A white dwarf.
white dwarf
white dwarf
white dwarf
When a red giant loses its outer layers, it typically sheds its envelope and leaves behind a hot core. This core, which shrinks to about one millionth of its original size, becomes a white dwarf. A white dwarf is a dense, Earth-sized stellar remnant primarily composed of carbon and oxygen that no longer undergoes fusion but gradually cools over time.
Stratus clouds are formed in blanket-like layers, covering the sky like a sheet. They often bring overcast conditions and can result in light precipitation such as drizzle or light snow. These clouds typically form in stable, low-pressure environments.
white dwarf
white dwarf
white dwarf
When a red giant loses its outer layers, it typically sheds its envelope and leaves behind a hot core. This core, which shrinks to about one millionth of its original size, becomes a white dwarf. A white dwarf is a dense, Earth-sized stellar remnant primarily composed of carbon and oxygen that no longer undergoes fusion but gradually cools over time.
Layers are formed in atmosphere. They keep the functionality apart.
Horizontal layers of rocks are rock layers that are parallel to the Earth's surface. These layers are typically formed over time through sedimentary processes, such as deposition of sediment in water or air. The horizontal orientation of these layers indicates the original horizontal position in which they were deposited.
Sedimentary rock, like limestone, is formed in layers.
Stratus is the cloud in flat layers
It is called the 'Principle of Original Horizontality' and was proposed by the Danish geological pioneer Nicholas Steno (1638-1686). This principle states that layers of sediment are originally deposited horizontally. However, please note that it is now known that not all sedimentary layers are deposited purely horizontally and the principle is only an approximation of reality.
Cross-bedding refers to inclined layers in sedimentary rock that were formed as a result of wind or water driven ripples or dunes in the original depositional environment.
Diamonds are usually formed in the mantle.
Detrital sedimentary layers.