<span>Conic Projection. With this type of map, there is a particular latitude at which the cone touches the globe. Using this projection, there is little distortion of elements around the areas along the latitudinal line but the top and bottom of such projection displays visible distortion. Nonetheless, their simplicity in construction has made it the preferred method used in large scale maps.</span>
Answer:
The principle of original horizontality and lateral continuity
Explanation:
The principle of original horizontality explains how sedimentary rocks are laid and arranged strategically in basins of deposition flatly and horizontally in space. It is very important when trying to determine the original orientation of strata in a sedimentary terrain. Sediments are laid in water under a strong influence of gravitational force.
The principle of lateral continuity shows that sediments are laid out laterally and parallel to one another until they thin or taper out on their edges. This shows the layered or stratified nature of sediments.
Answer:
Naples Italy for the queen of Italy
In ancient Rome, flat bread called "focaccia" was first topped with oils and herbs. In Greece and the Middle East, flat "pita"
Many Italian immigrants came to America in the 1800s and 1900s. One of these neighborhoods was "Little Italy" in New York City, where one of America's first pizza restaurants opened in 1905 . Finally, in the 1950s, many Americans opened "pizza parlors" that specialized in baking all kinds of pizza pies. Americans realized that pizza was delicious, fun, and convenient.
Explanation:
<span><em><u>B).the long-term, prevailing atmospheric conditions</u></em></span>
The long term average being 30 years. These weather variations are affected by the temperature, precipitation, and wind.
Climate determinants include latitude, altitude, proximity to mountains and oceans, proportion of land to water, thermohaline circulation of the ocean, ocean currents, density and type of vegetation present in an area, as well as the areas' water retention and rainfall.
Climate are classified into three groups. These are Bergeron and Spatial Synoptic, Koppen, and Thornthwaite.