The direction of the glacial scratches is from north to south.
The terms glacial scratches can be defined as abrasions into bedrocks caused by cuts made by ice as they flow across these bedrocks. Interestingly, the direction of the glacial scratches is in the direction of the flow of the ice.
Also, the direction of glacial movement determined by the arrows seen on the bedrock, at the bottom of the glacier, ice can slide over bedrock or shear subglacial sediments. More so, Ice flow direction is determined by the glacier surface: a glacier will always flow in the direction the ice is sloping
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