the difference between lower and upper epidermis?
mesophyll layer
What is the difference between a layer 2 and a layer 3 switch?
The difference between Layer 2 and Layer 3 switching is the type of information inside the frame that is used to determine the correct output interface. With Layer 2 switching, frames are switched based on MAC address information. With Layer 3 switching, frames are switched based on network-layer information.
What is the difference between a permeable layer of rock and an impermeable layer?
Impermiable rock means nothing can go through it
In lithology and geology which is a layer of rock with varying thicknesses called?
A stratum.
What is the discontinuity layer?
In geology, a subterranean interface at which seismic velocities change.
