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alexdok [17]
3 years ago
5

Need help on 8 and 9 HURRY PLZ

Biology
1 answer:
cupoosta [38]3 years ago
3 0
8 A and Idk the other one
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A single-celled organism can be classified as a prokarote based on the absence of the_______
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which statement best captures george vaillant's view of development? question 11 options: biology is the map of life events. kee
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George Vaillant's view of developmental biology is the map of life events. keeping on time will keep one's self well-adjusted life requires a constant series of adaptations. culture determines the life cycle. <u>Life requires a constant series of adaptations.</u>

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Life cycle, in biology, is the series of modifications that the individuals of a species undergo as they bypass from the beginning of a given developmental level to the inception of that identical developmental stage in a subsequent era.

A life cycle ends when an organism dies. In standard, plants and animals go through 3 simple tiers in their lifestyles cycles, starting as a fertilized egg or seed, growing into an immature juvenile, and then ultimately transforming into a grownup.

A life cycle approach can assist us to make picks. It implies that everybody within the complete chain of a product's life cycle, from cradle to grave, has a duty and a function to play, contemplating all of the relevant effects on the economic system, the environment, and society.

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If cells don't work together, what would happen to the organism? ​
Mama L [17]

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If cells do not work together, the organism would die.

Explanation:

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Why is it sometimes hard to establish an MPA?
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<h2><em>Why is it sometimes hard to establish an MPA?</em></h2>

  • <em>Arguably, it is difficult to declare such an MPA successful, when <u>the human populations responsible for degradation have been removed</u>, and its mere establishment is rife with such political contention. Issues also arise when considering the resources needed to support a large-scale MPA.</em>

<em>hope </em><em>it</em><em> helps</em>

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Read 2 more answers
Kitakami River region constraints
nalin [4]

Answer:

In March 2011, a magnitude 9.0 earthquake—the fourth largest recorded since 1900—triggered a powerful tsunami that pummeled the northeastern coast of Japan. The earthquake occurred offshore, about 130 kilometers (80 miles) east of Sendai at 2:46 p.m. on March 11. Within 20 minutes, massive swells of water started to inundate the mainland.

The tallest waves and most devastating flooding from the 2011 TÅhoku-oki tsunami occurred along the jagged coast of northern Honshu, a landscape dimpled with bays and coves known as ria coast. The steep, narrow bays of ria coasts trap and focus incoming tsunami waves, creating destructive swells and currents that can push huge volumes of water far inland, particularly along river channels.

That's exactly what happened in the days before the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER), an instrument on NASA's Terra satellite, captured the middle image above (on March 14, 2011). It shows severe flooding along the Kitakami River three days after the earthquake struck.

The top image, captured by the Advanced Land Imager on NASA's Earth Observing-1 (EO-1), shows the same scene a year later. And the bottom image, captured by ASTER, shows what the area looked like before the earthquake struck. All three are false-color images that combine infrared, red, and green wavelengths in a way that makes it easy to distinguish between water and land. Vegetation appears red, and fallow fields appear pale brown.

In the image from March 2011 (middle), wide swaths of flood water cover the north and south banks of the river channel, and sediment fills the river's mouth. Some of the most dramatic flooding occurred just to the south of the river, where floodwater washed across large tracts of farmland and the small village of Nagatsura. Notice how far up the river the flooding occurred: Research conducted by scientists at TÅhoku University suggests that waves from the tsunami traveled nearly 50 kilometers (30 miles) upstream from the mouth of the Kitakami River.

One year after the tsunami, floodwaters had subsided, the river was back within its banks, and many of the agricultural fields along the Kitakami were dry again. However, the landscape near the mouth of the river remains irrevocably altered in comparison to how it looked before (bottom image). The farmland immediately north and east of Nagatsura has become river bottom. The width of the river mouth has widened. And water from Oppa Bay has crept inland, leaving only a narrow strip of land and new islands near the river mouth.

See other images from the tsunami—including more imagery from 2012—in our feature slideshow: Tohoku Earthquake and Tsunami: Looking Back from Space.

Explanation:

That's is it thank you :]

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