Limestone and quartz are common minerals found in Florida. Sarah has a piece of each, but does not know which is which. To find out, she plans an investigation to determine the density of each sample, because limestone has a lower density than quartz. Density is equal to the mass divided by volume. She places a piece of each mineral into a graduated cylinder that contains water. The table shows the measurements Sarah recorded. What can Sarah most likely conclude is true? Mass of Mineral 1 9.50g Mass of Mineral 2 9g Volume of water in graduated cylinder 25ml Volume of water and mineral 1 in graduated cylinder 30ml Volume of water and mineral 2 in graduated cylinder 28.4 ml *
a.) Mineral 2 is limestone because it has less mass
b.) MIneral 1 is limestone because it has more mass
c.) MIneral 1 is limestone because it has a lower density
d.) Mineral 2 is limestone because it has a lower density

The Texas Adoption Project: adopted children and their intellectual resemblance to biological and adoptive parents. ... Intelligence test scores were obtained from parents and children in 300 adoptive families and compared with similar measures available for the biological mothers of the same adopted children.

Individual answers may vary, but your answer is expected to include some of the following points.

The impact of the Internet and the World Wide Web can be best understood by identifying the fields that have been influenced the most by these technologies. These may include education; banking, trade, and commerce; up-to-the minute weather reports; shopping; information exchange; socializing and self-expression; the arts; entertainment; navigation (maps); publishing; business networking.

Answer:

self diagnosing disorders upon yourself or others

Explanation:

The Diagnostic and Statistical Manual of Mental Disorders (DSM) is the handbook used by healthcare professionals in the United States and much of the world as the authoritative guide to the diagnosis of mental disorders. DSM contains descriptions, symptoms, and other criteria for diagnosing mental disorders.

Answer: BAC = 0.056%

Explanation:-

Data given;

Weight of the man = 150 lbs (Wt)

Number of drinks = 2 beers

We know that

A beer contains 5% (0.05) of alcohol (D)

1 bear = 12oz

So 2 beer = 2 × 12 = 24oz (A)

Derived from widmark formula;

BAC for Male = (A × D × 5.14) / ( Wt × 0.73 )

BAC for Female = (A × D × 5.14) / ( Wt × 0.66 )

WHERE

A = Alcohol consumed in ounces (oz.)

D = percentage of alcohol written as a decimal

Wt = weight of person in pounds (lbs.)

Using BAC for male

BAC for Male = (A × D × 5.14) / ( Wt × 0.73 )

We simply input our values

BAC = ( 24 × 0.05 × 5.14) / ( 150 × 0.73)

BAC = 6.168 / 109.5

BAC = 0.056%

Ocean basins can form at rift basins where continental crust is pulled apart and subsequently subsides, or at subduction zones where one plate dives beneath another. Ocean basins influence the size and movement of tectonic plates and can close over time, possibly leading to supercontinent formation.

An ocean basin is likely to form at a location where continental crust is being pulled apart due to the process of rift basin formation. As the crust on both sides of the rift subsides, the area initially becomes a narrow sea and, if rifting continues, eventually develops into an ocean basin. The East African rift basin is an example of an early stage in this process. Additionally, other types of basins such as trench basins, forearc basins, and foreland basins are associated with different tectonic settings such as subduction zones and the mass of volcanic ranges.

Ocean basins are relatively young geological features, not exceeding 180 million years in age. The formation of ocean basins can significantly influence the size of oceanic and continental plates, such as the expansion of the Atlantic Ocean due to the mid-Atlantic ridge spreading, which is not counteracted by subduction except in certain regions like the Caribbean. In contrast, the Pacific Ocean is slowly getting smaller because its formation rate is outpaced by subduction processes, such as under North America at the Cascadia Subduction Zone.

Over geological time, as oceanic crust subducts beneath continental crust, ocean basins can close, leading to continental collision and the potential formation of a supercontinent. Known cycles of supercontinent formation and breakup have occurred throughout Earth's history approximately every 500 million years.