Answer:
C.) influence how land is used
Explanation:
Among the physiographic and archaeological variables used for the elaboration of the settlement pattern are the altitude, the phytogeography, the area covered by the sites, the types of sites, their distance from the water, the type of water sources, the number of low floor structures per site, the diameter and depth dimensions of the low floor structures, the chronology obtained from radiocarbon and thermoluminescence analysis, the insertion into the terrain model, the solar orientation, the prevailing winds and the field of eyesight. The compilation of these archaeological distribution and implantation data and the observation of their characteristics aim to create a settlement pattern of the populations of origin of a given area.
The best and most correct answer among the choices provided by the question is the third choice "the Coriolis efffect"
The Coriolis effect<span> is most apparent in the path of an object moving longitudinally. On the Earth an object that moves along a north-south path, or longitudinal line, will undergo apparent deflection to the right in the Northern Hemisphere and to the left in the Southern Hemisphere.</span>
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Answer:
Explanation:
The three main types of volcanoes are as follows:
1. Composite volcanoes: These are also called as strato volcanoes. These are steep and formed by the layers of ashes and lava. The eruption from these volcanoes is in the form of pyroclastic flow. The pyroclastic flow is in the form of superheated mixture which consists of rock dust, ash, and hot steam. These volcanoes can rise above the 8000 feet. These are found in the destructive plate margins. Example of these volcanoes include the Mount Fuji in Japan.
2. Shield Volcanoes: These volcanoes are low and they have gentle sloping sides. These are formed by the layers of lava. Their eruption of lava is non-explosive. These produces the fast flowing fluids that can flow to many miles. These can destroy the nearby surrounding regions can cause injury and even death. These volcanoes are found in the region of constructive boundaries and also at the volcanic hotspots. The examples of shield volcanoes include the Maunaloa on Hawaii.
3. Dome volcanoes: These are also called as acid lava cones as these emit acid which is much thicker than that of the lava. These have steeper sides as compared to the shield volcanoes. The lava is thick and sticky as a result of this it cannot flow to far region and it cools and solidifies. The example of dome volcanoes include the Puy de Dome of Auvergne, France.
The Barringer crater in Arizona is an example of possible climate change from a asteroid impact. In the desert of northern Arizona, the United States, Meteor Crater, also known as Barringer Crater, is a meteorite impact crater located about 37 miles (60 kilometres) east of Flagstaff and 18 miles (29 kilometres) west of Winslow.
The location has been known by a number of other names in the past, and the meteorite shards are officially referred to as the Canyon Diablo Meteorite after the nearby Caon Diablo. The feature got its name, "Meteor Crater," from the local post office with the name Meteor since the United States Board on Geographic.
To learn more about Meteor, click here.
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