The cultural landscape reflects the people who live there in many ways. One of how cultural landscape reflects the inhabitants of a place is through "the techniques of sustainable land-use."
This is because the cultural landscape can tell a lot about the inhabitant regarding technological advancement, religion, economic development, and other important features.
For example, the battlefield is a historical site of a cultural landscape that signifies that the inhabitants are warriors or have fought in many wars.
Another example is a designed landscape such as estates or churchyards, which may define the level of wealth or religion that the people of that particular place practiced.
Other types of a cultural landscape that can help reflect the people are:
- Historical vernacular landscape
- Ethnographic landscape
Hence, in this case, it is concluded that cultural landscape is a vital factor to consider when defining the people of a place.
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Answer:
the time of the lowest temperature.
Explanation:
Relative humidity simply talks about the ratio of the quantity of water the air contains at any given time, to the highest quantity of water the air could ever have. So when the water vapor content in air remains constant while the temperature falls, then the relative humidity tends to increase. This phenomenon usually takes place in the morning when the sun is yet to come out and the temperature is usually cooler. When sun peaks, afternoon sets in, the relative humidity then reduces.
Some of the US states that borders Canada are Minnesota, New York and Idaho
Answer: It refers to the decline in travel time between geographical locations as a result of transportation, communication, and related technological and social innovations.
Explanation:
Volcanoes play an important role in creating land since they are the sources of magma, which once above ground normally cools to create new land. In the ocean, this land normally forms at divergent and convergent boundaries or hot spots. At divergent boundaries (where two plates move apart), magma constantly erupts along a trench deep below the ocean's surface. This magma rarely piles upward and instead is pushed to both sides of the trench. This is how new seafloor forms. Convergent boundaries can create island arcs like Indonesia as magma erupts bit by bit. Hot spots occur in the middle of plates. They are instances where the mantle pierces through the crust and begins to erupt directly onto to seafloor. Over time, these eruptions will pile up and create underwater volcanoes until they potentially make it above sea level, thereby forming an island. This is how Hawaii was and continues to be formed.
