My Green Iguana Baby Neo

Coming home with a baby iguana is usually an impulse buy. People see them in one setting or another and end up running out and getting one without realizing how much work they actually are. My husband and me don't want to make a mistake, read a little more and then decide if we are ready to be an iguana owner.

Choosing baby iguana is one of the most important decisions we make when getting our pet. We really need to be careful. Never blindly take one from a shop or private owner. We want to make sure that it is living in a clean environment (if the tank is dirty and the iguana is lying around in its own feces, it very well may be susceptible to very harmful bacteria). We also make sure the baby iguana we call it Neo skin is in healthy, that it is not skin and bones and the eyes are clear.

We have to create a natural habitat for this Neo. First things first though, we get a large tank, in the 50 gallon range. This is a good start, but eventually, we will remove the baby Neo to a dedicated room or very large cage when he get large.

At some time, no matter how well you have cared for your iguana, you will have to deal with the death of your pet. Over time, the bond between a pet and its owner makes for a very sorrowful and sad end to the time they've spent together. We lost our first iguana after several visits to the vet and regret was the hardest thing to deal with because I knew that if I had given him better care, he would still be here today. Dealing with the death of your iguana won't be easy, especially if you've spent day and times caring for it. Here are a few suggestions and some advice I'd like to give you to help you deal with the loss of your pet...


* First of all, don't blame yourself. Yes, it may very well be your fault that your iguana's life was cut short because of improper care (whether it was intentional or not), but blaming yourself will not make it any better. The best thing you can do instead of blaming yourself is to learn from your mistakes, and if you do choose to get another iguana, make up for it by providing better care for the next iguana (even if it's someone else's iguana).


* Even though you may want to rush out and replace your lost pet, it may be a bad idea to do so (till now we still missing Neo specially our daughter Farah, its hard for her to replace our lost pet). Take your time.
As strange as it may sound, you may want to sit back and remember your lost pet for a while, instead of replacing it. If you did lose your iguana due to improper care, it may also be a good idea to learn as much as you can about the proper care they need before you jump into another commitment of properly caring for another iguana. Even experienced iguana owners can learn more about proper care. Reading and learning more about good iguana husbandry may even take your mind off your sorrows as well. Chances are you will want to get another shortly after the death of your iguana. This is quite normal and I suggest you fight the urge and wait until you absolutely know the time is right to welcome another iguana into your life.


* Although it may sound like an inappropiate or "bad" idea, it can be a very beneficial thing to have a necropsy done on your iguana. A necropsy is an autopsy performed by a vet to determine the exact cause of death. Much can be learned by having a necropsy done and the facts you learn from it can help you improve the care you may give another iguana. You may discover that certain ways you cared for it, including diet and habitat requirements, could be improved on next time. Not only can a necropsy benefit you, but it may also benefit the overall care of iguanas everywhere. Your vet may learn a thing or two as well. Some vets who may not be true iguana experts will jump at the chance to perform a necropsy on an iguana, so they too will learn more about better iguana husbandry. Some vets may charge you for a necropsy, but most will perform one for free. Many people don't want their beloved pet "cut up" or "destroyed" with a necropsy, but if there is a chance that something can be learned to better the care of some iguana somewhere, please consider it before you give your pet a permanent resting spot.


* Another good idea to help you deal with the loss of your pet is to give your pet an appropriate burial with a memorial of some kind as well. Many people go as far as an all out memorial in a pet cemetery, but a nice resting spot in the back yard serves its purpose as well. There's nothing wrong with having an attractive constant reminder of a lost pet decorating your lawn for years to come. My iguana has a nice little iguana statue (that we have had a sweet memory as we had him) sitting on a pile of stones with vines growing throughout it. All of which sits under a nice shady tree our my back yard. As odd as it may sound, every time we cut the grass or do some yard work, We can't help but remember some experience or little thing about our Neo and the time we spent with him. As a matter of fact, our iguana was notoriously aggressive. We believe we may be allergic to the vines in his memorial, so even now that he's gone, he still manages to bite and scratch us. Things like this, even as bad as they may sound, can cheer you up when you least expect it.

most popular music

As humans we have a very special relationship with music. It seems to be able to connect to our soul, lift our mood, and give us pleasure and inspiration, yet the music that resonates with you is unlikely to have universal appeal. This is because the music we most appreciate is almost always what we were exposed to from our childhood to late adolescence. Thus the music that touches you deeply is unlikely to resonate with someone of another generation or culture.

For most of us music is an appetite and pleasure as deep as our hunger for food and money. It touches all stages of our life, and all areas of our brain. Our tastes in music are wired at about the same age we acquire mastery of language. Like language we absorb the music being played round us during our formative years.
As humans we have a very special relationship with music. It seems to be able to connect to our soul, lift our mood, and give us pleasure and inspiration, yet the music that resonates with you is unlikely to have universal appeal. This is because the music we most appreciate is almost always what we were exposed to from our childhood to late adolescence. Thus the music that touches you deeply is unlikely to resonate with someone of another generation or culture.

HRstrut - The Best Band You've Never Heard Of

Break your boredom with music that is derivatively fresh and original. It is appealing yet unlike anything you have ever heard. The band's name may not be familiar, yet they make music you will not want to forget.

HRstrut's website is:

http://www.hrstrut.com/

Try living No Impact for a week
The No Impact Experiment, brought to you by the No Impact Project, is a one-week carbon cleanse. It is a chance for you to see what a difference no-impact living can have on your quality of life. It’s not about giving up creature comforts but an opportunity for you to test whether the modern “conveniences” you take for granted are actually making you happier or just eating away at your time and money.


Earthquakes: Finding fault with nature
As Haiti recovers from a deadly earthquake and ongoing aftershocks, here's a look at why such tremors happen and where the next one might strike.

Within minutes of the earthquake in Haiti last week, shockwaves had twisted the landscape, crumbled buildings and wiped out entire neighborhoods. The already-poor Caribbean country was reduced to rubble, and people around the planet were given a tragic reminder: There's a world of danger lurking under our feet.

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Cruise ships dock at Haiti resort despite earthquake tragedy Earthquakes happen every day by the hundreds, most of them too weak or remote to affect many people. But all that seismic noise is helping hide the risk of catastrophic quakes, which have been periodically surprising us throughout human history. Rapid population growth along fault lines is now raising the stakes higher than ever — the Haitian capital of Port-au-Prince is just one of many big cities worldwide that's perched near a crack in the Earth's crust — and even people far from the active fault can be affected via tsunamis, as the 2004 Sumatran earthquake demonstrated.

Humans are unfortunately powerless to stop such disasters, and despite major breakthroughs in seismology during the past century, we still aren't even very good at predicting them. But while that may sound hopeless, there are nonetheless many pre-emptive steps we can take to at least prepare for major earthquakes before they strike. Below is a quick look at what we know about the planet's geologic outbursts, and what you can do to be ready for one.

Earthquake origins
Earth's crust is always shifting and swirling around, a slow-motion shuffle that's partly fueled by liquid magma under our flaky outer layer. The crust floats atop this magma, broken into several jagged discs, called "tectonic plates," that constantly push and pull each other around the globe. Friction at these discs' edges is what causes earthquakes.

Tectonic plates tug away from each other along a giant scar, called the global mid-ocean ridge, that zigzags Earth's surface like the seam on a baseball (see map below). Magma rises, cools and hardens here as two plates churn out in opposite directions, forming new crust that may become dry land after a few million years on the conveyer belt.


Meanwhile, as new crust is born in the ocean, older crust is being pushed underground where tectonic plates collide, a potentially violent process that creates mountains, volcanoes and earthquakes. Seismic tremors can be released by converging plates in a few different ways, depending how their rocky edges crash and interact. These are the three basic types of earthquake faults:


• Normal fault: Many earthquakes occur when two sections of terrain have slipped vertically past one another along an inclined crack. If the rock mass above this type of inclined fault slides down, it's known as a "normal fault" (see animation at right). This is caused by tension as the tectonic plate is stretched outward from the fault, and it results in an overall extension of the surrounding landscape.


• Reverse fault: Also called a "thrust fault," this type of opening occurs when the rock mass above an inclined fault is thrust upward from below, pushing it farther on top of the other block of land. Both normal and reverse faults exhibit what geologists call "dip-slip" movement, but unlike normal faults, reverse faults are caused by compression rather than tension, resulting in a compaction of the terrain.


• Strike-slip fault: When two sides of a vertical fault slide past each other horizontally, it's known as a "strike-slip fault." These earthquakes are caused by shearing forces, generated when the rough edges of bedrock scrape together, catch on a jagged edge and then snap back into place. California's San Andreas fault is a strike-slip system, as is the fault that caused the recent quake and aftershocks in Haiti.

Seismic waves
The rock walls along a fault spend most of their time locked together, apparently motionless, but they can quietly build up enormous pressure over hundreds or thousands of years, then suddenly slip and release it all at once. The force from an earthquake comes in two basic kinds of waves — body waves and surface waves — that arrive in a series of three increasingly destructive blasts.

Body waves, which pass through the interior of the Earth, are the first to hit. The fastest ones are known as primary waves, or P waves, and because they're dispersed so widely and push rock particles ahead of or behind them, they're usually the least damaging. P waves are immediately followed by secondary body waves, or S waves, which also pass through the entire planet but are slower and displace rock particles off to the sides, which makes them more destructive. To someone standing on the ground, both P and S waves feel like a sudden jolt.

After the body waves, there may be a brief lull before the quake's final, most violent tremors hit. Surface waves pass only through the crust's upper layer, flowing horizontally like ripples through water. Witnesses often describe the ground as "rolling" during earthquakes, and these slow, high-amplitude surface waves are typically the most destructive part of a quake. Their rapid back-and-forth shaking is what causes much of the structural damage to buildings and bridges. (Surface waves are further subdivided into Love waves and Rayleigh waves, the latter being the most dangerous.)

Earthquake damage
The dangers we face from earthquakes come almost entirely from the built infrastructure around us. Aside from falling trees and rocks, the collapse of homes, schools, stores and office buildings is the No. 1 cause of death during a typical earthquake. Roads and bridges can also crumble due to ground shaking and displacement, a problem that occurred throughout San Francisco during its 1989 quake. Seismic waves have been known to flip cars and derail trains, as well as crush vehicles under tunnels and bridges or send them careening out of control.

Floods are another potential byproduct of earthquakes, since tremors sometimes break dams or twist rivers, and fires may be ignited by snapped gas lines or toppled lanterns, candles and torches. During the notorious 1906 San Francisco earthquake, the resulting fires (pictured above) did more damage and took more lives than the earthquake itself.

Tremors also loosen soil and may cause landslides, a threat that's higher near mountains, during rainy seasons and where trees are scarce (such as in Haiti, where widespread deforestation has increased the landslide risk). Even without steep hills or rain, however, earthquakes can also temporarily turn soil into a quicksand-like substance by mixing it with the groundwater below. Known as "liquefaction," this process produces a soupy mud that sinks people and buildings into the ground until the water table resettles and the dirt solidifies again.

But perhaps the most devastating way earthquakes use water for evil is by creating tsunamis — giant waves that can tower more than 100 feet high and crash onto beaches thousands of miles from the quake itself. When land lurches along a fault on the ocean floor, it displaces huge amounts of water upward and outward, with nothing to stop it but the nearest shoreline. This happened in 2004 when a quake near Sumatra battered Southeast Asia with tsunamis (pictured above, in Thailand), and it has happened throughout history to almost every country that borders the Pacific Ocean.

Cities and fault lines
The Pacific Rim is infamous for earthquakes, dubbed the "Ring of Fire" for the seismic rumbling that frequents places such as Alaska, California, Hawaii, New Zealand, the Philippines, Indonesia and Japan. To the west, a pile-up of the Indian, Eurasian and Arabian plates creates another seismic hotspot, forging the Himalayan Mountains and spurring frequent earthquakes in Pakistan, Iran and southern Europe.

But while the Eastern Hemisphere may seem to suffer disproportionately, no place on Earth is truly safe from seismic waves. Disasters like the 2004 Sumatran tsunami, the 2005 Pakistan earthquake and the 2008 quake in Sichuan, China were so severe because they hit heavily populated areas, but San Francisco's long seismic history and recent events in Haiti illustrate similar risks in the West. (See the world map below for global quake hazards.) In fact, the two largest earthquakes in modern history occurred in the Americas: the magnitude-9.5 quake that hit Chile in 1960, and the magnitude-9.2 quake in Alaska's Prince William Sound four years later.



Earthquakes and volcanoes in the Americas tend to cling to the western coastline, but they can occur farther east, too. The Caribbean is one example, since it's home to several competing tectonic plates that make the region a seismic minefield. In addition to the recent magnitude-7.0 earthquake in Haiti and its ongoing aftershocks — one of which measured 6.1 on the Richter scale — smaller follow-ups were reported in northern Venezuela (magnitude 5.5), Guatemala (5.8) and the Cayman Islands (5.8). Geologists say the fault's pressure has now moved west, which means another major quake could be in store for western Haiti, southern Cuba or Jamaica.

In the United States, the land under several present-day cities has also suffered enormous tremors in the past that would likely obliterate their sprawling metro areas today. Among the most attention-worthy earthquake zones in the United States, scientists are especially focused on these five:

• San Andreas: California's iconic scar shifts along a series of strike-slip faults, caused by the Pacific plate grinding north against North America. It's considered a high-risk earthquake zone because several big cities are located nearby, putting millions of lives in danger whenever it ruptures. Previous quakes in 1906 and 1989 ravaged the San Francisco Bay Area, with the latter destroying most of the city by breaking water lines and starting fires. The San Andreas fault moves an average of 2 inches annually, meaning Los Angeles will be adjacent to San Francisco in about 15 million years.

• Pacific Northwest: North of San Andreas, a group of faults around Puget Sound make up one of the most dangerous earthquake hazards in North America. Known as the Cascadia subduction zone, this area releases a major "megathrust" earthquake about every 500 years. That last happened in 1700, when the Pacific Northwest was sparsely inhabited, but the Seattle and Vancouver metro areas have blossomed since then, making a repeat performance potentially catastrophic.

• Alaska: Seven of the 10 most powerful earthquakes that have ever occurred in the United States were in Alaska, including the massive Prince William Sound quake that rattled Anchorage in 1964. Alaska is the most seismically active U.S. state and one of the most dynamic hotspots on Earth, but its harsh climate has historically kept its human population — and therefore its earthquake death tolls — relatively low. Still, Anchorage is now much larger than in 1964, and cities from San Diego to Tokyo are always at risk from tsunamis spurred by Alaskan tremors.

• Hawaii: Not only is Hawaii seismically active itself, making the state susceptible to earthquakes and volcanic eruptions, but it often takes hits from far-away earthquakes, too. The magnitude-8.1 quake that shook far eastern Alaska in 1946, for example, sent a tsunami south to Hilo on the Big Island, where it killed 159 people and caused $26 million in property damage. Eighteen years later, another tsunami hit Hawaii following the Prince William Sound quake of '64.

• New Madrid: The Eastern United States' strongest known earthquake occurred about 200 years ago in the lower Mississippi River basin, wreaking havoc in Tennessee, Kentucky, Illinois, Missouri and Arkansas. It was actually a "swarm" of tremors, with residents of nearby New Madrid, Mo., suffering an estimated 200 "moderate to large" earthquakes during the winter of 1811-'12 — five of them above magnitude 8. Homes were flattened, a new lake was formed and the Mississippi River briefly flowed backward from sudden ground displacement. Only one death is linked to the quakes since the area was still so sparsely populated at the time, but if the New Madrid fault were to experience a similar event today, metro areas such as St. Louis (pictured above) and Memphis, Tenn., could be devastated.

[RELATED: Which U.S. volcanoes are likely to erupt next?]

Earthquake safety
Since buildings cause some of the worst problems during earthquakes, they're a reasonable place to look first for solutions. Seismic-savvy construction has come a long way in the last century, pioneered in quake-prone places like Japan and California to let structures go with the flow instead of standing rigidly still. By including more flexible joints and more room for sway, engineers can make buildings that let an earthquake's energy pass through them, doing much less damage than if its full force was felt.

In poor countries like Haiti, however, such quake-proof structures are rarely feasible projects, and many buildings in Port-au-Prince were already structurally unsound before the Jan. 12 earthquake. Even in wealthy nations, few homes, stores or offices are designed to withstand a major earthquake — leaving knowledge, preparation and quick thinking as most people's best hopes for surviving one.

The ideal place to be during an earthquake is out in the open, so if you're outside when one hits, stay there. FEMA suggests staying put at first when indoors, too, since studies show that most quake injuries occur when people in buildings try to move to a different room or run outside. Stay in bed if you're there, or get on the floor and protect your head; it may also help to hide under a sturdy table or other object that could protect you if the roof collapses. Crouching near interior, load-bearing walls and in interior door frames is often advised, but stay away from glass windows and exterior walls.

The initial tremors are often foreshocks that precede a larger quake to follow, or may be P waves foreshadowing the more destructive S waves and surface waves. Either way, it's wise to get outside as soon as there's a lull in the shaking. Once outside, get far away from buildings and anything else that might fall, and wait until the tremors stop. Also be mindful of aftershocks, which can occur minutes, hours or days after the main quake. For more tips and scenarios, see these FEMA guides about what to do before an earthquake, during an earthquake and after an earthquake.

And for more about the recent disaster in Haiti and other earthquake issues, check out the following links from MNN:
PHOTOS: Scenes of destruction in Haiti
PHOTOS: Scenes of recovery in Haiti
Reporter's notebook: MNN correspondent reacts to Haiti quake
Why Haiti keeps getting hammered by disasters
Haiti's environment needs long-term help
Forecasting the next big earthquake
Taiwan scientist develops earthquake alarm
New study finds Seattle in danger from a massive earthquake
Study finds sun, moon trigger San Andreas low-level tremors
Earth- and earthquake-friendly housing