Answer:
artistic techniques.
Explanation:
- Mosaics <u>are the images and pieces of art made out of small fragments of stone, glass, or ceramics. </u>They are glued to the background or held together by plaster. They often decorate walls or floors and have been used since ancient times, both in secular and religious art.
- Frescos <u>are wall paintings done in fresh plaster in order to make them one with the wall background</u>. They have also been done since ancient times, and are crucial to the art of Renaissance and Orthodox Christan churches.
- The sculpture <u>is the type of three-dimensional art of craving and modeling the material into the wished piece of art.</u> It is done in various techniques and materials. It can be attached to the wall (relief) or completely free and unattached (free-standing).
<u>Judging by all the descriptions of these three things, we can conclude that they are all different artistic techniques.</u>
Answer:
The five main latitude regions of Earth's surface comprise geographical zones[1], divided by the major circles of latitude. The differences between them relate to climate. They are as follows:
The North Frigid Zone, between the North Pole at 90° N and the Arctic Circle at 66° 33' N, covers 4.12% of Earth's surface.
The North Temperate Zone, between the Arctic Circle at 66° 33' N and the Tropic of Cancer at 23° 27' N, covers 25.99% of Earth's surface.
The Torrid Zone, between the Tropic of Cancer at 23° 27' N and the Tropic of Capricorn at 23° 27' S, covers 39.78% of Earth's surface.
The South Temperate Zone, between the Tropic of Capricorn at 23° 27' S and the Antarctic Circle at 66° 33' S, covers 25.99% of Earth's surface.
The South Frigid Zone, from the Antarctic Circle at 66° 33' S and the South Pole at 90° S, covers 4.12% of Earth's surface.
Earth's climatic zones
Ice cap
Tundra
Boreal
Warm temperate
Subtropical
Tropical
On the basis of latitudinal extent, the globe is divided into three broad heat zones.
Answer:Nicholas Steno first formulated the principles that allow scientists to determine the relative ages of rocks in the 17th century. Steno stated that sedimentary rocks are formed in continuous, horizontal layers, with younger layers on top of older layers.
Explanation:
