answer:
the relationship between climate-change and regularity of drought is global warming. climate-change can increase the chances of drought in a region; regions can gradually become drier overtime essentially due to the increasing concentration of temperatures and gases in the atmosphere. warmer temperatures enhance evaporation, which dries out soils and vegetation. this makes periods with low precipitation at high-regularity for drought.
(paraphrase if u can.)
The correct option is OXYGEN.
The biogeochemical cycle refers to the pathway by which a chemical element is moved through both the abiotic and biotic compartment of an ecosystem. Each element has its own cycle through which it is recycled.
Marine organisms in the biosphere usually create carbonated shells which are rich in oxygen, when these organisms die they serve as a source of molecular oxygen.
Answer:
The answer is below
Explanation:
a) Lily has 24 chocolate chip cookies and 32 vanilla wafers, since she has to put the chocolate and vanilla in the same bag, the number of bags must be a factor of 24 and 32. Below the bags are listed:
Number of bags: 1 2 4 8
Number of cookies: 24 12 6 3
Number of wafers 32 16 8 4
This means that the largest number of bag is 8 which would contain 3 cookies and 4 wafers
b) For the chocolate chip to be placed, the number of bags must be a factor of 24. It is given below:
Number of bags: 1 2 3 4 6 8 24
Number of cookies: 24 12 8 6 4 3 1
c) For the vanilla wafers to be placed, the number of bags must be a factor of 32. It is given below:
Number of bags: 1 2 4 8 16 32
Number of wafers: 32 16 6 4 2 1
Answer:
It helps with stratigraphic studies.
Explanation:
Bedding planes are the sheets that distinguish each successive layer of a stratified rock from its preceding layer, also known as sedimentary planes or stratification planes.
When one layer of sediment that is completely different from the former is formed or created over the old layer, bedding is said to have occured. This new layer may comprise of sand and tiny stones (called pebbles) or other sedimentary material. Because the components of the each new successive layer are totally different from the former in terms of composition, there is a marked division between each of them identifable by their quality and colur.t
The study of each of these layers to ascertain their time scale which provides basis for studies in historical geology is called stratigraphic studies.
The initial placement of strata in geologically diverse terrains is suggested in stratigraphical studies and the depositional nature of the sediment is established.
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