Fossils show us the long history of life and the past and current evolution processes on earth.
Where two plates glide past one another horizontally, a transform fault boundary develops. A transform fault causes plates to glide past one another. Tectonic plate boundaries are lines where two plates meet and interact. At transform margins, crust is fractured and broken rather than formed or destroyed, in contrast to convergent and divergent boundaries.
The borders at which two tectonic plates collide and interact are known as plate boundaries.At the plate borders, geologic activity, such as volcanic activity, always takes place.The limits of converging plates are those when plates are travelling in the same direction.Boundaries where motion is primarily horizontal are referred to as transform plate boundaries.When continental or oceanic plates move at different speeds or in the same direction but opposite of each other.A transform fault boundary forms when oceanic or continental plates slide past one other in opposing directions or move in the same direction but at different speeds. While no new crust is produced, subducted, or formed, and no volcanoes are formed, the fault produces earthquakes.
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Answer: Number 3 answer is: (5,3)
Number 4 answer is: (7,2)
Explanation:
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I would say that this is false and while the groundwater table could be right at the level of stream valleys and lakes, on hills provided they are underlain by permeable sediments or rocks, the groundwater table will be much higher than in the valleys as it usually reflects the topography more or less.