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Are oil pipelines above or below ground?

both


What is the soil above a permanently frozen layer of ground thaws only during the arctic summer?

Permafrost


The soil above the a permanently frozen layer of ground thaws only during the arctic summer.?

Permafrost


The soil above the a permanently frozen layer of ground thaws only during during the Arctic summer.?

Permafrost


What term is used to describe a perennially frozen ground whose temperature never rises above 0degree Celsius?

permafrost


Can you suggest any problems there might be with pipelines as means of transport?

expensive to build and maintain as they are above the ground there are always fair of accident


Can you suggest any problem there might with pipelines as a mean of transport?

expensive to build and maintain as they are above the ground there are always fair of accident


How has the discovery of oil affected the position of Southwest Asia on the world?

buried pipelines in southwest Asia help reduce the danger of above ground accidents. however, oil spills on land do happen. because oil is such a valuable commodity' pipelines are carefully monitored.


What are houses like in the arctic?

They tend to be quite colorful as they are in many parts of the Arctic, and they are all raised above the ground to allow air to flow beneath due to the permafrost.


Can you suggest any problems there might be with pipelines as a means of transport?

expensive to build and maintain as they are above the ground there are always fair of accident


Why was the Alaskan pipeline built above ground and insulated?

I would be inclined to believe that the pipeline was built above ground to avoid destroying the terrain that it runs through.Also dealing with the permafrost would prove costly and would have taken much longer to finish.Besides it makes maintaining it much easier.


What is the relationship between permafrost and solifluction?

Permafrost is permanently frozen ground that significantly impacts the landscape in cold regions. Solifluction is a process where thawed soil and sediment move slowly down slopes due to gravity, often occurring in areas underlain by permafrost. When the upper layers of permafrost thaw during warmer seasons, the saturated soil above can become unstable and flow, leading to solifluction features such as lobes and terraces. Thus, permafrost acts as a barrier that influences the dynamics of soil movement in these regions.