the correct answer is metamorphosis
Small to medium grain size.
During metamorphosis, an organism goes through physical changes, such as body shape, size, and sometimes color. It also undergoes physiological changes, like transitioning from one stage to another (e.g., larva to pupa).
The grain size of plutonic rocks is generally coarse, with individual mineral grains typically larger than 1 mm in size. This is due to the slow cooling and crystallization process of magma beneath the Earth's surface, allowing for the growth of larger crystals.
The grain size of fine sand typically ranges from 0.075 to 0.425 millimeters in diameter.
Grain size increases in the process of recrystallization.
In order to decrease the pressure within our respiratory tract, we have to expand our container. Our container is basically our thorax. If we can expand our thorax, the air pressure within our thoracic cavity will fall, and air will rush into our respiratory tract. The diaphragm is our primary means to increase our thoracic cavity
the correct answer is metamorphosis
Dinosaurs, as reptiles, did not undergo metamorphosis in the way that amphibians like frogs do. However, they did experience growth and developmental changes, transitioning from hatchlings to adults, which involved significant physical changes. Some species, like certain theropods, may have shown changes in feathers or size as they matured, but this is not classified as metamorphosis. Overall, the concept of metamorphosis is not applicable to dinosaurs in the same sense it is for amphibians.
there is no visible grain size
Small to medium grain size.
Particle size is another name for the term grain size.
During metamorphosis, an organism goes through physical changes, such as body shape, size, and sometimes color. It also undergoes physiological changes, like transitioning from one stage to another (e.g., larva to pupa).
Slaet in grain size is the size of sand crystals.
The size of a grain can vary depending on the type, but generally, a grain is around 1-3 millimeters in size. Grain size can also be influenced by factors such as processing and variety.
The grain size of plutonic rocks is generally coarse, with individual mineral grains typically larger than 1 mm in size. This is due to the slow cooling and crystallization process of magma beneath the Earth's surface, allowing for the growth of larger crystals.
The grain size of fine sand typically ranges from 0.075 to 0.425 millimeters in diameter.