Description of location cracks in rocks

Answers

Answer 1
Answer:

Answer:

A fracture is any separation in a geologic formation, such as a joint or a fault that divides the rock into two or more pieces. A fracture will sometimes form a deep fissure or crevice in the rock.

Explanation:

Can you specify your question

Answer 2
Answer: Cracks can be defined as fractures typicallcaused from pressure I believe

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Please help with this question for wastewater treatment, I can't figure out what formulas to use!Calculate the pounds of solids under aeration of the given plant:

Influent BOD: 310 mg/l

Influent TSS: 210 mg/l

Aerbay: 110' x 15' x 12 feet deep (operating level of the tank is 10')

Aerbay MLSS (mixed liquer suspended solids) 2,800 mg/l

Effluent BOD: 2.5 mg/l

Effluent TSS: 1.5 mg/l

Answers

Answer:

2884.17 lbs

Explanation:

Data provided:

Influent BOD = 310 mg/l

Influent TSS = 210 mg/l

Dimensions of Aerbay = 110' × 15' × 12'

Operating level of the tank = 10'  

thus,

The operating volume of aerbay = 110 × 15 × 10 =  16500 ft³

also,

1 ft³ = 7.48052 gallons

Thus,

16500 ft³ = 16500 × 7.48052 gallons = 123428.58 gallons  

Now,

Aerbay MLSS (mixed liquor suspended solids) = 2,800 mg/l

Therefore,

Pounds of solids under aeration

= Operating volume of aerbay × concentration of aerbay MLSS

also,

1 mg/L = 8. 3454 × 10⁻⁶ lbs/gallon

thus,

Pounds of solids under aeration

= 123428.58 gallons × ( 2800 × 8. 3454 × 10⁻⁶ lbs/gallon )

or

= 2884.17 lbs

In the United States, dry lines commonly develop over _____ during _____: Group of answer choices western Texas, Oklahoma, and Kansas; spring and early summer the Northeastern states; spring the desert Southwest; winter Southern California; early summer

Answers

Answer:

In the United States, dry lines commonly develop over southern Great Plains during mature cyclone.

Why do polar climates invaribly exhibit low precipitation values?

Answers

Answer:

Polar climates invariably exhibit low precipitation values because there is no humidity in those areas.

Explanation:

The polar climate is characterized by having almost permanently temperatures below 0 ° C; and little rainfall. The humidity in the air is non-existent and the wind is usually quite intense, which makes living conditions in this climate very bad.

The polar climate occurs mainly in the two poles, reaching more severe conditions in Antarctica, since being a continent, temperatures are cooler than those of the North Pole, reaching -70, -80 and even -89.5 ° C (record on the Earth's surface). The climate of the highest areas of the main mountain ranges of the planet closely resemble the polar, being able to occur on the summits of the Himalayas, the Andes or the mountains of Alaska.

What is the value of y?

Answers

Answer:

yes it is a type of seafood

y
=
2.4
x

4.5
,
x
=
4.5

1
y
=
2.4

4.5

4.5
1
y
=
6.3
y
=
1
6.3

0.159
d
)
1
y
=
0.23
x
+
14.7
,
x
=
4.5
1
y
=
0.23

4.5
+
14.7
1
y
=
1.035
+
14.7
1
y
=
15.735
y
=
1
15.735

0.064

What is Faint Young Sun Paradox?

Answers

The faint young Sun paradox or faint young Sun problem describes the apparent contradiction between observations of liquid water early in Earth's history and the astrophysical expectation that the Sun's output would be only 70 percent as intense during that epoch as it is during the modern epoch.

To calculate the dashed orbits from the stellar positions, astronomers had to assume that __________.if they observed for many more years, the dots would trace out ellipses

Answers

As the Earth travels closer to Saturn in its orbit and then both planets are situated on the side of the Sun, Saturn is enduring an apparent retrograde movement period.

Even with a good telescope, it would be impossible to see against the background of stars. The parallax angle is the difference, measured from a nearby star, between the Earth's location at one point in time of the year and the Earth six months later. Astronomers use this angle to determine how far away from Earth that star is. The procedure outlined previously, s, can be used to determine the distance to a nearby planet. Now that we have established an observation point O, we can calculate the angle that the planet is at, which is. P1P2 = d, where d is the diameter of the planet. Consequently, we may apply the parallax technique to determine a neighbouring planet's radius.

Learn more about Parallax here:

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