Answer:
<u>D. Gradient decreases, discharge increases.</u>
Explanation:
- As steam is a body of water that carries rock particles and dissolved ions, discharge is measured in terms of volume/time (m3/sec). So when a river discharges its flow from a headwater to its mouth the velocity increases in the downstream direction.
- Thus the river load-carrying capacity increases downwards and so does the discharge rate. The discharge rate can also be influenced due to the rainfall patterns, volume of water and velocity of flow.
- Rock types also impact the streamflow if it is a porous rock, the surface will absorb more of moisture content and comparative more will be the water penetration towers the mouth of the flow.
Explanation:
The main difference between attribute data and spatial data is that the attribute data describes the characteristics of a geographical feature while spatial data describes the absolute and relative location of geographic features.
Anemometers measure wind speed<span> and wind vanes measure wind direction. A typical wind vane has a pointer in front and fins in the back. When the wind is blowing, the wind vane points into the wind. For example, in a </span>north<span> wind, the wind vane points northward.
</span>mark me as brainliest if I helped:)
Answer:
Espero que esto te ayude porque no sabía lo que significa fosa, así que hice mi mejor esfuerzo para hacerlo
Explanation:
UNA PIEZA LARGA Y LARGA DE TIERRA ENTRE LA COLINA Y LAS MONTAÑAS SE LLAMA UN VALLE UNA COLINA ES TIERRA UN POCO MÁS ALTO QUE EL TERRENO Y UNA MONTAÑA SE LEVANTA MUCHO MÁS ALTO QUE EL TERRENO.
