Rocks and Minerals

3 Comments

In the comments of their poster entitled “Welcome to Grade THREE!”, the Battalion Bloggers asked some questions. Posts lead to questions and questions to a search for answers. Below is the next part of our shared learning journey as I attempt to find answers and learn more along the way.

For their original post…

Welcome to Grade THREE!

For the related preceding post on this blog...

The Outback and Other Information

Hello Battalion Bloggers,

I know you're having are busy in school at this time and I have been very busy with DVD/CD work for schools and community groups so it seems it can take us some time to reply to each other but our contacts are always interesting.

I thought I would share some ideas I had when thinking about the questions and curiosities in your comment. I know some ideas I share can be a little hard to understand at times but this is what can make learning interesting as we try to discover meaning. To answer you, I always have to research more information, try to understand what I find and then try to explain what I find in in a way you can more easily understand. Our posts and comments means our learning journeys cross for a time. Here's what resulted...

We are glad that the perentie and lace monitors are only slightly venomous and that they are shy and will run away when they see people. Can the perentie and lace monitor venom kill a person if they bite them?

In the original post, I mentioned the monitors are thought to be slightly venemous but I haven't heard of any deaths from monitor bites in Australia. Some of the effects of a monitor bite from lace monitors or Komodos might be (according to Wikipedia's Komodo reference) rapid swelling, localized disruption of blood clotting, and shooting pains, with some symptoms lasting for several hours. The large Komodo has been known to attack and kill animals such as goats and there are reports of human deaths. As with all animals, we should be careful with the biting end and leave wild animals alone.

Perentie

This graphic has been sourced through Wikimedia Commons and is listed as in the public domain.

This graphic has been sourced through Wikimedia Commons and is listed as in the public domain.

Lace Monitor

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

We wonder why the komodo dragon is only found in Indonesia now and not in Australia anymore?

Komodo Dragon

The photo was sourced through Wikimedia Commons where it was listed as in the public domain.

The photo was sourced through Wikimedia Commons where it was listed as in the public domain.

Different species of monitor lizards are found in many countries. According to Wikipedia, they are found "through Africa, the Indian Subcontinent, to China, down Southeast Asia to Indonesia, the Philippines, New Guinea, Australia and islands of the Indian Ocean, and the South China Sea. A large concentration of monitor lizards occurs on Tioman Island in the Malaysian state of Pahang." What this suggests is there are many species of monitor lizards. The Komodo, perentie and lace monitors are just three.

HOW could they get to Indonesia when they once roamed Australia?

In my post, I mentioned fossils of Komodo dragons were found in Australia so they had once been here. If you look at the Komodo Dragon Evolutionary History link, it mentions recent fossil finds in Australia suggest it's possible Komodo dragons evolved in Australia and spread to Indonesia when sea levels were much lower during the last glacial period (around 12,000 to 110,000 years back). With the end of the glacial age, they were cut off from Australia by rising waters.  Perhaps a changing environment wasn't suitable for them here in Australia so they died out leaving the Komodo only in Indonesia. We would need more information to be certain but, at this time, an accepted belief is the monitors evolved in Asia perhaps 40 million years back and then spread.

We also have evidence of much a much larger monitor lizard in Australia known as Megalania (Megalania prisca or Varanus priscus). It is thought to have died out 30,000 to 40,000 years back so it's possible the earliest indigenous Australians had seen them. Most recent estimates say they might have grown to 4.5m (15 feet) and weighed up to 331kg (730lb). With the largest wild Komodo measuring 3.13 m (10.3 ft) long and weighing 166 kg (366 lb), the megalania would have been huge. I wouldn't go hiking in our national parks if they were still around.

The photo was sourced through Wikimedia Commons where it was listed as in the public domain.

The photo was sourced through Wikimedia Commons where it was listed as in the public domain.

We wonder if they lived in both places but then they died out in Australia.

I liked your suggestion and suspect there was a time when they were found in both places. Somewhere back in time monitors must have had a common ancestor. The different species evolved when populations were cut off from others. Adapting to the local conditions, in time they developed differences to other populations. When there is enough change so one population is unlikely to breed with another*, they are said to be a new species. Look at the monitor lizard below. It is a varanus salvatorii (Salvatori's monitor) from New Guinea.

Do you notice all of the monitor lizards on this post have similarities? They are all part of the genus varanus (monitor lizards).

Do you see they also all have differences? The differences suggest different species.

Salvatori's Monitor Lizard

The photo was sourced through Wikimedia Commons where it was listed as in the public domain.

The photo was sourced through Wikimedia Commons where it was listed as in the public domain.

New Guinea's Salvadori's Monitor Lizard

* There are examples where animals of different species can interbreed (have babies together) so long as the animals are of the same genus.

horse (equus ferus) + donkey (equus tigris)= mule   

(equus is the genus and ferus/tigris are the species names)

male tiger (panthera tigris) + lioness (panthera leo) = tigon

male lion (panthera leo) + female tiger (panthera tigris) = liger

(panthera is the genus and tigris/leo are the species names)

Why would they die out?

As mentioned above. the Komodo dragons may have died out in Australia because of climate change. As an example, when the first people came to Australia perhaps fifty to sixty thousand years ago, Australia was much wetter with forests and lakes. In time, changes in climate led to Australia drying out leaving desert where once there was forest. There might have been other reasons why they became extinct in Australia but, without evidence, we're only guessing.

Spike is SO cute! We think that the picture of the echidna digging his claws into the grown and curling into a ball to protect himself was SO cute! Do echidnas get frightened easily?

Echidna

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

When I discovered an echidna in my garden, it was probing the soils with its snout in search of food. It didn't take much notice of me and I suspect their eyesight isn't too strong. When I came too close, it dug its claws into the ground and showed its spines. I don't think they are too easily frightened but, just like you, they are careful if danger is near.
Once they feel danger has gone, they go back to their hunt for food.

We wonder if they do much damage to gardens like voles can do?

If I hadn't seen the echidna in my garden, I don't think I would have known it had been there as they leave little trace. It's possible others have been in my garden but I have only ever seen one. I have seen many in the wild. I saw the above echidna waddling its way across a local park. Even though I was close, it either didn't see me or wasn't frightened.

We wonder what they like to eat … besides ants!

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

In the wild, the echidnas mostly eat ants and termites. The above photo shows a local termite mound around 1m high although I have seen some termite mounds much higher in other parts of Australia. When hiking, I sometimes see termite mounds where I can tell echidnas have been using their strong claws to dig. Once opened, the echidna can use its long, sticky tongue to catch ants or termites.

My favourite local animal sanctuary, Potoroo Palace , has three echidna. It isn't possible to gather enough ants or termites for them so the keepers mix a special recipe to feed their echidna. The mix includes minced meat, olive oil, raw egg, glucose powder, baby porridge, processed bran, vitamin E powder and calcium powder. In the video below, you will see Spike enjoying a meal as the keeper shares information with tourists.

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We wonder how small an echidna’s egg would be. We STILL think it’s SO cool that they are egg-laying MAMMALS like platypuses!

Echidna eggs are only about 2cm across. The females produce only one small egg about two weeks after mating. It's egg is placed in a backward facing pouch where it hatches about 10 days later. The baby echidna (known as a puggle) stays in the pouch for about two to three months before it's ejected from the pouch. It's spines start to develop in the pouch. Can you imagine a mother with a spiky baby in it's pouch? Perhaps when the puggle gets too spiky, mum thinks it's time for baby to leave the pouch.

How BIG do echidnas grow … we wonder if our Grade Six teacher would be a GOOD referent for measuring an echidna!

Long-beaked echidna can be 45cm to 100cm in length and weigh around 4kg to 9kg. The short-beaked echidna in my area  can be around 30cm to 45cm in length and weigh 2 to 7 kg.

We really enjoyed seeing all the pictures of your fieldtrip to the Outback! It looks like hardly anybody lives there. It would probably be a hard place to live because it looks like there aren’t any stores around to get food or water. It looks SO hot too!

 Summer temperatures in Australia can reach over 40C in summer. There has been a few examples measured up to around 50C. My first full time school wasn't in a desert area but was in a semi-arid (not quite desert) area. I recorded a maximum temperature in the shade of around 45C for two weeks running. As the sun goes down, the temperatures in Australian deserts can normally drop down to around 3C to 6C and there have been recordings of temperatures as low as -7C in Alice Springs in winter.

We loved Ayer’s Rock and the Devil’s Marbles at Karlu Karlu. We wonder how those rocks got stacked like that. They look like they could fall off at any moment! We wonder how long they’ve been stacked like that...

Karlu Karlu

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

Schools and students have permission to use this graphic for non-commercial, educational purposes.

Schools and students have permission to use this graphic for non-commercial, educational purposes.

In the top photo, you can see Karlu Karlu has many such granite rocks but they haven't been stacked. The second photo gives you an idea of how large they can be. The man in the photo is standing on and leaning against the same rock. Erosion by rain and wind has been at work wearing away the rock at what looks like the base of the upper section. The upper section will eventually break off and fall. Maybe it already has. The photo was taken 28 years back but the erosion is a slow process.

… and also how old Ayer’s Rock is! It just looks like a place where tons of poisonous snakes and spiders would live.

Uluru is known as a monolith (single stone) and is sandstone. The sandstone was thought to have been deposited perhaps 550 million years ago. There are snakes and spiders around Uluru but I think the snake is the woma python. Being a python, it isn't poisonous. There are poisonous species of snakes in my area near the coast. They are the red-bellied black snake, brown snake, tiger snake, and death adder. I have seen the first three in the wild but, as yet, haven't seen a death adder.

Do armadillos live in the outback?

Armadillos aren't native to Australia.

How long and how tall is Ayer’s Rock?

It is really much larger than what you can see in the photos. Most of it is below the surface. If you were to go for a walk around the base of the Uluru you see in the photo, it would be a walk of a little over 9km (~6 miles). The second photo gives you an idea of how high it is. You can see people have climbed to what looks like the top although the real highest point on Uluru is 348m above the base and is to the left and not quite in the photo.

Uluru  (Ayers Rock)

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

Uluru Climb

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

 We LOVED all your pictures of the outback. We loved how you told us that people would build their houses underground to stay cooler. How would they get to their houses?

Coober Pedy

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

Coober Pedy's underground homes can be basic but I have been inside one I would consider more luxurious. It included a swimming pool with a walled part built out of the home. Like most homes, it had a front door, rooms, furniture and electricity. While there are no windows in walls, there are vents in the ceilings for light and air.

What would happen if a rainstorm came … would those houses get flooded?

Being in an arid area of Australia, its average yearly rainfall is only about 156mm (about 6") so flooding isn't too much of a problem. The homes also tend to be built into hills and not low where water might be a problem.

Do the houses leak when there is a rainstorm?

Low rainfall means having leaks would be a rare but I guess they would have big problems if climate change brought much higher rainfall. People find being underground is more comfortable where summer temperatures have reached as much as 47C although the average summer temperature is 30-32C. The big attraction for living in Coober Pedy is the opal. Opal is mined and made into jewellery.

Wouldn’t it be hard to dig into the ground to build a house?

Many in Coober Pedy are miners. They can use digging machines to dig mines in search of opals or to dig homes. Early settlers probably used a pick to dig their homes. Imagine, you don't need bricks or timber if you want a new room, you just need a place to dump what you dig. If you're lucky, you might even find opal when digging your house.

I thought I had a photo of a home interior but I haven't as yet located it amongst thousands of old photos so below is a photo I found through Wikimedia Commons.

This photo was sourced through WIkimedia Commons. The information below shows the original author.

This photo was sourced through WIkimedia Commons. The information below shows the original author.

Description: Coober Pedy, South Australia - underground house display.        Date: 26 August 2003     Author: Nachoman-au

Couldn’t it cave in?

The home I visited looked very solid. Experienced miners would know the danger of cave-ins if they weren't careful. You would probably find the town has rules on how dugout homes should be built. I suppose a serious earthquake might cause problems but serious earthquakes are rare in Australia.

We wonder, if they go out, how do they find their houses again, if they are underground. Do they mark an x on the roof?

Like you finding your home, they know where their homes are in town so they wouldn't need to mark their homes. They might simply remember it's on the north side of the third hill from the local shop.

We wonder what kinds of animals live in the outback.

That is a big topic so let's look at the area around Uluru. Go to the Wikipedia reference on Uluru and scroll down for some details.

There are known to have been 46 mammal species found around although there are currently only 27 including bats. There are also birds, reptiles, insects and frogs. Frogs in the desert? There are four known species of frogs found around the base of Uluru where you also find waterholes. There can also be introduced animals such as mice, camels, dogs, foxes, cats and rabbits.

emus

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

camels

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5 Comments

Hello Heather and Keira,

Firstly, let me apologise for taking two weeks to reply to your question. It has been a very busy time working on a project for a choir but I now have two weeks before the next project starts so it's time to catch up.

I now have another post for you but it may be challenging to understand some of its content. I have found the more I learn, the more I realise how little I know. Checking ideas and information for you and others when I write a post can often challenge my understanding but its by challenging ourselves to understand we can learn.

 

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

Back on the "How did Earth begin?" post I tried to answer your challenge. Like all good enquiring minds, one idea can lead to another so, in the comments section, you added...

 In one of the paragraphs, we noticed that you talked about possible life on Mars. Keira thinks that over time, the sun will come too close to Earth, and Earth might shatter. That might be a possibility. There is one problem though. Martians could have died, but Mars didn’t shatter. Do you think that WE are Martians CHANGED into human?

Our minds can be a very powerful weapon against ignorance when we have curiosity and a will to find answers. This is particularly important for science as it tries to find the answers to questions. As lovers of science, your curiosity can lead you in all sorts of directions. I know mine does as I try to find answers. Let's look at a simple answer...

Do you think that WE are Martians CHANGED into human?

It's possible.

Too quick an answer?

Let's put it this way, I'm not comfortable completely ruling out many ideas. It is possible first life on Earth came from Mars but I don't think it's likely.

Here's some mind blowing maths for you. Just say you shuffled a deck of playing cards and put four down on the table...

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

When you put down the first card, the chances of it being a 7 of Diamonds is 1 in 52 because there is only one 7 of Diamonds in a deck of 52 cards. To then put down a 3 of Clubs, the chances are 1 in 51 because there were 51 cards left.  For the King of Spades, it's one in 50 and, for the 10 of hearts, 1 in 49. So what is the chance of dealing just those four cards in that order from any normal deck of cards...

The chance of dealing those exact cards in that order is only 1 in 6,497,400 ... (52 x 51 x 50 x 49 = 6,497,400). It's not very likely we would get those exact four cards in that order if we shuffled and dealt four cards again but it is possible. Of course, a magician or a card trickster could cheat to get the results over and over but then the cards aren't random.

This type of maths looks at probability, i.e. chances of something happening. If we only have one card and it's the King of Clubs, the chances of dealing a King of Clubs is one in one or 100%. The chances of dealing a 7 of Diamonds is zero in one or 0% because we don't have that card. Can't maths be amazing?

For really mind blowing maths, go to the end of this post where I work out the chances of dealing out all 52 cards in an exact order, at least if I have the maths correct.

Where Did Life On Earth Come From?

I know of two main ideas for the origin of life according to science.

1. The Primordial Soup

This idea suggests billions of years ago, chemicals became concentrated (thicker) in pools of water (the primordial soup). By chance, these chemicals were able to form amino acids (the basis of life including us). In time, they combined to make more complex compounds and eventually life. This process is known as abiogenesis.

The chances of life in this way would be seen as very unlikely but, if this process is correct, it did happen. Look again at the card example in "The REALLY Mind Blowing Maths" at the end of this post. The order of cards I dealt was very unlikely but it did happen.

2. Panspermia

Some theorists suggest life might have evolved elsewhere and was brought to Earth on meteorites (Panspermia). This might be better suited to the idea life on Earth started on Mars. If life had started on Mars, a meteor strike might have thrown Mars rock into space and it may have made it to Earth but, then again, life on Earth and Mars might have come from anywhere in space. Remember, if it was life, it would have been very simple, possibly single cells, not animals like us.

No, if you watch the video clip to the end, I don't believe aliens are experimenting with us. It is possible but very unlikely. 🙂

What does Ross think?

The first idea can explain how life itself could have started, whether here or somewhere else in the universe. The second suggests how life might have made it to many places in the universe. Think of it, life might have started in many places in the universe and been spread to the stars, or at least their planets.

Did Mars Once Have Oceans and Rivers?

One of the important resources for life as we know it is liquid water. There is evidence rivers, lakes and oceans once flowed on Mars but liquid water hasn't been seen on Mars. Much of the water was probably lost to space long ago. There is plenty of evidence water as ice is found at the Martian poles and growing evidence it is to be found in the rocks and soils so life may well exist there waiting to be discovered but don't expect anything like animals running around. It's very unlikely intelligent life ever existed on Mars but is likely life did and/or does exist.

You have questioning minds so I suspect you're wondering, what happened to the Martian oceans and rivers?

Here is a video looking at the way Mars may have lost much of its atmosphere...

You may have understood the idea energy from the sun (the solar wind) caused Mars to lose most of its atmosphere so you might wonder why this didn't happen here on Earth.

Why did Earth keep its thick atmosphere while Mars lost much of its atmosphere?

Let's first look at the photo I prepared for you. It's made by placing a magnet under a piece of paper then sprinkling iron sand over the paper.

 

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

The lines you can see in the sand help us see the magnetic field of the magnet. You can see the lines run from one end to the other of the magnet. The Earth also has a magnetic field because of its rotating iron core in its centre. The iron core helps create a much stronger magnetic field than on Mars. It protects us from much of the solar wind. Think it of a little like an umbrella in the rain.

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

Earth's umbrella (magnetic field) is stronger than that of Mars so we get better protection. Below is a NASA diagram showing the magnetic field of Earth. If Earth's centre cooled and slowed reducing our magnetic field or solar wind became stronger, Earth would also eventually lose much of its atmosphere.

This NASA graphic was sourced through WIkimedia Commons where it is listed as in the public daomain.

This NASA graphic was sourced through WIkimedia Commons where it is listed as in the public domain.

 Keira thinks that over time, the sun will come too close to Earth, and Earth might shatter. That might be a possibility. There is one problem though. Martians could have died, but Mars didn’t shatter.

 Watch this video clip...

In this model of Earth's future, the Earth would eventually be pulled towards the sun and, in a sense, "shatter". Its matter would turn to plasma, a major part of the sun. I have shown Mars didn't lose much of its atmosphere because it shattered, it was lost because it didn't have a strong enough magnetic field to protect it in the way Earth is protected.

I found another video but it is harder for you to understand. It was made by a college student as an assignment looking at the life of the sun. At the stage where our sun becomes a red giant life would no longer be possible on Earth but we are looking billions of years into the future. In this model, it's not so much that the sun comes closer, it grows larger.

What will really happen in the Earth's future? Trying to find answers to what, how and why is the reason science is so interesting. We can observe, gather data, carry out experiments, discuss our ideas with others... When we have enough evidence, we can make an hypothesis (the next step up from an idea). If others find evidence supporting our hypothesis, it can take the next step and become a theory. Theories are the strongest ideas because they have much evidence to support them.

What's my idea about Earth's future? Perhaps when the sun starts threatening life on Earth, someone will press the reset button and the sun will return to a safer stage but that's even less likely than dealing the cards in the exact order below five times in a row. 🙂

The REALLY Mind Blowing Maths

Okay, the card maths at the beginning of this post seems mind blowing but it gave me an idea. If I was to deal out all 52 cards from a shuffled deck...

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

then shuffled the cards and asked you to deal them out in that same exact order, what would the chances be of dealing all 52 cards out one at a time in exact order without cheating or using magician tricks? Here would be the calculation...

Chance of dealing all 52 cards in an exact order = 52 x 51 x 50 x 49 x 48 x 47 x 46 x 45 x 44 x 43 x 42 x 41 x 40 x 39 x 38 x 37 x 36 x 35 x 34 x 33 x 32 x 31 x 30 x 29 x 28 x 27 x 26 x 25 x 24 x 23 x 22 x 21 x 20 x 19 x 18 x 17 x 16 x 15 x 14 x 13 x 12 x 11 x 10 x 9 x 8 x 7 x 6 x 5 x 4 x 3 x 2 x 1

and what answer did I get?

The chances are one in ~80,658,200,000,000,000,000,000,000,000,000,000,000,000,

000,000,000,000,000,000,000,000,000.

In maths, the tilda (~) is used to mean approximately (about).

The chances of dealing all 52 cards in an exact order is so small most would think it's impossible but I had done it the first time and, by chance, you might be able to do it but it isn't very likely.   🙂

4 Comments

Keira left a quality comment on a blog post.

What Stone Is That? - for Mrs. Yollis and class

Hello Keira,

Your rock has certainly caused much thought as we have tried to uncover its secrets. Science can be like that, a chance to uncover mysteries. After leaving a reply to Heather's quality comment, I found you also left a quality comment.

Here is a link to the information I shared with Heather...

What Stone Is That? - A Follow Up Post for Heather

This photo was supplied by Mrs. Yollis and class.

This photo was supplied by Mrs. Yollis and class.

Now for your comment...

Do I know why your rock looks amber on the outside?

From the picture, I'm not able to see the amber colour on the outside. It may be just the remainder of stone or dirt once surrounding your rock. Look at these photos. The first shows a collection of four geodes, one complete. The second shows a geode containing amethyst (mauve quartz). If you look closely, you can see the colours on the outside aren't always the same as the colours inside the geodes. There are other minerals probably once from the surrounding rock. Did you notice one in the top photo has a yellowish outside?

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

It's also possible some citrine quartz crystals might have started to form on the outside. The picture below shows citrine quartz in the paler rock. We can't be certain unless your rock is checked but, no matter what is on the outside, I found your rock very interesting.

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

About Galena

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I like your description of galena. It does look a little like tinfoil. Tin (Sn) is an element as is the metal in galena. Galena is lead sulfide (PbS). It's where we get much of the lead (Pb) we use. Below is the heaviest sample in my collection. It's not the biggest in size but weighs 2500g (5.5lb). The gold coloured part of the sample is iron pyrite. It also contains zinc (Zn) but is mostly lead (Pb) in the form of galena. The small whiter patches on the lower left are quartz. The sample comes from one of my state's major mining areas, Broken Hill.

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Click on GALENA and it will take you to a Wikipedia page on galena. You will see where it can be found around the world and in U.S.A..

How do you find out all these facts?

I have been interested in very many subjects over the years. When I see something interesting, I sometimes remember facts and information I think might be useful in an extended comment. As I write, I start looking for more information and learn as I go.

For geology, I have assorted books and I can also search online. I always try to check the information I share on blogs because I'm not an expert in any area. Like you, I'm a learner. I've just had more time to learn.

Where did you get all these rocks?

Most of the samples I have were bought in rock shops with only some being collected by me. Many come from countries I have never visited. As an example, the big round geode and the one cut in half beside it are from Brazil. While it can be fun searching for your own samples, collectors often have to buy samples of rarer minerals or ones found in other countries. I have been collecting stones and crystals since I was about your age. It's just a matter of keeping your eyes open  in many cases. Look at these...

The first sample caught my attention because I could see crystals in it. Could it be a geode waiting to reveal something special inside? Perhaps I might one day break it open to find out.

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

This one is a geode from Queensland. You can see the crystalline mass in it. Perhaps cut and polished, it could look very good but I like it as it was found.

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

This rock was very interesting when I found it. You can see it also has a yellowish exterior like your rock but some chips broken off the rock have revealed what could be agate. I suspect this sample could look very impressive if cut and polished. The material inside might look like your rock.  As I don't have access to a diamond saw to cut it, I keep it as it is, a mystery.

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

A Hand Painted Geode?

"...Geodes, the first one looks interesting to me. The middle almost looks like it is hand painted. Was the middle polished or was it like that when you discovered it?"

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

I must say this sample looks as though it's the work of an artist. What I believe has happened is, as different minerals have mixed as the crystals formed in a space, different colours were formed. In this geode, crystal growth has filled the space.

I saw this cut and polished sample in a rock shop. It was the pattern you noticed that caught my attention.

In the middle of the rock that is cut open it looks like there is a little nook. Am I right?

 

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

You are a very observant person. There does seem to be a little nook in the cut rock but it is due to the way the crystals have grown inside the geode. Along the inner cut edge, you can see the crystals aren't even like a circle but have some areas thicker than others. This unevenness means some areas extend out over the others. Sunlight on them leaves a shadow below. In the shadowed area, the crystals look much like the small crystals in the middle.

Considering your curiosity and interest in rocks, I hope you keep learning and discovering. A mind with curiosity can be a very powerful learning tool.

In a previous post,

"What Stone Is That? - for Mrs. Yollis and class"

Heather provided a quality comment needing to have a reply including a little more than words.

What Stone Is That?

This photo was supplied by Mrs. Yollis and class.

This photo was supplied by Mrs. Yollis and class.

Heather, one of the best things about sharing learning through blogging is the way we can exchange ideas so easily no matter where or how far we are apart. Your comment was an example where we both learn from each other. Reading what you shared, I realised I would need to share extra graphics to give you some answers.

Your suspicion the rock might have been microline had me examine the microcline more closely, something you can't do easily from a picture. When I looked closely, the way the crystals had formed suggests Keira's rock wouldn't be microline. Her rock looks too smooth to match the microcline sample I have. Your observation was good even if it may not be correct. My suggestions might also be wrong.  It's by presenting different ideas and solutions science gets understanding. Your comment meant I had the chance to think about and research other ideas. 🙂

How Quartz/chalcedony/agate forms...

A concentric, banded, fibrous variety formed by precipitation from watery solutions in rounded cavities in lava rocks (geodes), sometimes with beautiful clusters of rock crystals or amethyst at the centre.

It was a little unfair of me to leave just the above without explaining it so I was impressed you asked for a simplified explanation. It meant you were really trying to understand. Here is an explanation in other words...

A concentric, banded, fibrous - is about the fine layers you see in this magnified part of your class photo. Fine layer after fine layer had built built up making bands in the sample.

This photo was supplied by Mrs. Yollis and class.

This photo was supplied by Mrs. Yollis and class.

formed by precipitation from watery solutions in rounded cavities in lava rocks (geodes) -

Water can absorb many types of minerals, some slowly and some quickly. When the water evaporates, the minerals can be left behind. In some examples, crystals can grow. Here's something you can try. Take salt and dissolve it in warm water or take some sea water, the saltier the better. Put the water in a flat, clear dish (glass is better so you can see under the result) and leave it in a sunny, warm place. Don't move or stir it as this can effect the results.

Over time, the water will evaporate and you will see salt crystals forming. Once the water has all evaporated, you can examine the crystals. Use a magnifying glass to see the finer crystals. Crystals are fascinating. If you see a larger crystal, you might see it has a certain number of sides. How many can you see?

Crystals are growing rocks. We don't consider them alive but they do grow as long as the "watery solution" is still able to provide raw materials. Here are some crystal photos I have taken to show you.

Quartz crystal

You can see quartz crystal has six sides.

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

Schools and students have permission to use this graphic for non-commercial, educational purposes.

Schools and students have permission to use this graphic for non-commercial, educational purposes.

Citrine Quartz Crystal

The different colours in quartz can depend on other minerals dissolved in the watery solutions.

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

Smoky Quartz

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

Amethyst (quartz) Crystals

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

Blue Calcite crystal

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

Sulphur (Sulfur) Crystals

This sulphur sample has been inside a sealed container for over 30 years. With permission, it was collected from a fumerole (where gases and steam escape from volcanic areas) in New Zealand. Sulphur (and salt) crystals break down in water so they would have become powdery instead of shiny if not in an airtight container.

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

Iron Pyrite (fool's gold) crystal

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Keira's Rock - How did it get there?

Rocks can sometimes be found a distance from where they formed. They can be moved by erosion (the wearing away of rocks by wind and water) or perhaps even movement in the Earth. Let's look at some samples you might recognise...

Gold can often be found associated with quartz rock but is much rarer. Most quartz won't have any gold. Just like other minerals, small amounts of gold can be in water and other fluids (it doesn't really dissolve but can be present in very small amounts). As water evaporates, gold can be left behind in cracks in rocks. If enough gold is carried in enough time, it can build up in amount. The sample of quartz below is from a mine in Hill End, N.S.W.. This is mined gold in quartz.

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

If the gold bearing quartz is exposed to wind and rain, larger pieces of gold can be eroded out. This is how we can find gold nuggets in streams and rivers. The below sample is only 0.127oz or about 1/8oz (3.6g). It is only about 1.4cm across. You might even be able to see a tiny quartz crystal in it. This small nugget came from New Zealand.

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

Finer pieces of gold can be eroded off larger pieces or out of quartz. To retrieve this gold, panning is often used. I panned some of this in Australia and New Zealand and bought some. The amount is 0.264oz or about 1/4 oz. (7.5g)

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

Gold starts it's journey as precipitated (left behind when water dries) gold in rock. It can be mined or found in nuggets and flakes if eroded. Gold, as you know, is used in jewellery and is also import in electronics but my favourite use is to make gold coins. The photo below shows a 0.1oz Australian Gold Nugget coin. It has a diameter of about 1.5cm and its value for the gold content today is about $135 U.S..

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

 

I found one reference to a Californian beach where agates can be found at low tide. The San Francisco Gem & Mineral Society blog post tells us Pescadero Beach about 40 miles (64km) south of San Francisco. If you look at the photos they share, you will see the agates have been rounded by wave action on the rocks and sand.

Where Can Azurite be found in Australia?

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Azurite is really a bluish coloured form of copper. The other colours are impurities of other material. There are a number of places it can be found in Australia including, in N.S.W. (Girilambone and possibly to Nymagee), Northern Territory (Areonga), Queensland (Chillagoe) and South Australia (Burra Burra). I think it can be found in the U.S. in Morenci, Arizona.

 I have a crystal that looks almost like the purple crystal that was cut in half. My crystal is blue. What kind of crystal is the purple one?

I think the purple crystal you mean is amethyst, a quartz type, shown also above.

There are many crystals and minerals that can be blue, purple, green, red or other colours so it would be hard to say without looking at the stone. Here are some blue, purple, green samples from my collection. They are only small samples and some have been cut and polished.

Amazonite (cut and polished)

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Apatite

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Dumortierite

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Howlite

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imitation (fake) green beryl (cut and polished)

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Lapis Lazuli (cut and polished)

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Lepidolite

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Sodalite

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Zooisite

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How Do I Know So Much About Minerals?

I don't think I do know a lot about minerals but I am interested in them and over the years have collected some. I know enough to get some ideas but my secret is knowing how to find answers when I need them. It could come from one of my geology books or online.

If you were to talk to someone just starting school, they would probably wonder how you knew so much but that's what learning is about. If you keep your mind and senses (sight, sound, touch, smell and taste) open to new things, learning seems to come in to try and fill the space. I'm still learning new things so it seems an open mind is pretty hard to fill. Your questions helped me learn a little more about my collection.

Be a lifelong learner. There's so many interesting things to discover.

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I received a question via Twitter...

Do you know what kind of stone this is ?

There was the below photo attached to the tweet...

This photo was supplied by Mrs. Yollis and class.

This photo was supplied by Mrs. Yollis and class.

I like a challenge and, although not always successful, finding an answer. I have an interest in geology but l find I know a little about many things but not a lot about anything. Without being able to hold the rock and look more closely, and without expertise, my first stop was to look more closely at the photo. Here's what I noticed...

The stone was white to bluish-grey.

Breaks around the edges looked a little like they might break off in flattened, sharp edged pieces.

There appears to be an inner border (lining) on the stone.

I wanted to see the border closer so I enlarged a section of the photo (below). I also enhanced contrast and colour a little.

This photo was supplied by Mrs. Yollis and class.

This photo was supplied by Mrs. Yollis and class.

 I now noticed there seems to have been some fine layering around the edge of the stone up to the border. Layering can mean sedimentary rock but, it can also be a sign of a space in rock filling with crystals. I had seen something like this before. I probably have a few hundred small mineral samples in my collection so I started to search. Firstly, a display of stones I had used with classes over the years...

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

A few of these showed some of the features I was looking for, especially calcite, agate and quartz.

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This reminded me of larger samples I had in my minerals database, I found items 41 and 46. They are listed as "Quartz - Chalcedony - Agate". They are examples of silicon oxide (SiO2).

The first sample has been cut and polished. The layering towards the outer edge is easy to see. There are small quartz crystals in the centre of the sample. I have seen this in other of my samples where inner spaces aren't completely filled. See geodes and the additional photos at the end of this post.

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The second sample was a piece broken off a larger sample and only had a low sheen.

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Without being able to hold and examine the sample in Mrs. Yollis's class, I suspect they have a sample of agate or chalcedony. Remember, I am only interested in geology and not an expert so I'm really only guessing.

How is it formed? My database explains it this way...

A concentric, banded, fibrous variety formed by precipitation from watery solutions in rounded cavities in lava rocks (geodes), sometimes with beautiful clusters of rock crystals or amethyst at the centre.

From my collection, below are photos of geodes. Most have been cut and one polished to show the interior.

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

The last photo shows one cut sample and an uncut geode beside it. What's inside the uncut geode? I can tell you it is about the same size as the cut geode if it was whole. This means the uncut geode should be about twice the weight of the half but it is around three times the weight of the half. It may be solid or have a small central cavity. It could be very beautiful or possibly plain inside. We'll never know because I won't have it cut. I like a little mystery in the world. 🙂

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In the comments of their poster entitled "Welcome to Grade THREE!", the Battalion Bloggers asked some questions. For their original post...

Welcome to Grade THREE!

Monitor Lizards

Perentie Lizards

This graphic has been sourced through Wikimedia Commons and is listed as in the public domain.

This graphic has been sourced through Wikimedia Commons and is listed as in the public domain.

The Perentie tend to live in central Australia across to Western Australia but are not native to my area. Their patterning is very attractive but I have only seen them in zoos and not in the wild. They are one of the monitor lizards.

 Lace Monitors

 The photo below shows a local lace monitor (goanna) I photographed while hiking. It was about 1.5m long and was seen eating an animal killed on the road. I have seen them a number of times.

Lace monitors are our second largest monitor lizards after the perentie. The perentie and lace monitor are thought to be slightly venomous but they are generally shy and run away if surprised. I have read fossils have been found in Australia showing komodo dragons, the largest of the monitors once also roamed Australia but are now only found in Indonesia.

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Kangaroo, Koalas and Echidnas

I have seen kangaroos (and wallabies), koalas and echidnas in zoos and in the wild a number of times. There has been an echidna in my garden and kangaroos on the sports oval across the road. While wild koalas aren't common in my area, my local animal sanctuary has had them. Potoroo Palace has a female named Sapphire who was born in their sanctuary. I have known her since birth.

All of the video clips shown below were filmed by me at Potoroo Palace.

Kangaroo

The most common kangaroo in my area is the eastern grey kangaroo. The males can be up to around 2m tall and are common in my area. The pictured male was as tall as me. He watched me as I took his photo them he hopped away. They are only dangerous if they feel trapped.

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Here is one of my short video clips showing eastern grey kangaroos.

Koala

The photo shows Sapphire when she was younger but had left her mother's pouch.

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The first of my video clips shows one of the first times Sapphire looked out from her mother's pouch after about 26 weeks inside the pouch.

The second clip shows Sapphire with her mother, Suzie. Too big, Sapphire stayed out of the pouch but with her mother.

With the loss of Blinky (father) and Suzie (mother), Sapphire is now the only koala at Potoroo Palace. I am certain the staff will be hoping for a suitable mate for her to continue their koala breeding.

Echidna

 I have seen echidna when hiking, in a park in my town and even in my own backyard. Their eyesight isn't good and they can't bite. If threatened, they dig their strong claws into the ground, hold on, and show only their spines.

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This is what they look like when they dig in.

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 Below is a video clip of Potoroo Palace's Spike.

The Outback.

There was an old saying, "Out back of Bourke". Others have talked about the outback starting at the dingo fence or  beyond the  "black stump", or a number of other areas but, mostly, outback refers to isolated inland areas of Australia. Unlike Canada, much of Australia is arid or semi-arid (deserts or near deserts) where rainfall is low and the soil is often reddish from iron oxides (rust). I'll share some photos, a number just scanned into the computer from old 35mm film slides, so you'll be the first to see them since many were taken back in 1985.

In 1981 and 1982 I was the Teacher in Charge of a one teacher school. It was very isolated and ranked number 6 in our state. Town was 100km away. The school was there for children from sheep and cattle stations. I lived 20km distant in a shearer's quarters on a 100,000 acre sheep station. We did have a computer on loan for about six weeks each year but the internet was still many years away for schools.

Below is a picture from 1982. Does it look isolated?

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1985 - A Trip to Uluru (Ayers Rock)

By 1985, I was a teacher in an 850 student school in western Sydney. In 1983, I had organised a trip for some families to New Zealand but, for 1985, organised a trip through the centre of Australia. I was the 20 seater bus driver for most of the trip of over 7000km. Our first night was spent in the schoolroom of my old school pictured above. From there, we took dirt roads and a main highway until we reached Bourke. From there, we could have said we were in the outback.

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Here are some photos from back then...

This is the Darling River in the town of Bourke. The Darling River is part of an inland water system stretching from Queensland through New South Wales (N.S.W.), Victoria and out to sea in South Australia(S.A.). In times of severe drought it can run dry or overflow in flood during big rain.

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Heading north from Bourke along the Mitchell Highway, we stopped at the state border between N.S.W. and Queensland. The countryside was very flat but green as we had some rain the week before our trip.

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 We came to the mining town of Mt. Isa in Queensland. Mt. Isa is in the tropical but dry north of Australia. The red colouring of the soil is caused by iron oxide (rust) in the soil. Lead, silver, copper and zinc is mined there.

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From Mt. Isa, we headed west and crossed into the Northern Territory, heading about half way across N.T.. before heading south to the Red Centre (the middle of Australia). One of our stops was at Karlu Karlu (Devil's Marbles) where there are many large rocks seemingly balanced on their ends. They are important in traditional Aboriginal beliefs.

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Along the way, we crossed from the tropics back into the sub-tropics. A sign marked the line of the Tropic of Capricorn but I liked what someone had painted on the road. (The man in the photo was one of the dads and you can see we had some rain.)

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Finally, we arrived in Alice Springs, the town close to the middle of Australia if not really then in our minds. Again, as you can see in the photo, we were travelling in a wet period. The Todd River passes through Alice Springs but flowing water is rarely seen so, when they hold the Henley-on-Todd Regatta, it's more a running race holding something looking like a sailing boat. If the river is flowing with water, they have to cancel their boat races. 🙂

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The MacDonnell Ranges are the mountains around Alice Springs. There are many gorges and beautiful rock formations to visit. Below is a photo of Standley Chasm. The people in the photo will give you an idea of the size of the chasm.

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Schools and students have permission to use this graphic for non-commercial, educational purposes.

Heading south out of Alice Springs, we stopped at the Henbury Meteorite Craters. The twelve craters were formed when a meteorite broke into pieces before hitting the ground it's estimated about 4,700 years back.

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Finally, we came to our main aim for our tour, Uluru (Ayers Rock) and Kata Tjuta (The Olgas). Like Karlu Karlu, the sites have special significance to the local Aboriginal people who are the caretakers of the land. The first photo shows Uluru at sunset. It is the visible part of a huge monolith (single stone). The second photo shows the position where it's possible for visitors to climb the rock. The Aboriginal people wouldn't climb to the top of Uluru because of its cultural importance but they allow visitors if they choose to do so.

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As you walk or drive around the base of Uluru, there are many places with simple barriers and signs asking people to respect special places for Aboriginal people. There are sacred places for Aborginal men and women they ask visitors not to enter. The photo below shows some Aboriginal artwork on Uluru in a place where visitors can visit.

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Approximately west of Uluru is Kata Tjuta (The Olgas). You can see them in the distance in the first photo taken from Uluru and part of them up close in the second and third.

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Heading south from Uluru, we crossed into South Australia (S.A.).

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...and eventually reached the opal mining town of Coober Pedy where many people have built their homes underground to protect them from summer heat. The area is dotted with opal mines.

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We started to see salt lakes. Water flowing all the way from Queensland during high rainfall, has nowhere to go when reaching the lakes. As the water evaporates, salt is left behind. The next photo, taken from our bus, shows a salt lake in the distance.

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Upon reaching the town of Port Augusta, we headed north-east through the Flinders Ranges.

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We crossed the border into N.S.W. and travelled 1200km to reach home.

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Here is a link to Mrs. Watson and class's brilliant soil study post...

Soil Investigations

Dear Mrs. Watson and class,

Your soil investigation techniques are wonderful and I see you have discovered soil isn't as simple as it might seem. The soil around my house is mainly a clay/sand mix but we have improved the soil in our garden by adding to our natural soil. We help build the humus layer.

Let's have a quick look at the story of soils...

 Rocks

Formed from lava flows.

This photo is from my collection of photos but was unmarked and so I am not certain of its source.

Location: Kilaeua, Hawaii, U.S.A.

Blown out by volcanic eruptions.

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Location: Mount Tarawera, New Zealand

Can build up in layers.

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Location: Rock cutting, Yellowpinch, Australia

Eroded by wind and rain to form sands.

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Location: Bournda National Park, N.S.W., Australia

Shells can add to the mix.

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Location: Bournda National Park, N.S.W., Australia

In time some hardy plants can grow.

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Location: Bournda National Park, N.S.W., Australia

Other plants take hold as the soil builds up. Dying plants build the humus layer.

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Location: Bournda National Park, N.S.W., Australia

Fires can add ash to the mix making soils richer and help plants grow

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Location: Royal National Park, N.S.W., Australia

Sometimes drought can take away the plants...

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Location: Bournda National Park, N.S.W., Australia

...but water can make the plants burst into life again.

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Location: Bournda National Park, N.S.W., Australia

 

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Location: Bournda National Park, N.S.W., Australia

 

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Location: Bournda National Park, N.S.W., Australia

 The process goes on as layers form and erode away, sometimes sharing beautiful colouring with us as they do...

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Location: North Tura Beach, Bournda National Park, N.S.W., Australia

and looking more like the work of an artist's brush.

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Location: North Tura Beach, Bournda National Park, N.S.W., Australia

Did you know colour can sometimes give you clues to soils?  When I lived in western New South Wales the soil looked reddish in colour. It was coloured by  iron content in the soil. The soil was rusty.

In the above photos I recently took, you can see many colours. Being a national park, I couldn't take samples to check what the different colours were but I could take photos. I was left with questions...

How many colours can you see?

Are the red areas high in iron?

Are the yellows coloured by sulphur?

Could the white be layers formed from shells?

Could the pink be a mixture of the others?

Soils and how they are made can be a very interesting subject and, as you have found, are not just dirt.

Danny from Techie Kids asked about my state of New South Wales...

Hi, Danny.

So I could share some photos with you, I thought it better to answer with an extended comment.

While New South Wales isn't Australia's largest state, it is the state with the highest population. New South Wales has an area of 809,444 sq km (312,528 sq mi). This makes it larger than Texas but only half the size of Alaska. Western Australia is our largest state and is about 50% larger than Alaska.

Emblems of New South Wales.

Floral Emblem

The Waratah (Telopea speciosissima)

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Location: Merimbula, Australia

Bird Emblem

Kookaburra (Dacelo gigas)

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Location: Merimbula, Australia

Animal (Mammal) Emblem

Platypus (Ornithorhynchus anatinus)

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Fish Emblem

Blue Groper (Achoerodus viridis)

Copyright (c) 2004 Richard Ling (richard@research.canon.com.au). Licensed under GFDL and CC-by-sa-2.5. All other rights reserved.

This graphic was sourced through Wikimedia Commons.

Gemstone Emblem

Black Opal

This is a public domain graphic sourced through Wikimedia Commons.

For a class looking at Rocks and Minerals...

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Below are links to "Rocks and Minerals posts I have made over the last year.

In 2012, I sent some rock samples to a class in England. I followed up with a series of posts examining what was sent...

This is the first of some posts I will make on my experiences with volcanoes. Looks at the samples sent.

Samples – Scree & Obsidian samples

Samples – ‘A’a and Pahoehoe

Iron Sands (NZ) and Pumice Stone

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Location: Mt. Tarawera, New Zealand

Looking at Volcanoes - Some links to post

Hotspots (Geological not internet)

New Zealand

A final volcano post of You Tube links

More on Volcanoes for Global Grade 3

New Zealand’s Beautiful landmarks – for B4 and Bradley

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The Earth

How did the Earth begin? – A challenge from Heather and Keira

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Examining Some Rock Samples from Canada - Are they fossil rocks or volcanic?

Something Special from Canada

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For the students who sent me a kind gift. Here is a link to their blog...

Battalion Hawk Bloggers

Hello Battalion Hawk Bloggers,

Well, it did take some time for the parcel to arrive but, as you already know, it finally appeared. Here is what I found inside...

A clapper board to help me align video clips.

A packet of chalk so I can write on the board.

Three rock samples bearing fossils.

Just by chance, later the same day your parcel arrived I had a phone call. I was asked if I was willing to video the opening performance of the Candelo Village Festival. I agreed and realised I had the chance to use the clapper board very soon after receiving it.

This also presented me with another idea, I had a blog where little had been posted as I didn't have a strong use for it. I cleared away some old posts, some of which ended up on this blog because they were my earliest extended comments. After reorganising the layout and content,  I renamed it...

Exploring Ideas: How to and why… A look at blogging, graphics and activities

The idea is to use this blog when I explain how or why I do things the way I do. I left two posts from March, 2012 because they looked at how to write a googol (special number where 1 is followed by 100 zeroes) and how I approach writing a story, particularly long ones.

Your gift gave me an idea for the first post made especially for the blog. It tells how I used the clapper board. I have included a video clip I made for you showing me use the clapper board to mark the film position. I also included 15 seconds of a performance so you can hear a little of my experience on the evening of Friday (April 12).

The people have been deliberately blurred for privacy reasons. You will not have heard the song before as the music festival opening included original works by local composer/musicians. Here is the link to the first real "How to and Why" post...

Aligning Video Clips

Now, let's look at the rocks you sent. There were the three stones and something sounding fossil-like. I'll explain shortly...

 Crinoid or Corallite Fossils?

 

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Both suggestions people made through Twitter seem reasonable and both types of creatures still exit in our oceans today. Of the two choices, I would favour crinoid-like fossils but, remember, I am not an expert so this is only my opinion. There is a third option I might add soon. Let's look at the two choices...

Corallite

(Wikipedia reference: Scleractinia )

This is a Wikimedia Commons image of one type of hard coral taken by Nhobgood

Corallite, if I have my information correct, is the fossilised remains of stony corals. When you look at photos, you can see they are well formed, rock-like structures so I would expect fossils of them to include a more regular pattern than in the samples you sent (see the photo below). Of course, it is also possible what you see in the rocks are broken bits of coral cemented together in the way sedimentary rocks can form.

 

Below is a photo of a piece of coral I found washed up on the shore in Queensland. It came from the Great Barrier Reef. Can you see the pattern of openings where coral polyps once lived?

 

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Crinoid

(Wikipedia reference: Crinoid )

This is a Wikimedia Commons image of one type of crinoid taken by Alexander Vesanin

Crinoids tend to have small tube-like structures that could be what we see in the stones. There have been some beautiful, almost complete crinoid fossils found. What you see could also be the remains of small shellfish, i.e. their shells (see the photo below). I don't know what rocks are native to your area but, whatever, the stones you sent will now take their place in my rocks and minerals collection. They are my first from Canada. 🙂

Below is a rock I picked up on a beach. You can see, like the samples you sent, it has been rounded by water action. Can you see the shell fossils embedded in it? In these cases, you can see the shell was from spiral shell type similar to ones I sometimes find washed up on our beaches.

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Did I say "something sounding fossil-like" back there? I'll explain.

You know my mind tends to wander in many directions and this is what happened when I saw the packet of chalk. The question came to mind, "What is chalk?" I thought I would share my answer with you.

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Location: Dover, England

I took the above photo when I was in Dover in England. It shows the famous White Cliffs of Dover. The cliffs are chalk but what exactly is chalk?

 

Here is a quote from Wikipedia...

"Chalk is a soft, white, porous sedimentary rock, a form of limestone composed of the mineral calcite. Calcite is calcium carbonate or CaCO3. It forms under reasonably deep marine conditions from the gradual accumulation of minute calcite plates (coccoliths) shed from micro-organisms called coccolithophores."

(Wikipedia Reference: Chalk )

What this means is chalk has formed under the ocean from the remains of algae so tiny you would need a microscope to examine them properly. Can you imagine the cliffs of chalk in the above photo would have involved many billions of these tiny organisms over a very long time?

Is this the same chalk you sent? While it could be, much of the blackboard chalk manufactured today is made from a stone called gypsum. Below is a photo of gypsum from my collection. This particular piece is known as rose gypsum because of its appearance. (It is shown glued onto a shell for display.)

 

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What was the third option for the stones you sent?

I can be a very curious person when seeing something interesting. This is what happened when I was looking at the rocks.

I suspected I might not be looking at fossils in rock at all so I broke open the smallest piece of stone so I could examine its centre. I found the stone was made of small crystals. Below is a graphic showing four photos I took of one of the pieces of the small stone. Can you see the shine of the small crystals?

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Now I was really curious because I suspected the stone wasn't fossil bearing sedimentary rock. I thought it might actually be igneous rock, i.e. volcanic rock. I spent more time searching my rocks and minerals books and the internet. I think I might have found what the stones could be. I think they might be diabase (aka dolerite).

Below is a reference for diabase. Visit the site and look at their photo of diabase. Tell me what you think.

Diabase

Of course, I could be completely wrong but it is fun to try to find answers even if they're sometimes wrong. We can learn from both right and wrong answers if we keep our minds open.

* * * * * * * * * *

I just had an afterthought on rereading this post and thought I'd share. When I broke open the small rock and looked inside, I realised I was the first person to have ever seen what's inside that particular stone and now I'm able to share what I found. In your lives, you will have many first person experiences. Will you recognise them when you do? I wonder if that makes us all curiosity explorers a little like early explorers seeing somewhere for the first time?

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Dear Heather and Keira,

I never know when a post or comment from a student or class might prompt an extended comment. Something written makes me recall some information I have read or seen over the years and before long I find a comment growing longer or I want to include photos, videos, audio or links.

In the "How did the Earth begin?", the challenge was one I thought I could meet. Being keen on science and many other things, I had been following theories on the origin of the Earth and the universe. Once I have an idea for a post, I research my facts to try to make certain my thoughts are on the right track then start writing the post. I knew "How did the Earth begin?" would be a longer post because there is much to consider.

Geocentric is a term used to describe the belief the Earth is the centre of the universe and all planets, stars including our sun, and the moon orbit us. From research, I have found many people still believe in geocentrism today. For some, it may be a religious decision, others a firm belief they believe science can support, and for others it's more a matter of not knowing any other way.

We do live on the crust of the Earth. It's the solid part that is our land and the bottom of oceans and seas. Compared to the rest of our planet, it is very thin but I wouldn't have it any other way. If you cut an apple in half, you can see the thin skin (like the Earth's crust) covering the rest of the apple down to its core.

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The inner core is thought to be very hot but solid iron hotter than the surface of the sun. It's pressure keeping it solid. The outer core is still mostly iron but it is liquid and flows around the inner core. Remember, the Earth turns on its axis and this causes the spin and also gives us night and day. Think of stirring a drink. You can see the liquid moving around as you stir.

It's this movement of the outer core that gives our planet a magnetic field and protects us from much of the sun's dangerous radiation. Mars doesn't have this activity so has a weak field. Even if there was air to breath on Mars, we would probably still need special clothing to protect us.

The mantle is semi-liquid and is basically moving hot rock (magma).

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The mantle movement is known as convection. We can see this effect in boiling water. Below is a video clip I prepared for you. To see the movement of the water, some rice grains were dropped into the water. You can see them move to the side being heated, rise with the heated water then sink back down as the water cools a little. The same thing happens in the mantle. The hot rock (magma) sinks down as it cools a little, is heated near the outer core and rises again. There are many of these convection currents in the mantle not just one big one.

Schools and students have permission to use this video clip for non-commercial, educational purposes.

Sometimes this movement of the magma brings magma to the surface and it flows out as lava. I was on Hawaii (The Big Island) a number of years ago and took a helicopter ride over the Kilaeua and along the coast. Look in the photo below and you see see the lava pouring out into the sea. Kilaeua has had a very active period.

The photo is a scan of an old 35mm slide so the quality isn't the best.

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Location: Kilaeua, Hawaii, U.S.A.

Curiosity is a great gift. It's something still driving me to explore new ideas and things. I can see you both have curiosity. I wonder what great discoveries and learning is ahead for you? 🙂

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I had written a post on plate tectonics and continental drift for Mrs. Yollis and her class. Two students, Heather and Keira, challenged me to explain how the Earth began. This post is an attempt to provide an explanation according to my understanding of the science. To see the comment and challenge, click the link and scroll down to the comments.

Plate tectonics and our dynamic continents

How Did the Earth Begin?

Dear Heather and Keira,

There are so many stories of how the Earth began if we look though the amazing cultures in our world. It would be remiss of me not to mention one or two. Because of my home and yours, I have chosen stories from the native people of Australia and North America.

The Aboriginal People of Australia

Many people think there was one Aboriginal (native Australian) culture and one language but, before the coming of European colonists, there were many, many of those cultures now lost. One of the best sites I have seen comes from the Yolngu people of Ramingining in the northern part of Central Arnhem Land in Australia's Northern Territory.

For one of their creation stories, click the link Twelve Canoes and wait for the site to load. The picture below will appear. Once loaded, click on the picture indicated by the arrow to see a creation story.

This graphic should not be copied.

I think you will find many interesting things on this site as well as one of their creation stories.

Native American People

I found the following You Tube clip telling the story of creation of the Earth through the traditional beliefs of three Native American tribes, the Iroquois, Seminole and Cherokee.

This embedded You Tube clip is not my video.

Let's now start looking at what science is finding...

Let's start with some word learning. You have had many ideas in your life but have you ever heard someone say they have a theory? Many people confuse "idea" and "theory".

A scientist has an idea after looking at the information available through study or research and proposes an explanation for what has occurred. Other scientists look at the conclusions and test the idea against other data or new information. This may lead others to agree with the idea. With other scientists agreeing and available evidence supporting, the idea becomes a theory. Science is a path to discovery. We learn more and more about how things work.

Did you know up until a few hundred years back people thought the Earth was the centre of the universe and all of the stars, planets and our Sun orbited around us? This idea is called Geocentric.

A Geocentric View of the Universe

This drawing is based on a map by Bartolomeu Velho (1568)

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A second geocentric model has Earth at the centre of the universe. The other planets orbit the sun and the sun and all the planets orbit the Earth.

It wasn't until about the 1500s more and more evidence was being gathered to show Earth isn't at the centre of the universe. It is a planet orbiting our Sun and now we know our Solar System is towards the outer edge of a double spiral galaxy we call, The Milky Way. We also know our galaxy is one of very many, probably billions, in our universe. We know this because of what scientists have been able to observe and because of the theories arising.

Watch the below video to see an explanation of what is thought to have happened to form our planet and others in our Solar System. Remember, you can click on the small box symbol on the bottom right of the video to watch full screen.

 Now let's look at the information in the video

* About 9 billion (9,000,000,000) years after the universe was born a massive start went Supernova - A supernova is an explosion of a star. It might have been caused by the collapse of the massive star's core. Radiation, energy and stellar dust explodes out from the collapsed star. Back in 1987, we were able to look into the sky and see a supernova astronomers named SN 1987A. Where once nothing could be seen, a star bright enough to be seen without a telescope had appeared. It is said to be 167,885 light years distance. This means the light took 167,885 years to reach us. The supernova happened a very long time ago.

* Gravity began its work on regions of the massive dust "cloud" sent out. The "cloud" particles started to gather. Pressure and heat increased. Our Sun was being formed.

* The temperature increased to about 10 million (10,000,000) C or about 18,000,032 F. About 4.5 billion (4,500,000,000) years ago our sun lit up.

* The Sun used much of the "cloud" leaving only 0.1%. Look at this picture. Imagine the cloud was made up of 1000 students in a school. 999 of them would go to make up the Sun. Just one of them would be left to make all of the planets and asteroids in the Solar System. The little guy in red looks a little lonely. 🙂

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* The left over material was caught in the pool of the Sun's spinning motion. The left over material was spinning (orbiting) around the sun. The spin and gravity of the sun was drawing the material into rings (like Saturn's gravity has drawn material into rings around it). The way the material was orbiting the sun stopped it from being pulled into the Sun. I know this can be hard to understand so look at the next graphic I have prepared.

Imagine you are the Sun. You have a long, strong elastic attached to a tennis ball and you are spinning it around your head.

The ball is orbiting you. The elastic is your gravity trying to pull the tennis ball to you. The tennis ball is one of the planets. If the movement of the ball slows, the elastic draws it closer. If the ball moves faster, the elastic stretches further. Yes, in case you wonder, if the tennis ball was instead a basketball, the amount of stretch would be bigger.

Jupiter is said to be 317 more massive than the Earth. Imagine trying to spin 317 tennis balls on the end of the elastic. You wouldn't need to spin the balls as fast to keep the elastic as stretched as one tennis ball. Our Earth takes one year to orbit the Sun (that's what a year is, the time it takes our Earth to go once around the Sun). Jupiter takes about 12 years. If you could spin the tennis balls fast enough, the elastic would break and "Jupiter" would sail off into space.

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* The debris in the rings around our sun started to collide and come together to form larger masses. Their journey to becoming planets had started.

Have you heard of the asteroid belt between Mars and Jupiter? This ring of debris wasn't able to form a planet because it was being pulled from two sides, the Sun and Jupiter, the largest of our system's planets. Our ring was able to produce a planet which is fortunate for us or I wouldn't be writing this.

* From 4.8 to 3.5 billion years ago (4,500,000,000 to 3,500,000,000 years ago), the Earth was being bombarded from space. Combined with this bombardment, radioactive elements and pressure, Earth became a molten furnace. Heavier minerals like iron and nickel sank into the core and lighter minerals rose to the surface.

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You have probably seen how certain things float while others sink. If you drop stones or pieces of metal into a container of water, they sink to the bottom because they are heavier. Put in olive oil and it will float to the top.

* Around this time a large object about the size of Mars collided with our early Earth. Part of the collided matter broke off to eventually become our moon. The Moon at first was much closer to our planet.

Remember the elastic experiment? Earth's "elastic" isn't quite strong enough so it is gradually "stretching" but the Moon isn't expected to break away, just reach a distance where there is a balance but this is billions of years into the future so we needn't worry.

* Because of all of the heat and volcanic activity throwing out gases, Earth's atmosphere was mostly nitrogen, water vapour and carbon dioxide. We couldn't have survived the heat let alone the poisonous atmosphere.

* As the bombardment of debris from the creation of the Solar System reduced, Earth's surface started to cool. Water vapour cooled and the first ancient ocean formed. The cooling crust of the Earth formed the first land, Pangaea. Remember the layers of the Earth?


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In the  final video clip at the end f this post you will hear it said, if the Earth were a basketball, the crust would be thinner than a piece of paper on its surface yet that's where we live.

* The Earth had an atmosphere and water, conditions needed for the first life but that is another story.

Are there any other systems with planets or are our Solar System planets the only ones? Is there life on other planets in our universe?

I have a favourite quote from a man called, Carl Sagan. He was an astronomer, astrophysicist, cosmologist and author. He wrote a novel named "Contact". The quote comes from his book...

"The universe is a pretty big place. If it's just us, seems like an awful waste of space."

Many people had suspected other stars would have planets but it wasn't until 1988 the first planet outside our Solar System was found. Before this we simply didn't have the technology to do this. Now the possibility of around 2400 planets outside our Solar System are being investigated. It would seem planet formation as is said to have happened with our system is much more common that we had thought. You know I like numbers so look at this...

 

If there were only 1 billion galaxies in our universe each with 1 billion star, then there would be...

1,000,000,000,000,000,000 stars

(one quintillion stars)

Just say of these only 0.1% (like the amount of material left when our sun formed) had planets, then there would be...

1,000,000,000,000,000 stars with planets out there.

That is one quadrillion stars with planets.

Now just say of these only 0.0001% of the planets had life (that is not 1 out of a 1,000. It is 1 out of a million), then there would be...

1,000,000,000 planets with life.

That is one billion planets with life.

But there are probably many more than a billion galaxies in our universe and I suspect life is much more common than the above but reaching planets outside our Solar System to find life doesn't seem likely because of the vast distances between the stars and far greater between galaxies.

As you know, NASA has the Curiosity rover on Mars. Latest news shows it has found rocks on Mars have some of the chemicals necessary for life - sulfur, nitrogen, hydrogen, oxygen, phosphorus and carbon. If we find evidence of life on Mars or that it once existed, we have proof we are not alone but don't expect Martian people. If life is found it will most likely only be something like bacteria.

Early Earth & Plate Tectonics

This one talks of the possibility of a number of land masses forming over time and gives them names. This is quite possible but I am happy enough with just Pangaea unless I find further evidence. The clip does show you how our Earth is protected from harmful radiation from our sun by it's magnetic field caused by our rotating liquid iron outer core. Mars's interior cooled a very long time ago. Solar radiation shed much of Mars's atmosphere but Earth has been protected. Our volcanoes, tectonic plates and earthquakes show us our world is still very active and I am thankful it is.

This embedded You Tube clip is not my video.

 New Video Clips to Watch

(added: March 24, 2013)

When checking through You Tube, I found this clip showing an animation of the Big Bang, and the beginning of our system, the Sun, Earth and Moon. This clip has nothing to read just images to watch as billions of years pass.

This embedded You Tube clip is not my video.

You know our Sun is much larger than the Earth. It's said it would take about a million Earths to make the size of the Sun but is our Sun a very big star? I found this video clip to show our Sun is so much smaller than the largest known star. This video clip shows just how tiny our Sun is compared to some other suns (stars).

This embedded You Tube clip is not my video.