From the color of the background in your photos (I assume it was white) I believe the color balance is pretty close to actual, so the blue colors are fairly represented.
The colors certainly have the appearance that is common to copper oxides and copper carbonates. This is probably a specimen from the weathering zone on the top of a copper deposit and represents the secondary minerals from that zone that have been glacially transported.
Any chance this specimen was found in the glacial rubble south or south-southwest of Ladysmith?