Solution:
The basis of the straight line is a depreciation and amortization process estimate. That is the best way to calculate the loss of value of a capital asset over time also known as direct depreciation.
The straight line basis is determined by dividing by either the number of years it is planned to use the variations between the cost of such an asset and the estimated recovery value.
--- use double-declining value year 1
(1/5) x 2 = 0.40
--- Cost x 40% = 22400
--- 22400 / 0.40 = 56,000
Savage value:
56,000 - 50,400 = 5,600
Answer:
My plan is to work in the oil field making about four thousand a month. one thousand a week, spending 500$ a month on food, 250$ on car note, 750$ on house note 60$for gas 1000$ for personal expenses.i will have 1440$ to put in my savings
Explanation:
Answer:
c. as the price of bread increases, the quantity of bread supplied will increase.
Explanation:
According to the law of supply we find out that there is a direct relationship existing between price of a good and quantity no supplied of same good. The law states that holding all factors fixed an increase in price brings about a resultant increase in quantity supplied. With this in mind, as the price of bread soars or goes up, the quantity of bread supplied would also increase too.
Answer:
These are the options for the question:
a. Gantter
b. Apptivo
c. Microsoft Project
d. Smartsheet
And this is the correct answer:
a. Gantter
Explanation:
Gantter is online, cloud-based, and very complete, it would be the best option for Mauricio. Smartsheet is also cloud-based but is a bit more simple, and it is not as well-reviewed.
Apptivo and Microsoft Project are not cloud-based, instead, they have to be downloaded, thus, would not meet the first requirement that Maurio is looking for.
Ocean sediment core provides a climate record of the past 70 million years.
1880 is the reliable global record which we can say the climate began. Proxies(climate) helps the scientists to determine the climatic patterns even before starting record-keeping.
Some examples of proxies are sub-fossil pollen, lake and ocean sediments, tree rings, and ice cores. Climatic of the time influenced the growth rate of proxies material. It is from proxies where we can recover quantities of particular isotopes from climatic changes.
The combination of proxies can produce temperature reconstruction which is longer the instrumental temperature.
