<span>A. potential energy because it depends on mass and the gallon has more mass. </span>
Answer:
The difference lies in their size, wind velocity, rate of travel, and duration.
Explanation:
<h3 /><h3>Tornadoes</h3>
- reaches rotating speeds up to 300 miles per hour.
- travels between 25 and 40 miles per hour.
- lasts for a few minutes but can exist for hours.
<h3>Typhoons</h3>
- winds that vary from 75 to 200 miles per hour.
- moves between 10 and 20 miles per hour.
- has a diameter up to 600 miles.
- exists from days up to a week
The stomata open up to absorb the carbon dioxide needed to perform photosynthesis.
Answer:
meiosis I
Explanation:
Independent transmission is Mendel's second law. Like any Mendel law it is based or is about the transmission of alleles. Therefore, the law of independent transmission is based on the fact that when forming gametes, the alleles of one gene are segregated independently before the segregation of the alleles of another gene. This second law can not only be applied to the characters that Mendel analyzed, which were two genes with two possible alleles, this law is fulfilled with more than two characters. We must bear in mind that alleles are the different forms that a gene can present.
On the other hand we have the concept of meiosis I which is a type of cell division that in animals generally gives rise to gametes for sexual reproduction or sexual spores (in plants and fungi). That is to say in mitosis we find that there is only a cell division between homologous chromosomes, so that from a tetraploid number (4n) we pass to a diploid number (2n). While in meiosis we find that there are two cell divisions in which we go from a tetraploid number (4n) to a haploid number (n). This means that this is a reductive process. These haploid cells will join together to give rise to a diploid cell. Another important concept to consider in meiosis is the formation of chiasmas that are created between non-sister chromatids, thanks to this phenomenon the exchange of genetic material occurs.
Shield volcanoes,<span>This is caused by the highly fluid lava they erupt, which travels farther than lava erupted from </span>stratovolcanoes<span>.
The steady accumulation of broad sheets of lava</span> Low volumes of such lavas layered over long periods of time are what slowly constructs the characteristically low, broad profile of a mature shield volcano
