Language is most likely to connect a cultural region because communication is the key to everything.
Answer:
landslide
Explanation:
This question is related to a picture. In the picture you can see that a small town was affected by a landslide located near a steep hill. As the statement reads, it can be a destructive process as not only is the countryside affected by removal of the top earth layer along with all the vegetation in that area, consequence of heavy rainfall or a mayor earthquake or shift in landmass, but it also turns into a constructive process as at the bottom of the hill, where the landslide or mud accumulates, the debris forms a new layer over the old and it is then seen as constructive.
Unlike their equatorward neighbours, marine west coast climates are located beyond the farthest poleward extent of the subtropical anticyclone, and they experience the midlatitude westerlies and traveling frontal cyclones all year. Precipitation totals vary somewhat throughout the year in response to the changing location and intensity of these storm systems, but annual accumulations generally range from 50 to 250 cm (20 to 98 inches), with local totals exceeding 500 cm (197 inches) where onshore winds encounter mountain ranges. Not only is precipitation plentiful but it is also reliable and frequent. Many areas have rainfall more than 150 days per year, although the precipitation is often of low intensity. Fog is common in autumn and winter, but thunderstorms are infrequent. Strong gales with high winds may be encountered in winter.
Annual temperature ranges are rather small (10–15 °C or [50–59 °F]), about half those encountered farther to the east in the continental interior at the same latitude. Mean annual temperatures are usually 7–13 °C (45–55 °F) in lowland areas, the winters are mild, and the summers are relatively moderate, rarely having monthly temperatures above 20 °C (68 °F). In North America and South America, Australia, and New Zealand, north–south mountain ranges backing the west coasts of the landmasses at these latitudes confine the marine west coast climate to relatively narrow coastal strips (but enhance precipitation). By contrast, in Europe the major mountain chains (the Alps and Pyrenees) run east–west, permitting Cfb and Cfc climates to extend inland some 2,000 km (about 1,250 miles) into eastern Germany and Poland.