Cancellation print.
recessive plate boundary
It is neither, because plate is not being made or destroyed. Divergent is constructive. Convergent is destructive. Subduction is constructive.
An artist may cancel a plate or block if they are unsatisfied with the results of the print, if there are technical issues with the plate or block, or if they have changed their mind about the image they want to create. Cancelling a plate or block allows the artist to prevent any further prints from being made and start fresh if needed.
Crust is destroyed (or recycled!) at convergent plate boundaries. Usually between oceanic and continental plates where subduction of the more dense oceanic crust occurs.
The type of plate boundary where oceanic crust is destroyed is called a convergent boundary, specifically a subduction zone. At these boundaries, one tectonic plate, typically oceanic, is forced beneath another plate, which can be either oceanic or continental. This process leads to the formation of deep ocean trenches and can result in volcanic activity and earthquakes. An example of this is the boundary between the Nazca Plate and the South American Plate.
recessive plate boundary
The plate boundary where oceanic crust is destroyed is a subduction zone. In this process, one tectonic plate is forced beneath another into the Earth's mantle. As the descending plate moves deeper into the mantle, it is eventually melted down and destroyed.
The process in which an image is drawn with a waxy pencil or crayon directly on a plate which can be made of zinc stone or aluminum is called lithography.
It is neither, because plate is not being made or destroyed. Divergent is constructive. Convergent is destructive. Subduction is constructive.
At divergent plate boundaries, crust is formed through the process of seafloor spreading. At convergent plate boundaries, crust is often destroyed through subduction, where one plate is forced beneath another into the mantle. At transform plate boundaries, crust is neither created nor destroyed, as the plates slide past each other horizontally.
Continental Plates are made of old rocks because they are never created or destroyed. For example, when an earthquake occurs, it can be caused by one tectonic plate going underneath another. The plate that goes underneath is always an oceanic plate because the rock is of a higher density. So, in summary, continental plates are lighter than oceanic crust, so they are never destroyed (hence why they are made of old rock).
What factor control image quality through a film or plate processor?
they are crushed
Image Carrier
Instantaneous results. The primary advantage of the photographic plate over CCDs is image quality--an 8x10 plate carries a lot more image information than a CCD can capture.
Oceanic crust isn't destroyed because it's old; it is, in fact, destroyed due to destructive plate boundaries. This is where a continental plate and an oceanic plate move towards each other. As the oceanic crust is denser, it is pushed under the continental plate. Here it is forced into the mantle of the earth, where it is destroyed due to heat and convection currents.
A daguerreotype is an early form of photography that involves exposing a silver-coated copper plate to light, creating a latent image. The plate is then developed using mercury vapor to bring out the image and fixed using a salt solution. The final image is incredibly detailed and permanent due to the silver on the plate.