Answer:
It would look like an uplift or dome because the laccolith below is a lens-shaped mass of magma that pushes the rock above it upward.
Explanation:
The laccolith is formed by volcanic activity. Not all of the magma is contracted in the volcano and comes out form it or solidifies in it. Some of the magma actually moves below ground in the surrounding area, using the cracks as pathways. When this magma cools off deep underground it creates intrusions.
One of those intrusions is the laccolith. The laccolith can be described as having a lens-shape, or that it looks like a mushroom. The laccolith is in intrusion that pushes the crust upwards, so the surface above it uplifts or looks like a dome that sticks out in its surroundings.
The laccolith may come out eventually on the surface because of the weathering and erosion, but for that to happen usually millions of years are needed.
B) the force of gravity causes mass wasting to occur is the answer
As a mountainous island chain, New Zealand has a complex maritime climate whose weather is greatly affected by the mountains and the sea. The climate ranges from warm sub-tropical in the north, to cool sub-temperate in the south. The prevailing winds are westerly and this leads to a reasonably high rainfall particularly in the west. New Zealand's location relative to Antarctica means that weather systems from that direction can cause very sudden deterioration in weather and extreme drops in temperature particularly in the south.