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Updated August 13, 2007

Student Questions Explained


Are you struggling to understand a particular BC Science 10 concept? Is there a particular term or section of a Science Foundations 10 unit that you find difficult to grasp? You've come to the right place!

In the collection of explanations below, you may find the answer you are looking for. But if you don't find your answer, submit your question and the Science Foundations author team will do their best to post an explanation for you.

Send your questions by email to the following address:

Please include your first name and the school you attend. We'll only use your first name in relation to answering the question.

We will do out best to address all questions as promptly as possible, but please understand that we may not be able to answer them all.

Please limit your questions to the BC Science 10 curriculum content.


Menu of Student Questions

Unit 1 Cells

No questions posted yet!

Unit 2 Genetics

  1. What's the relationship between genes and proteins?
  2. What is the difference chromatin, chromosomes and sister chromatids?
  3. Are genes and DNA the same thing?

Unit 3 Chemistry

  1. Are the ions on the Data Booklet also  molecular compounds?
  2. What exactly are the purposes for an electron orbit and how it affects the atom?

Unit 4 Electricity and Magnetism

  1. How do you describe and diagram magnetic field lines?
  2. What is the difference between current and voltage?

Unit 5 Radioactivity

  1. How can radiation help to cure diseases if radiation is harmful?
  2. Is radiation a wave or a particle?
  3. What is the difference between ionizing and non-ionizing radiation?
  4. Is the wavelength and frequency of all types of electromagnetic radiation the same?
  5. I always get the wavelength, frequency, energy relationship mixed up. Can you summarize this to help me remember it?
  6. I have trouble understanding concepts of radioactive decay...

Unit 6 Earth Forces

  1. Where exactly is the Mid-Atlantic Ridge?
  2. How do we know the locations of all the trenches and ridge in the world?
  3. What are the benefits of living near active volcanoes?
  4. How does the presence of glaciation in places like India add credibility to Wegener's theory?
  5. What does looking at the Earth's surface tell a geologist about what is happening underground?
  6. What are two different uses for a geological map of an area?
  7. How do geologist determine the start and end of an era?
  8. What does the magnetic pattern in the bands of rock suggest about the formation of the sea floor?
  9. Why are the magnetized particles in igneous rocks on the sea floor are not all pointing in the same direction?

Answers to Student Questions

Unit 2 Genetics

1. What's the relationship between genes and proteins?

A very good question! Let's see if we can figure out the difference. J. Martha

Genes and Proteins

The short answer to this question is, genes provide the information for the construction of proteins. Proteins are very important molecules in our body, because they serve so many important functions. The proteins that are constructed by your cells have several functions:

  • Structural functions, such as helping to maintain cell shape.
  • Enzyme functions, such as catalyzing chemical reactions.
  • Signaling functions, such as serving as chemical messengers in the immune system.
  • Hormone functions, such as carrying chemical messages throughout the body via the bloodstream.

Where do proteins come from? Proteins are made by cells by combining amino acids. Amino acids are obtained in two ways - your body synthesizes some, but many come from the food that you eat.

How do your cells know how to make the hundreds of different of proteins that your body requires? That's where genes come in. Genes are the bits of information that are found in the DNA, the genetic material that is found in the nucleus of every cell in your body. Cells access the information, or the "code" found in the genes that instructs the cell which amino acids to put together, and in what order, to make a protein. It is interesting to note that it is small variations in the genetic code from person to person that allows for varying amounts and types of protein construction from person to person. This is what accounts for some of our individual differences!


2. What is the difference chromatin, chromosomes and sister chromatids?

Hmmm... as a biology teacher, I understand those terms can be confusing. I will try to clarify them for you. J. Martha

Chromatin, Chromosomes and Chromatids

The reason these three terms, chromatin, chromosomes and chromatids, are easily confused is due to the fact that they are all different forms of the same thing - DNA. Deoxyribonucleic acid (DNA) is the molecule that is found in the nucleus of our cells, and holds the genetic instructions for the structure and function of all living things. The DNA that is pictured to the right in an artist's drawing of its famous double-helix structure. The structure of DNA is usually modelled or drawn in textbooks, because the actual DNA molecule detail is far too small to be seen with the light microscope. When you look at a cell under under the light microscope, you are far more likely to see DNA as part of much larger structures - which brings us back to the terms we are trying to understand: chromatin, chromosomes and chromatids.

With a powerful light microscope, the nucleus of a cell can be seen. If the cell has been stained, chromatin is usually fairly easy to see (the name chromatin literally means "coloured material"). Chromatin is simply a gathering of the DNA of the cell, in a large clump mixed together with some proteins. Imagine a strand of DNA as a single elastic band that you hold twisted between your thumbs - by itself, it is easy to see the structure of the elastic. Now imagine a huge tangled ball of elastic bands, the kind you might find in a junk drawer at home. The tangled ball represents the chromatin in the nucleus. Because DNA is a small and delicate molecule, it is almost always found in the form of chromatin - bunched together and mixed with proteins. Biologists believe DNA exists mainly in the form of chromatin because it is more protected in a large "clump".

There are times however, when the clump of chromatin "unwinds". This happens during cell division; it is necessary to make a copy of the DNA, so each daughter cell gets a complete copy of all the genetic instructions contained in the DNA. When chromatin "unwinds" we can finally see more defined versions of the DNA molecule - chromosomes and chromatids.

A chromosome is a actually one very long strand of DNA. Under the light microscope they can only be seen during cell division - this is when the individual chromosomes have doubled in preparation for cell division. When the chromosomes have doubled, many of them appear to have an "X" shape, as shown in the diagram to the right. The two segments that make up the chromosome are known as chromatids, and represent identical copies of the same DNA strand.

You can also see in the diagram that the two chromatids that make up the chromosome are held together by a structure called a centromere. During cell division, the chromatids will separate at the location of the centromere forming two separate strands, each of which goes to opposite poles of the dividing cell. As the cell division continues, the two strands will become permanently separated, one each in the two new daughter cells formed by the cell division.

Now here's the real confusing part! Once the two chromatids have separated and have migrated to their respective daughter cells, they are now known as chromosomes! The term chromatid is only used when a chromosome is in a "doubled" state (as shown in the diagram to the right), to help differentiate between the two different strands.

There! Hopefully that has cleared up some confusion between three similar genetic terms.


3. Are genes and DNA the same thing?

In a way "yes", and in another way "no"! Let me explain the difference. J. Martha

Please take a quick look at the image of DNA in the answer to the previous question - the famous double-helix of the DNA molecule is unmistakeable. But what is the purpose of this fascinating molecule? The ultimate purpose of DNA is hold the information that allows living things to develop and function. The complexity of living things requires many thousands of pieces of information, all of which must be stored by the DNA. This is where genes enter the picture.

Genes are segments of the DNA molecule that serve as units of heredity. Each gene carries a bit of information that helps direct the development of the organism. For example, a particular gene may carry information for hair colour, when expressed in the organism, results in red hair. A different version of the same gene with slightly different information may result in brown hair in the organsim.

So to answer the question, genes and DNA are really not the same thing, but genes ARE specific segments of the DNA molecule. In a particular chromosome (see question #2 above) there are large parts of the DNA molecule that are not genes - these parts of the DNA may be responsible for activating and deactivating genes, or they may be responsible for nothing at all.

Unit 3 Chemistry

1. Hi... I'm a little confused about something. Are the ions on the Data Booklet also  molecular compounds? Some of them are two non-metals joined and a molecular or covalently bonded compound is a compound that contains only non-metals.

Hi Nancy, besides being the author of the chemistry unit, I am a teacher at Stelly's Secondary School in Saanich, which is a couple of (metric) stone throws away from Buchart's Gardens. D. Lacy

Molecules, Compounds, and Polyatomic Ions

I'd like to start off with these ideas:

  • A molecule is a group of atoms connected to each other with covalent bonds and which have a fixed number of atoms. For example, CH4 is a molecular compound that contains 5 atoms covalently bonded. DNA similarly is a molecule with billions of atoms, but still with a definite number. Glass, on the other hand contains covalent bonds but is not a molecule because it is an array of atoms that extends indefinitely. (It is a network solid).
  • A compound is by definition electrically neutral. Physically, it is something that can be put into a jar. You can get a jar full of sodium chloride, but you can't get a jar full of just sodium ions, or just chloride ions. So no individual ion is considered a compound.

The polyatomic ions in the data booklet are definitely connected by covalent bonds. It would be correct to call them molecular ions, but this usage is not particularly common. They are definitely not compounds when taken individually, such as NH4+1 or  NO3-1 . When both ions are taken together they still are not molecular compounds, since they are formed from ions they are ionic compounds.

This means that compounds made of polyatomic ions have the interesting feature that they contain both ionic and covalent bonds.

 "A molecular or covalently bonded compound is a compound that contains only non-metals."

Here's a nit-picky distinction that I rarely share with my students: Compounds of non-metals have covalent bonds. However, there sometimes metals engage in covalent bonds too. The data table shows three of these: chromate and dichromate, which have a chromium oxygen covalent bond, and Hg2+2 which contains a mercury-mercury covalent bond. So although I don't go into the explanation with my students, I am careful about how I phrase these things.

Well, I hope I have covered off the right points without raising any new problems or too much overkill! But feel free to write back until it is all sorted out.


2. I wanted to know if you could explain what exactly are the purposes for an electron orbit and how it affects the atom?

Hi Naila, good question - thank you. Here's an answer for you. D. Lacy

We have to be careful about how we use the word 'orbit' when talking about the atom. When the word orbit is used on the provincial exam, it is better to think of it as meaning energy level. That is, a region of space surrounding a nucleus, in which the electrons have a certain amount of energy. The lowest energy level can have two electrons and the next one up can hold eight. The electrons don't fly around the nucleus like a fast moving particle. They just exist in all parts of the energy level all at once.

Counting the number of electrons in the energy levels tells us about how the atom can react. For example, oxygen has 6 electrons in its second energy level. It can hold two more electrons in this orbital, which tells us that oxygen is likely to form an ion with a minus two charge. Neon, which has 8 electrons in a full orbital is not expected to form an ion at all.

I would stay away from the term orbit. How did 'orbit' come into use? The Earth and other planets orbit the sun, which means of course that they move in a path around the sun. The planets are always in one particular place at any given time, but always on the move. An early model of the atom by the great physicist Neils Bohr treated electrons like a planet going around the Sun, but experiments showed it wasn't a very good model and he quickly abandoned it. He then came up with a much better model that is still in use today. Unfortunately the image of electrons whizzing around the nucleus keeps getting used even though it is wrong.

As you learn more about the atom in later courses, the model gets more sophisticated. Eventually is can explain a lot, such as why ruby crystals can produce laser light and why diamond is the hardest substance known. These come from a theory of matter called quantum mechanics, and Einstein and Niels Bohr were early thinkers on the matter. It is one of the two most successful theories in all of science.

But it does have some strange results. For example, consider that I am writing this note at the keyboard of my computer. The theory says that an electron in the lowest orbit, or energy level, of an atom in my finger exists all around the atom all at once. The amount of negativeness from the electron gets less and less as the distance from the nucleus increases. But - and this is a little strange, but as far as we know it is true - the negativeness never goes to zero. A tiny bit of it is in the wall next to my computer, even less of it is on Mars, and much less, but still some, is in the Andromeda Galaxy, 4 million light years away! How's that for the idea that everything is connected to everything else?!

Unit 4 Electricity and Magnetism

1. How do you describe and diagram magnetic field lines?

Considering the confusion with "magnetic north" and "geographic north" of the Earth, this can be tough to understand. But let's see if we can sort it out. J. Martha

Magnetic Field Lines

The first part of the answer is relatively simple. When you are diagramming and describing magnetic field lines, you always diagram them as running from the N-pole toward the S-pole of the magnet. So if you were diagramming the field lines of a simple bar magnet, it would look like this (note the direction of the arrows from N to S):

Another situation is when a wire has an electric current going though it. In this case, the magnetic field goes around the wire in a circular pattern. To determine the direction of the magnetic field you use the left hand rule.  Point your left hand thumb in the direction of the current and the way your fingers grab the wire is the direction of the field. This can be seen if you check out this page (be patient while it loads - it is a QuickTime movie).

If you are dealing with the Earth, this can be a bit confusing! Since the N-poles of magnets point to the Earth's "north" - there must be a magnetic south pole there. How did this situation occur - is it a mistake of science? Well, not really.

In the late 1500's William Gilbert studied natural magnets by floating them and suspending them on strings. He noted that they would always align themselves in a North-to-South orientation. Because of this orientation, Gilbert decided to describe the ends of the magnet according the geographic poles they pointed to. Gilbert labeled the end of the magnet that pointed to geographic North the "North-seeking pole" - the other end of the magnet was labeled "South-seeking pole".

Over time, the "North-seeking pole" of magnets has been shortened to "N-pole", or "N". Likewise for the "S-pole"or "S" end of magnets. Of course, N-poles are attracted to S-poles of magnets.  Therefore, if the N-poles of magnets are attracted to the geographic North of the Earth, according to Gilbert's system, which we still use today, the magnetic pole near Earth's geographic North must be an S-pole.

This may seem a little confusing, but what one must realize is that the magnetic poles really have no physical or scientific connection to the geographic poles of the Earth. While geographic North and South never move and will always be on the same place on a map, the magnetic poles actually move year to year.  Geologic evidence suggests that the poles actually "flip", on average once every 200 000 years. In fact, we are long overdue for a flip of the Earth's magnetic poles!

So the fact that there is an S-pole near the geographic North pole is simply a result of a centuries-old naming method for the poles of magnets that we still use today.


2. What is the difference between current and voltage? When you turn off a radio, have the electrons disappeared or not? Why? When objects are neutral and have a similar amount of protons and electrons, do they still repel and attract to one another?

Thanks for your email and your excellent questions. I'm the author of the Electricity unit for Science Foundations - hopefully I can help with your questions. J. Martha

Voltage and Current

The unit for current is amperes (often called "amps"), and the unit for voltage is volts. Voltage is a measure of how much energy electrons have, and current is how many electrons pass a point in a circuit every second.

It might help to think about the flow of water when trying to understand the difference between voltage and current. Imagine two waterfalls – one short, one very tall but otherwise similar in all respects. The water falling from the taller waterfall would reach a greater speed before hitting the river below, striking with a terrific splash. The water falling from the short waterfall would splash too, but with a much lower speed and not nearly as spectacular. The taller waterfall represents high voltage, the short waterfall represents low voltage. The higher the voltage, the more energy each electron has. Voltage is what makes electrons "flow" in a circuit, much like the difference in elevation of a waterfall makes water flow.

Current can also be visualized with water. Imagine two waterfalls of the same height, but one very wide and deep – the other narrow and shallow. The deep wide waterfall would have much more water flowing over it than the trickle of water coming over the narrow and shallow waterfall. More water passing a point every second means a greater current – and it's the same with electricity. More current means more electrons flowing past a point per unit of time.

Moving Electrons

Electrons don't disappear when you turn off a radio, but they do stop moving. With the radio turned off, there is no voltage applied to the circuit. Without voltage, there is no difference in energy to make the electrons move – so they don't. As soon as you turn on the radio, the voltage returns and the electrons start moving again, creating an electric current.

Neutral Objects

Two neutral objects will not attract or repel, because there is no net difference in charge. Protons are positive, and electrons are negative – so when they are in relatively equal amounts and spread out amongst each other, there is no area of net positive or negative charge.

Now, if I were to bring a negatively charged rod close to a neutral doorknob that would create a repulsion between the electrons in the rod and in the knob, making the electrons in the knob move away. This would create areas of net positive and negative charge in the knob, which could in turn result attractive and repulsive forces on other charged objects brought nearby.

I hope these answers have been of help to you – please don't hesitate to ask other questions if you need to.


Unit 5 Radioactivity

1. How can radiation help to cure diseases if radiation is harmful?

Good question. Sometime people think radiation can only be harmful. Here's an example, written as a short story, to answer your question. D.Lacy

Curing Cancer with the Help of Radiation

Steven Mulder stepped into the Iodine Radioisotope Isolation room at the Royal Jubilee Hospital in Victoria, BC, and turned to look again at Dr. Gurdip Singh. Dr. Singh was his physician and oncologist, or cancer specialist. Steven was relieved that his 6 week wait for radiation treatment was finally over, and that he had at last come to the front of the line for treatment. He was excited, but also nervous, because he was about to be injected with a form of iodine that releases enough radiation into his blood that fast growing cells in his body will be killed. This will include, he hoped, any cancer cells still remaining after the operation to remove his cancerous thyroid. His thyroid gland used to be located in the front of his neck. He reached up and felt the place where his collar bones met, and the small scar that marked the place where his thyroid gland was only three months ago. He was reassured that the special medication he was given would do the job that his missing thyroid no longer could. But what about the cancer – had it all been removed in the operation?

Dr. Singh waved to her patient. "Remember Steven, there is a very good chance that all the cancer was removed when your thyroid was taken out. We just want to be as thorough as we can be. If any cancer cells moved fro your thyroid to other parts of your body, this radiation treatment is very effective at killing them." Steven looked at the books he had brought along to read – a nine day supply. Once the radioactive iodine had been administered, he would be in isolation. No one could come into his lead lined room, and he could not leave. "And don't forget that those books and the clothing you are wearing stay here when you leave. They are now radioactive waste. You, however, get do get to come out!"

The technician had arrived with a heavy case, lead lined, and containing a freshly prepared dose of radioactive iodine. Steven stared at Dr. Singh "Don't worry, Steven.", she reassured him, "It's completely painless. Your biggest problem will be deciding which channel you want to watch when you get bored form sitting in here. In nine days you'll be playing baseball with your son again." Steven sighed, and asked again the question he had asked his doctor on almost every visit. "But, Dr. Singh, will it work – will it kill the cancer?"

Dr. Singh responded in a very straightforward manner. "Honestly, Steven, no one can answer that. But we are doing all that we can do to give you the best outcome possible. I just want you to know that the success rate for treatment of this kind of cancer is now very high. Remember that you went to your family doctor as soon as you noticed some symptoms, and so we were able to get your thyroid out quickly. Most people in your situation have no re-occurrence within five years of treatment.""Of course, from now on, you'll also glow in the dark." said Dr. Singh, with a smile. "What???" said Steven. "Just kidding," said Dr. Singh. "The half life of iodine-131 is five days. That means that five days from now, the amount of radiation you started with will be cut in half. Then five days later it will be half of a half. Here's a little problem for you: after 40 days, what percent of the original radiation you are starting with today will be left floating around in your body?"

"Thanks doctor", said Steven, "I'm glad I have nine days to try to figure that out. Do you have a calculator I could borrow? That is, if you don't mind it turning into radioactive waste?"


2. Is radiation a wave or a particle?

Actually, it can be both. Here’s how I would explain it. L.Sandner

Characteristics of Radiation

Radiation is energy in transit, and it comes in two basic forms: waves of electromagnetic energy and high speed particles. It may be energy moving from a rose petal to your eye, which you might describe as red light. This radiation moves in the form of an electromagnetic wave. Or it may be a high speed electron moving from the back of a television picture tube to the front of the screen, where it is used to help draw a TV image. This kind of radiation is in the form of high speed particles.


3. What is the difference between ionizing and non-ionizing radiation?

Ionizing and Non-ionizing Radiation

We can actually see many varieties of electromagnetic waves, and they are as varied as the colours of the rainbow. In fact, they are the colours of the rainbow: all the different colours that we can see are carried to our eyes in the form of visible light. Each colour is a slightly different form of electromagnetic energy, and each differs only in the shape of the electromagnetic wave. Our vision systems are amazing because they can detect these subtle differences. All the different kinds of electromagnetic waves taken together is called the electromagnetic spectrum. We will now examine the characteristics of the major components of the electromagnetic spectrum.

The differences are important, especially for life on Earth. J.Martha

One important characteristic of electromagnetic waves is whether they are ionizing or not. Ionizing radiation is radiation with enough energy that it can remove electrons from atoms, causing them to form ions. X-rays, from dental exams, and gamma rays, which arrive from deep space all the time, are both forms of ionizing radiation. Most ionizing radiation received by humans is absorbed by the water in our tissues, and causes no damage. However, as the dosage, or amount of radiation, we are exposed to increases, the chance that important chemical bonds will, such as those in our DNA, will be destroyed or altered, also increases.

On an evolutionary scale, changes in DNA are not necessarily a bad thing, because this it helps to cause genetic variation within a species. Such variation is very good for a population, because it makes the population more able to adapt to changing conditions. However, for an individual, such a mutation is more likely than not to cause cancer or serious disease. It’s best for our individual health to limit our exposure to high energy, ionizing radiation.

Many forms of radiation are non-ionizing, and cannot affect chemical bonds. Visible light and radio waves are non-ionizing. Microwaves are also non-ionizing. It is important to realize however, that even large amount of non-ionizing radiation can carry a lot of energy, and can harm people. It is now a historical fact that during the Cold War, Soviet (Russian) spies probed the American Embassy in Moscow with massive amounts of microwave radiation. Embassy staff had very high incidents of cancer during this time.


4. Is the wavelength and frequency of all types of electromagnetic radiation the same?

No, in fact each type of electromagnetic radiation has a different wavelength and frequency. D.Lacy

Wave Characteristics

Visible light, radiant heat, ultraviolet light, and radio waves are all major component of the electromagnetic spectrum. All of them can be considered to travel through space – even empty space - as waves. While scientists are still trying to understand how a light wave can travel through empty space, no one disputes that it is possible. To prove it for yourself, all you have to do is look up into the sky on a starry night.

Water can also carry waves. If a pebble is dropped onto the surface of a pond, a series of circular waves spread out from a central point. These waves have certain characteristics, such as the height of the wave, the speed at which the wave moves across the water, and how far it is from the crest of one wave to the crest of another wave. The last characteristic is called wavelength. A wavelength is the distance from one point on a wave to the same point on the next wave.

A wavelength is the distance from any point on a wave to the same point on the next wave.

Wavelength is one of the most important characteristics used to describe the shape of an electromagnetic wave. For example, knowing the wavelength of a light wave is enough to determine its colour. All light waves have extremely short wavelengths. For example, red light has a wavelength of about 800 nanometers, or 800 nm. This is a very small number. If the distance from the Victoria, BC to St. John’s, NFLD corresponded to 1 metre, then 800 nanometers would be the distance from one wall of a classroom to the wall on the opposite side of the room – about 5 metres. It is an unimaginably small distance. Yet, blue light has an even shorter wavelength – 400 nm, or about half the wavelength as red light. Not only can our eyes distinguish these differences in wavelengths, it can do so for a million different colours in between.

Radio waves have much longer wavelength, varying from the length of an ice rink, to the many kilometres. X-rays, incredibly, have wavelengths much smaller that visible light, corresponding to the size of a single atom.

Water waves have other important characteristics. If you have ever been to an ocean beach and stood in the surf as the waves pounded the shore, you will have a good feeling for the kind of energy that a water wave can carry. Electromagnetic waves, such as visible light and ultraviolet light, can also carry a significant amount of energy. In fact, all of the weather on the earth, all of the oil reserves in the ground, and all life on earth derive their energy through electromagnetic radiation, mostly as visible light, that traveled to the earth from the sun. Energy is certainly a very important characteristic of electromagnetic radiation.

The last characteristic of waves that we need to look at is wave frequency. Frequency is the number of wave crests to pass a point in a certain amount of time, usually in one second. There are many common examples of frequency. For example, when two children operate a skipping rope for a third person, who is jumping in the middle, it is easy to tell the frequency of the skipping. One way is to count how many times the jumper lands in one second. It is not very difficult to land twice per second. This is a frequency of 2 Hertz or 2 Hz. Hertz is a unit that means 'how many times in one second'. If the rope is skipped faster, doing ‘pepper’, it could easily reach a frequency of 4 Hz. This corresponds to 4 skips per second.

It is worth asking which frequency of skip rope involves more energy? Certainly, for the people operating the rope, as well as for the skipper, that the higher frequency will get them tired the most quickly. It turns out that for all waves, including the sound waves produced by skipping ropes, and also by electromagnetic waves, that the higher the frequency, the greater the energy that is carried by the wave. This is always true: the higher the frequency the greater the energy that is carried by the wave.

The frequency unit, Hertz, is named after Heinrich Hertz who was the first person in history to broadcast and receive radio waves. Of course, radio waves are a kind of electromagnetic radiation. In fact, FM radio uses frequency to identify radio stations. For example, CBC radio in the Lower Mainland and Vancouver Island broadcasts at 690 kiloHertz, or 690 kHz. This is 690 on the radio dial and corresponds to a frequency of 690 000 wave crests per second.


5. I always get the wavelength, frequency, energy relationship mixed up. Can you summarize this to help me remember it?

This is an important relationship, so I’ve summarized the key points below. J.Martha

Wavelength, Frequency, and Energy Relationship

The relationship between frequency and wavelength is called an inverse relationship. This means when one value goes up, the other one goes down, like a see-saw in a playground (Figure B5.2 page 197). For example, if the frequency of a wave increases, the wavelength decreases.

This means that for any kind of wave, the wavelength, frequency, and energy carried by the wave are all related.

Short wavelength, high frequency, and high energy go together.

Long wavelength, low frequency, and low energy go together.

Figure B5.3 on page 198 of the text shows the different forms of electromagnetic radiation that occur in nature. There are many different forms of electromagnetic radiation, such as radio waves and ultraviolet light. Each one has its own range of wavelengths and frequencies. You do not need to memorize the diagram of the electromagnetic spectrum in Figure B5.3, but you should be able to use it to help you understand the characteristics of the different forms of radiation.

A key idea to remember is how the frequency-wavelength-energy relationship applies to the electromagnetic spectrum. On the left of the spectrum, the long wavelengths have a low frequency and low energy. As the wavelength gets shorter, the frequency gets higher and the energy increases. This means that AM radio waves have less energy than TV waves do, and X-rays have more energy and a shorter wavelength than both radio and television waves.


6. I have trouble understanding the concepts of radioactive decay. I was doing some questions from the unit review worksheets that my teacher downloaded from your website. # 32 asks: "Approximately how much daughter product would be found in a 15-million-year-old rock sample?" (Use the radioactive decay chart for  "shannonium" below to answer questions 31 and 32). I just don't get what a daughter product is and why the answer is 35% instead of 65%.

Another question relating to that is #35 - "After 3 half-lives, a rock sample contains 70 grams of the daughter product of a radioactive isotope. How many grams of the parent radioactive material did the rock originally contain?" I put down 280 as the answer but the  correct answer is 10 grams. I don't see why that is the case.

Hi Joanna: Thank you for your questions. Don't feel bad, radioactivity is a tough subject. Your questions are very good ones. Lets tackle them in order. J. Milross

Decay Problems

With regards to daughter product: gtradioactive isotopes tend to be unstable, that is, they give off energy in the form of alpha, beta and gamma radiation. Because the isotopes are the material we start with, we call them "parent material". When the parent material gives off this radiation, it is called decay. After a radioactive isotope decays enough, it becomes stable. This stable material is called "daughter product" (because it was produced by the parent --- although, I have two teenage daughters, and I am not sure I would refer to them as "stable"...) and usually does not decay any more. By knowing how fast an isotope decays, and determining the amount of parent and daughter material is in a rock sample, we can calculate the age of the rock sample.

You were correct in your answer to 32. It should be 65%. After 15 million years, there will be 35% of the original shannonium in the sample. There will be 65% of the daughter product in the sample. I checked the answer key, it is correctly marked "D". I wonder if there was a mixup with the exam keys because we have the unit exam from the book, and  another unit exam available online that the teacher can use.

For question #35, the correct answer is 80 grams. P= parent material; D= daughter product (in grams)

  • After 0 half lives: P = 80 (100%) D = 0 (0%)
  • After 1 half life: P = 40 (50%) D = 40 (50%)
  • After 2 half lives: P = 20 (25%) D = 60 (75%)
  • After 3 half lives: P = 10 (12.5%) D = 70 (87.5%)

Some quick math: if X is the original amount of parent material --> X x 87.5% = 70; or X = 70/.875 = 80

The correct answer is C, 80 grams. It can be done with fractions, as well, but I will leave that to your teacher to explain.


Unit 6 Earth Forces

1. Where exactly is the Mid-Atlantic Ridge?

2. How do we know the locations of all the trenches and ridge in the world?

Hi Katie: Thank you for your questions. Lets tackle them in order. J. Milross

Trenches and Ridges

This is going to sound silly, but the Mid-Atlantic Ridge IS actually near (but not exactly) the middle of the Atlantic Ocean. It is the reason there is an Atlantic Ocean. 200 million years ago, South America and Africa were part of one big continent (Pangaea). A rift opened up right down the lower middle of this big continent splitting it apart. South America went one way, Africa went the other. A rift is a diverging plate boundary, where magma comes up from the mantle, and (kind of) pushes plates apart. Because we are dealing with such huge chunks of land, the movement is not exactly even on both sides. So to say the ridge is exactly in the middle of the ocean may not be completely accurate.

One thing to keep in mind. The Mid-Atlantic Ridge is not a perfect crack in the oceanic crust, but rather a series of little cracks that are joined together. The pattern is similar to a zig-zagging  zipper. [I hope that makes sense to you]

We know the locations of trenches and ridges because geophysicists and oceanographers have studied the bottom of the oceans using sonar (sending sound waves to the ocean floor, and studying the "echo", just like ultrasound used to "see" babies inside their mother's womb), seismic waves (caused by earthquakes), and x-rays to observe the oceanic crust as if  there were no water in the way. Trenches occur where two plates are colliding (oceanic - oceanic, or oceanic - continental), and ridges form when two plates  are moving away from each other (in the ocean, these are called ridges; on land, they are called rifts). By studying the movement of the plates, scientists could anticipate where they should expect plates to be coming together, or moving apart.

Thanks again for your great questions, and for using our book. If you should have any other questions, please don't hesitate to contact us. Remember: Earthscience Rocks!

3. What are the benefits of living near active volcanoes?

Hi Ashley: Thank you for your question. At first glance, living next to a volcano doesn't seem like a good idea. Personally, the thought of front row seats to a violent eruption sounds a little too extreme for this science teacher. J. Milross

I suggest there are two main benefits to living next to a volcano:

1. Volcanoes occur in areas where there is magma  (molten rock) under the ground (that's why volcanoes happen - the magma makes it to the surface). The magma is very hot, and heats up large areas surrounding it. Water trapped in rock underground gets heated by the magma, and can come to the surface as a geyser, or a hot spring. These features can be used to generate hydrothermal power, or be used for hot water, or the heating of homes. Harrison Hot Springs uses hydrothermal springs (heated by magma) to attract tourists.

2. When volcanoes erupt, they send a great deal of ash into the air, which covers large areas of land. This ash is rich in nutrients (nitrogen, potassium, etc), which makes for ideal fertile soil.  Trouble is, you're farming next to a volcano...

I hope this helps. If you have any other questions, please do not hesitate to ask. Thank you again for your thoughtful question, and thank you for using Foundations 10. Best of luck.

4. How does the presence of glaciation in places like India add credibility to Wegener's theory?

5. What does looking at the Earth's surface tell a geologist about what is happening underground?

6. What are two different uses for a geological map of an area?

Here is a response from our Earth Science author, J. Milross.

The Earth's Surface

4. India sits across the equator, and is currently considered tropical in many areas. Even low elevation areas show evidence of large ice sheets having once covered most of India. This evidence, (glacial scratching, deposits, and u-shaped valleys), does not make sense for such a warm area. The pattern of the glacial evidence also does not make sense for India in its present position. It does make sense, however, if India is part of Pangaea, and is moved to its position 200 million years ago, much further south, towards the pole.

5. Geologists will look for evidence on the surface that reveals what is going on underneath. For example, a steep, flat-sided cliff may suggest a deep fault. A small area of rock that stands out from the rock around it may indicate igneous rock that cooled underground, solidified, then had the rock layers above it removed (through erosion). A hilly area may indicate the presence of magma deep underground causing the surface to buckle. Rounded hills may indicate tectonic forces being applied.

6. Searching for: mineral resources; sources of water; areas that are safe to build houses, buildings, or highways; areas that are suitable for farming; areas that may be subject to earthquakes; etc.


7. I was just wondering, what's the answer to - "How do geologists determine the start and end of an era?" 

Hi Lilian: Thanks for your question. I hope this helps:

Eras

On page 234 of the text, the third paragraph describes the divisions of the geological time scale being determined by things like rock types, fossils, etc. The eras are usually divided by the first appearance, or the last appearance of a group of organisms. For example, the beginning of the Cambrian period was marked by the "Cambrian Explosion", a time when there was an incredible amount of diverse (really strange and different) life forms first appearing on Earth.

Thank you again for using Foundations 10. Good luck on your final. Sincerely, J. Milross

8. What does the magnetic pattern in the bands of rock suggest about the formation of the sea floor?

9. Why are the magnetized particles in igneous rocks on the sea floor are not all pointing in the same direction?

Magnetism and the Sea Floor

Hello, and thanks for your question. We asked our Earth Science author and here is his reply. Good luck on your upcoming exam.
As molten rock cools at spreading ridges on the seafloor, magnetic minerals in the magma align to magnetic north. The minerals act like little compasses indicating the direction of Earth's north magnetic pole. When the rock solidifies, the magnetic minerals remain aligned. Every once in a while, the Earth's magnetic poles flip (i.e. north is south, and south is north). The rock that forms during one of these flips will show a magnetic north in a different direction. The spreading seafloor is a history of magnetic flips (reversals) in the Earth's poles. When a magnetic survey is taken across a spreading ridge, the north and south patterns form bands. This helped prove the plates are moving - they are pushed apart at spreading ridges.
bcscience.com

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