Answer:
The rest of the energy from grasshopper will be transferred to the next trophic level in the food chain with in the ecosystem.
Explanation:
All the organisms with in an ecosystem are part of some food chain. Hence when ever an organism feed upon some other organism/plant to get energy , retains some part of it and transfers the rest of energy to the next trophic level.
Usually in a food chain, all organisms retain 10% of the energy they get from the preceding trophic level and transfers 90% of the energy to the next trophic level.
Thus, whichever organism feed on grasshopper or depend for food on grasshopper in some or the other way will get the rest of the energy.
v=bh v=26pi+(6.5)
v=bh v=26pi(6.5)
v=bh 26pi=b(6.5)
Answer:
Explanation:
Given that:
Volume of the cylinder,
height of cylinder,
Let the area of the base of the cylinder be:
As we know that volume is the one dimensionally extruded form of area:
Answer:
this may not be the answer but i am trying to help
V=(pi)(r^2)(h)
26x=(pi)(r^2)(6.5)
or
V=(area of b)(h)
26x=b(6.5)
Explanation:
I am confused by 26x did you mean pi?
information, what are the genotypes of the red parent tulips?
Answer:
According to the information, the parent red tulip plants have a heterozygous genotype for red colour. The allele for red colour is dominant whereas the allele for white colour is recessive. Hence, the recessive allele will be masked by the dominant allele and the parent plants will have red tulips.
When heterozygous red tulip plants will be crossed, then 25% red homozygous plants will be made, 50 % would be red heterozygous plants whereas 25% would be white homozygous.
pyroclastic volcano
composite cone volcano
shield volcano
Answer:
Composite cone volcano
Explanation:
Composite Cone Volcanoes are large volcanic buildings with long, generally conical shape, usually with a small crater on the summit and steep flanks, constructed by the interleaving of lava flows and pyroclastic products emitted by one or more conduits, which can be punctuated. over time by episodes of partial cone collapse, reconstruction and changes in conduit location.
Compound volcanoes are found in all regions of volcanism, but it is in plate convergence zones, where a tectonic plate subdows (plunges) toward the earth's mantle beneath another tectonic plate, that these volcanic buildings are most abundant. The magmatic expression of a converging plate margin environment is usually a series of sub-regularly spaced Compound Volcanoes, forming a sub-parallel volcanic arch to the tectonic fossa.
composite cone volcano