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Written By: HeySal on January 20, 2011 No Comment

Serious gold has been found in about 3 out of every 5 states in the US.  While there is still untold amounts of gold to be found, however, it’s not as easy as it was in the 1800′s to find open land to prospect.  You can jump right in and start fishing through streams for a cache, but it can also be a risky and disappointing way to go about any serious prospecting.  There are a few things to consider before loading up the mule and heading off to the mountains that will greatly increase your odds of success – and decrease your odds of ending up in court.

Just because a mine or claim is no longer worked does not mean that the gold is gone.  That particular property, however, might still be off limits to hunters.  Public lands are not always a free for all gold prospecting areas, either.  Some public land contains claims and other areas are off limits to hunting at all.  Some areas are restricted hunting, meaning you can use a pan, but not a dredge or sluice, or other equipment.   If you are thinking that you can just slip into off-limits areas and slip out without notice, you are taking one healthy risk to your wallet or freedom.   By getting some research under your belt before diving into the creeks with your prospecting gear, you can avoid not only fines, arrests, or being shot for claim jumping, you can also get a pretty good idea where your best bet is to find a good productive placer.  The search for records can be time consuming, but it is a “must” do for anyone serious about gold prospecting.

While you will want to know the ownership status of the land you wish to hunt, it’s not going to do you much good to hunt if there isn’t a decent amount of gold to be found in the area.  While you may have heard that gold can be found just about anywhere, a few flakes dropped by glaciers aren’t really going to make a hunt worthwhile.  You should start your search by studying mining records to find areas from which good amounts of gold have already been found. State Bureau of Mines offices will have information about mining in the areas you are researching.  Remember, thousands of people already have searched the country for gold.  You aren’t likely to make much headway in new and untouched territory.  Your best bet is to stick with known territories. While some people believe that areas that contain mines are tapped out, this is rarely the case. Gold in these areas still works its way down into streams and forms placers downhill from the sources.

The city office in the area you are researching will have records of current mining claims as well as records of claims that are now abandoned.  Once you study these and are content with pursuing prospecting in an area, you will want to do another bit of study.  The BLM offices have maps containing land status plats that show the ownership of public lands. Their offices also have mining and mineralogy maps. These offices are where you find out where you are free to prospect.

Claims  become abandoned for many reasons.  Some might be abandoned because the area had been worked until the claim quit producing.  Others may just have never been fruitful in the first place.  Others could be abandoned due to other difficulties that the owner encountered, such as inability to get to and from the claim, illness or death, and a myriad other reasons.  If a claim is abandoned and the land is open to prospecting, you might be able to pick up the claim for a low price and continue work on it. If it has been a considerable amount of time since a claim has been worked, it may contain fresh gold which continues to wash down into placer areas over time.

Local assay offices are sometimes willing to provide information about their own records of gold assays from local area claims, although sometimes you will be charged for records searches.  If the claim produced gold recently enough, someone in the office might just even remember that it produced well.

A bit of geological study about gold is always a good idea for those who are extremely serious about prospecting, too.  What you learn may just help you identify “new” localities near the older, known ones.

While these studies can be time consuming, most areas have several months a year (in some places most of the year) which are not suitable for hunting in the field so these are excellent months to do your “indoor” prospecting.

Once you have the information you need about open land and available claims, you are then ready to go out into the field and try your luck in the 2010 Gold Rush.


Click Here For The Best In Prospecting Equipment

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Written By: HeySal on November 17, 2010 No Comment

Earthquake stats for the year so far have been pretty shaky indeed.  As always, below is included an explanation of where averages come from.  Below that you will find the statistics for the third quarter and the year totals so far.   It’s been a very interesting year all the way around.

About The USGS and RHS1 Averages:

The USGS statistical averages are averages compiled from 1990 to 2000.  That is when global tracking was achieved and we have no way of knowing for sure how accurately those statistics represent numbers before that time.  There are scientists who did tracking, but there were also many very volatile areas that aren’t populated and it was impossible to track before.  From old records we can assume that there have been more recently, but there is no way to know for sure.

We also use an RHS1 average which is 3 year statistical average which was drawn from my three year quake report from  2006, 07, 08  that I will compare the quarterly statistics to, so we can see a more current trend.  At the end of this year we will add this year’s average to the three year average, making an average of 4  of 5 years since the middle of the current decade.  If data can be retrieved for 2009, a year in which our site was being rebuilt from hacker/virus injection damage, we will add those in to make a current half decade statistical average.

8 Magnitude and Stronger:
We had none during the second or third quarter.  We had one in the first quarter.
The USGS average is 1, if any per year.  The RHS1 average is two per year.
We are holding steady at low average for these massive quakes.

7 Magnitude and Stronger:
We experienced a whopping 9 of these shakers this quarter bringing the year total in the third quarter up to 17 – which is the USGS yearly average for these massive quakes.  RHS1 3 year average is 11 annually, a  35% drop from the USGS average.  It looks like these are going to break both averages this year.
.

6 Magnitude and Stronger:
We experienced  37 of these strong quakes in the third quarter.  With  only 29 of these quakes in the second quarter and a the high number of 48 during the first quarter, we have now experienced 114 mag 6 quakes already as of the end of the 3rd quarter.  The USGS average is 134 per year.  RHS1 average is  159 annual mag 6 quakes per year.  Only 20 quakes in the forth quarter will see the USGS average but 45 still need to occur to reach the RHS1 average.  It looks like we will be considering this year a high or a low according to which average you want to look at.

5 Magnitude and Stronger:
There were 401 of these quakes during the 3rd quarter of the year.  We experienced only 285 of these strong shakers second quarter – but we had extremely high numbers the first quarter – 565 of them!  At 1251 total for this year as of the end of the third quarter, we will exceed both averages this year.   USGS average is 1319 per year. The RHS1 average  is only 1275 per year.  Judging from my recordings so far of the 4th quarter, we already have.  The only question left is by how many we will be exceeding averages.

During the first few quarters of the year most quakes were happening at depths of 10 and 35 km, indicating a crustal shift was going on.  In the third quarter there were still quakes occurring at these depths but not in such a profusion as earlier in the year.  The depths are becoming disperse again with no real perceivable patterns to them.

The high number of quakes this year are mainly due to some strong and lengthy aftershocks occurring after the major 7 and 8 magnitude quakes experienced near the beginning of the year.

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Written By: HeySal on October 15, 2010 No Comment

After the first dig, Jessie and I just couldn’t resist taking a second run back there right away. We had another person with us, too – she had seen Jessie’s cache from the first trip and was gung ho to try her hand at digging a few herself. This time the weather was warm but not as excruciating as the first time in.

I did some studying before this trip and found that our spot is in the Southern portion of a formation that runs all the way up to highway 26 and possibly even further North than that. Not having a lot of time to explore this time, we settled for just going back to the dig knowing that we’d find something. Something turned out to be a lot better than our first try at the pit.

Beginner’s luck doesn’t quite explain Jessie’s luck in finding a major pocket. She again had the biggest load to carry back to the car this time. While I had the biggest stone of the day – Jess once again topped me out with a spectacular green moss crystal. Her friend,Gina, was amazed and thrilled with her cache. While she came along expecting to find a few crystals, she was not prepared for the size of the stones she was finding. To tell the truth – neither were we.

For all Gina’s friends back home she said would never believe she actually found those herself — yeah, she did – and they were AWESOME!  I didn’t get pics of hers, but they are about the same trend as the ones in the pics below.

That said – we took some more pics for you all to enjoy.

Favorites from my dig cache

These are my favorites for the day. The one on the left is the biggest single crystal of the day.

The crystal on the left was the biggest single of the day. It’s not the best crystal, however. It’s got a bit too many of the watery feathers in it to be clear at the size it is. The medium size crystals are much clearer than the larger ones.

Quartz Crystals from Copperopolis 5

These are Jessie's favorites from the day.

Jessie  had the biggest cluster (top left) and a lot of beautiful medium sized clear stones. She also got a lot of so-so stones that will probably end up being the start of what I call “driveway rock” collection. Those are the stones you toss in the yard somewhere for decoration. Non-hunters seem to love looking at these piles and picking something out for themselves to take home. There’s always party favors somewhere when you visit a rockhound’s home.

Let’s move on to the real prize of the day – also one of Jessie’s finds:

Moss quartz crystal

Gorgeous water clear crystal with green moss.

I have never seen a true moss quartz crystal before, and perhaps that isn’t the right technical name for it, but one look at that picture and I’m sure you’ll agree that it’s about the best description to be had for this gorgeous stone. It’s close to an inch wide and there is a crust, as you can see, but promises to be a stunning pendant piece when the layer is removed.

We did explore around the rock formation above the dig up by the main road this time. The view was spectacular. Almost spectacular enough to make me actually like being in California for awhile.

Copperopolis view from the top

Veiw from the rock formation above the dig site.

And of course – Rickie had a great time and enjoyed a little more sun and hiking this time with the weather a bit cooler than last time. I think his smile says more about how the day went than anything else I can say.

Dogs can so smile.

Love this guys smile - he says it all for all three of us.

Um….if anyone should make it out to Copperopolis and find a folding army shovel……..It’s mine. Could ya let me know it’s been located?   I’ll be back for it – trust me  on that one!

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Written By: HeySal on October 11, 2010 No Comment

Finding an ancient stash of coins or metal relics has always been exciting, but if a coin was corroded enough, there wasn’t a lot of historical significance that could be tapped from that coin. Advancements in technology are allowing coins to tell tales we never had access to before with old methods of coin analysis.

Using new applications of X-ray fluorescence and isotope analysis, and specialized software and reference materials from the National Institute of Standards and Technology, scientists have at their fingertips a means of nondestructive evaluation analyze coins while extracting vital data about the coin which was previously unavailable to them using older and more destructive methods of analysis.

Coins can now be correctly attributed to the particular ruler when corrosion leaves questions about the origin of the coin, but using the new methods of calibration, scientists can also fingerprint the ores from which the coin was fashioned. Because metals differ from location to location, by fingerprinting the metal the coin is composed of, scientists are able to use the new technologies and methods of calibration to tell where the metal in the coin came from.

By putting together the rulers coins were minted under and location from which the metal originated archaeologists have a means to place the dates of mining industry and find out more about a culture’s commerce than they could ever uncover before. They can also do so with unprecedented accuracy. Tests run on coins have already shown that the mines of Arabia operational much earlier than presumed, although it is still a question whether the Romans had moved to the region earlier than presumed or or whether the mines were already running when they arrived. The interaction between Romans and Arabian culture was going on earlier than supposed.

Fingerprinting metal artifacts is likely to lead to some very startling discoveries about early mining and trade. Perhaps it won’t be long before we find which far away culture was mining the copper of Northern Michigan over six thousand years ago. Is the who-done-it novel about to succumb to a new breed of archaeological reports?

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Written By: HeySal on August 9, 2010 No Comment

Hi Earthquake followers. The second quarter report may come as a bit of a surprise to you who saw our first quarter report, which surely indicated our planet might just shake into pieces at any time!

For those of you who are new to these reports, the explanation of averages is just below.

About The USGS and RHS1 Averages:

The USGS statistical averages are averages compiled from 1990 to 2000. That is when global tracking was achieved and we have no way of knowing for sure how accurately those statistics represent numbers before that time. There are scientists who did tracking, but there were also many very volatile areas that aren’t populated and it was impossible to track before. From old records we can assume that there have been more recently, but there is no way to know for sure.

We also use an RHS1 average which is 3 year statistical average which was drawn from my three year quake report from 2006, 07, 08 that I will compare the quarterly statistics to, so we can see a more current trend. At the end of this year we will add this average to the three year average, making an average of 4 of 5 years since the middle of the current decade. If data can be retrieved for 2009, a year in which our site was being rebuilt from hacker/virus injection damage, we will add those in to make a current half decade statistical average.

The Current Statistics for the 2nd Quarter of 2010:

8 Magnitude and Stronger:
We had none during the second quarter. We had one in the first quarter. The USGS average is 1, if any, per year. The RHS1 average is two per year. We are holding steady at low average for these massive quakes.

7 Magnitude and Stronger:
We experienced 5 of these extreme quakes this quarter. We had 3 during the first quarter. The USGS average is 17 per year RHS1 average is 11 annually, a 35% drop from the USGS average.
With 8 of these quakes at 1/2 year, we are high average for USGS averages, and 68% over for our RHS1 3 year averages.

6 Magnitude and Stronger:
We experienced only 29 of these quakes in the second quarter but had a whopping 48 during the first quarter, which brings us to a total of 77 at the half year mark. The USGS average is 134 per year. RHS1 average is up 16% and from the USGS at 159 annual mag 6 quakes per year. We are currently running below for the RHS1 3 year average at 96%, and high for the USGS 10 year average, running at 114%. Either way we are close to normal but over or under by just a bit depending on whose average you are comparing.

5 Magnitude and Stronger:
We experienced only 285 of these strong shakers this quarter – but we had extremely high numbers the first quarter – 565 of them! So far for the year that brings us to 850 mag 5 quakes at the mid year point.
USGS average is 1319 per year. The RHS1 average is only 1275 per year. If we continued this rate for the rest of the year we would see 129% of the USGS average and 133% of the RHS1 3 year average – a whole third more than average!

Despite a completely calamitous beginning to this year, quake frequency has slowed to a more normal rate of frequency than we could have expected from our first quarter. Of course with half of the year still in store for us, anything is yet possible. We could see either record highs or lows yet – but if frequencies continue as they did this quarter we will be having a pretty unspectacular quake year. When talking about earthquakes, unspectacular is a very good thing!

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Written By: HeySal on May 19, 2010 No Comment

Because gold hunting is taking on interest for so many recently, I’ve been posting some information here on the Gazette for avid new gold enthusiasts. It suddenly occurred to me, though, that I may have put the horse before the cart a little bit in some of my articles. I’m going to correct that now and let you in on exactly where the gold hunt really starts – and where it starts…is on paper.

Serious amounts of gold have been found in about 3 out of every 5 states in the US. While there is still untold amounts of gold to be found it’s not as easy as it was in the 1800′s to find open land to prospect. You can jump right in and start fishing through streams for a cache, but it can also be a risky and disappointing way to go about any serious prospecting. There are a few things to consider before loading up the mule and heading off to the mountains that will greatly increase your odds of success – and decrease your odds of ending up in court.

Just because a mine or claim is no longer worked does not mean that the gold is gone. That particular property might or might not be still be off limits to hunters. Public lands are not always free for all gold prospecting areas, either. Some public land contains claims and other places are off limits to hunting at all. Some areas are restricted hunting, meaning you can use a pan, but not a dredge, sluice, or other equipment. If you are thinking that you can just slip into off-limits areas and slip out without notice, you are taking one healthy risk to your wallet or freedom. By getting some research under your belt before diving into the creeks with your prospecting gear, you can avoid not only fines, arrests, or being shot for claim jumping, you can also get a pretty good idea where your best bet is to find a good productive placer. The search for records can be time consuming, but it is a “must” do for anyone serious about gold prospecting.

While you will want to know the ownership status of the land you wish to hunt, it’s not going to do you much good to hunt if there isn’t a decent amount of gold to be found in the area. You may have heard that gold can be found just about anywhere, but a few flakes dropped by glaciers aren’t really going to make a hunt worthwhile. You should start your search by studying mining records to find areas from which good amounts of gold have already been found. State Bureau of Mines offices will have information about mining in the areas you are researching. Remember, thousands of people already have searched the country for gold. You aren’t likely to make much headway in new and untouched territory. Your best bet is to stick with known territories. While some people believe that areas that contain mines are tapped out, this is rarely the case. Gold in these areas still works its way down into streams and forms placers downhill from the sources.

The BLM office in the area you are researching will have mining and mineralogy maps. Once you study these and are content with pursuing prospecting in an area, you will want to do another bit of study. The BLM also has maps containing land status plats that show the ownership of public lands. You will find there where you are free to prospect. You may also want to check for claims that have been abandoned.

Claims can become abandoned for many reasons. Some might be abandoned because the area had been worked until the claim quit producing. Others may just have never been fruitful in the first place. Others could be abandoned due to other difficulties that the owner encountered, such as inability to get to and from the claim, illness or death, and a myriad other reasons. If a claim is abandoned and the land is open to prospecting, you might be able to pick up the claim for a low price and continue work on it. If it has been a considerable amount of time since a claim has been worked, it may contain fresh gold which continues to wash down into placer areas over time.

Local assay offices are sometimes willing to provide information about their own records of gold assays from local area claims, although sometimes you will be charged for records searches. If the claim produced gold recently enough, someone in the office might just even remember if it produced well.

A bit of geological study about gold is always a good idea for those who are extremely serious about prospecting, too. What you learn may just help you identify “new” localities near the older, known ones.

While these studies can be time consuming, most areas have several months a year (in some places most of the year) which are not suitable for hunting in the field so these are excellent months to do your “indoor” prospecting.

Once you have the information you need about open land and available claims, you are then ready to go out into the field and try your luck in the 2010 Gold Rush.

For the latest in gold equipment to aid you in hunt Click Here

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Written By: HeySal on April 13, 2010 No Comment

Earthquake Watch 2010 1st Quarter Report

There are a lot of people right now who will say that quakes have increased in frequency.  As of this quarter, they are absolutely correct.  There have been an extremely large amount of earthquakes this quarter – when we speak of 5 and six magnitude quakes, anyway.  7 magnitude quakes are actually about average or below, depending on which average you are using and we’re at the average for 8 magnitude.

Most of the overage of 5 magnitude quakes is aftershock from major quakes.  Chile’s recent 8.8 magnitude quake was the seventh largest in recent history and that area rumbled with 5 magnitude aftershocks for several weeks.  Only now are they tapering off.  The aftershocks of major quakes always have the capability of raising the stats for a quarter.

What is different about the recent quakes is they are all happening at depths of either 35 kilometers or 10 kilometers globally.  We are undergoing a shift in the lithosphere at these depths.  Many of the plate borders have already responded to the shift.  There are still areas that haven’t that we really hope will not be effected.

All in all, some of the stats are a bit startling, but there is still three quarters of a year for them to normalize and equal out.

The USGS statistical averages are averages since 1990.  That is when global tracking was achieved and we have no way of knowing for sure how accurately those statistics represent numbers before that time.  There are scientists who did tracking, but there were also many very volatile  areas that aren’t populated and it was impossible to track before.  From old records we can assume that there have been more recently, but there is no way to know for sure.

We also have an RHS1 3 year statistical average which was drawn from my three year quake report from  2006, 07, 08  that I will compare the quarterly statistics to, so we can see a more current trend.

What are the statistics?

8 Magnitude and Stronger:
We had one so far this year.  The 8.8 magnitude that hit Chili last month was the 7th largest in recent history.
The USGS average is 1, if any per year.  The RHS1 average is two per year.

7  Magnitude and Stronger:

We only had three of these this quarter.  The USGS average is 17 per year so we are light of average by around 30%.
RHS1 average is 11 annually, a  35% drop from the USGS average.  If this rate continues we will be  light by one per year so can still be considered in a very average range for these severe events.  In the first weeks of the 2nd quarter, however, you will see these quakes buck up to just barely over RSH1 averages and headed toward USGS averages.

6 Magnitude and Stronger:
Um….wow.
We had 48 of these strong shakers in this quarter.  This amount is over average any way you look at it.
The USGS average is 134 per year.  RHS1 average is up 16% from the USGS  at 159 annual mag 6 quakes.  At the rate of occurrence we saw this quarter we would be seeing  192 of these shakers. If this rate continues we will be 31% over the USGS average and  18% over the RHS1 average.   Ten of these quakes can be attributed to aftershocks of the 8.8 magnitude quake in Chile.  All but a few occurred at depths of 10 – 35 kilometers.  5 were at depths of greater than 100kms.  The rest were shallow quakes of 10 to 35 kilometers, with a few ranging to 50 kms deep so again we are seeing a rash of very shallow quakes for the most part.

5  Magnitude and Stronger:
Another Wow here and add a Yikes.
We had 565 magnitude 5 quakes this quarter.  A continuance of this rate would put us at a whopping 2260 for one year. That is a 42% increase from the USGS average of 1319 per year.  It is an even  larger increase from the RHS1 average which is only 1275 per year.  For the three years of tracking at RHS1, we actually had fewer than average mag 5 quakes. We are sitting on a 44% increase from the more recent 3 year average.  Again, many of these quakes – literally hundreds were aftershock tremors of strong quakes.

Aftershocks can be expected after any major quake.  The statistics for average amounts of quakes are built over years and the years always include some major quakes so the statistics do reflect these aftershocks as well as random quakes.  This year as our major quakes are occurring at shallow depths, we’re getting massive amounts of aftershocks, too. We are also experiencing these shallow quakes around the globe generally as well.  Doomsday sayers can  have fun with this shift in the lithosphere, but if you aren’t real fond of “end of the world” stories, you’re in the right place because I’m not going to tell you one.

Our crust shifts periodically just as our magnetic poles do.  A few years ago I found out that our magnetic North pole is traveling toward Siberia at the rate of 25 miles a year.  As a magnetic pole travels, matter will align with it just as it always does.  When this alignment begins to effect the centrifugal force, land mass will move.  That appears to be the case in the current frequencies of quakes as they are all being experienced at the same depths globally and the plate boundaries are being shaken with extreme strength indicating severe pressure on them.  If you find this movement frightening, if you live on a subduction zone or major fault line, you have a right to be worried.  So far several of these zones have been experiencing strong quakes. As far as the end of the world?  Um…don’t count this shaking being an indication of it.   Our magnetic poles shift fairly often.  They have done so several times in the last few hundred years and so far humans seem to be surviving as a species even though there are more people living in zones with catastrophic potentials.  If masses of people live in a volatile subduction zone area, we will see massive destruction when the zone snaps.  We will see destruction from tsunamis as humans continue to build in tsunami prone areas of coastlines.

While there is still no sure-fire means to predict earthquakes, the recent trend makes it likely that other plate boundaries will snap in the near future. You will find information about two of the most volatile subduction zones in the May RHS1 Connector newsletter.

Until then, may all your shaking take place on a dance floor.

<a href=”http://www.mylivesignature.com” target=”_blank”><img src=”http://signatures.mylivesignature.com/85678/heysal/3d7cebe4711209357a777bce172bf9a1.png” border=”0″ style=”border: 0 !important; background: transparent;” /></a>

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Written By: HeySal on February 27, 2010 No Comment

HAWAII TSUNAMI — (for general info about Tsunamis, please see my comments to the last post.)

USGS WARNING for HAWAII TSUNAMI
EVALUATION

A TSUNAMI HAS BEEN GENERATED THAT COULD CAUSE DAMAGE ALONG
COASTLINES OF ALL ISLANDS IN THE STATE OF HAWAII. URGENT ACTION SHOULD BE TAKEN TO PROTECT LIVES AND PROPERTY.

A TSUNAMI IS A SERIES OF LONG OCEAN WAVES. EACH INDIVIDUAL WAVE CREST CAN LAST 5 TO 15 MINUTES OR MORE AND EXTENSIVELY FLOOD COASTAL AREAS. THE DANGER CAN CONTINUE FOR MANY HOURS AFTER THE INITIAL WAVE AS SUBSEQUENT WAVES ARRIVE. TSUNAMI WAVE HEIGHTS CANNOT BE PREDICTED AND THE FIRST WAVE MAY NOT BE THE LARGEST. TSUNAMI WAVES EFFICIENTLY WRAP AROUND ISLANDS. ALL SHORES ARE AT RISK NO MATTER WHICH DIRECTION THEY FACE. THE TROUGH OF A TSUNAMI WAVE MAY TEMPORARILY EXPOSE THE SEAFLOOR BUT THE AREA WILL QUICKLY FLOOD AGAIN. EXTREMELY STRONG AND UNUSUAL NEARSHORE CURRENTS CAN ACCOMPANY A TSUNAMI. DEBRIS PICKED UP AND CARRIED BY A TSUNAMI AMPLIFIES ITS DESTRUCTIVE POWER. SIMULTANEOUS HIGH
TIDES OR HIGH SURF CAN SIGNIFICANTLY INCREASE THE TSUNAMI HAZARD.

THE ESTIMATED ARRIVAL TIME IN HAWAII OF THE FIRST TSUNAMI WAVE IS

1105 AM HST SAT 27 FEB 2010

Please note that this huge quake has sent shock waves headed for all Pacific coastlines. These waves have been measured between an inch and 7.3 feet. If you live in any pacific coastal area you should be taking precautions at this time. It is not the day to enjoy the beach – trust me on that one.

Since my last post there have been 8 more 5.2 – 5.5 mag quakes in Chili. Only one of the 5 mags quakes so far today have been in another location – which was the Rukuyu Islands of Japan where a 7.0 magnitude quake was experienced just yesterday (2/26). One of the subsequent 6 magnitude 6 quakes was also in Argentina rather than Chile, but is most probably resultant from the Chili occurrence.

IN OTHER NATURAL DISASTER NEWS — VOLCANOES

There are at the time 25 Volcanoes at Code Orange, alert level 3 are active globally at the time

There is also one Volcano at Code Red, Alert Level 5 is now active — Chaiten on the Gulf of Corcovado has been code red since the 18th of February.

About Alert Codes and Alert Levels:

ORANGE = Volcano is in eruption or eruption may occur at any time.
OR Alert Level 2
Alert Level 3 = Significant local eruption in progress.
Alert Level 4 = Hazardous local eruption in progress.

RED = Significant eruption is occurring or explosive eruption is
expected at any time.
OR Alert Level 5

It seems that the current crustal shift is playing some havoc. Those in volatile areas may want to start keeping track of what scientists are saying about prospects for disasters in their own areas, and start learning to prepare for them as well.

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Written By: HeySal on February 27, 2010 2 Comments

Over the last few weeks earth has been showing signs that there is crustal shifting – 10 km deep quakes have been occurring globally. These quakes were accompanied by the recent deadly quake in Haiti and have been occurring with frequency since….although not always at notable magnitudes.

Last night Chile was hit by an 8.8 magnitude quake that is sending a wall of water toward Hawaii. It is expected to hit the Hawaii coast in a few hours – around 11:00. They have updated that time recently -the water is moving faster than they had first realized.

On the 26th a 7.0 magnitude quake hit just off of Japan at 22km depth – sparking tsunami watches.

As of the magnitude 8.8 quake that hit Chile last night at a depth of 35km, there have been six magnitude 6 quakes at 35km depth – on 6.9 quake which is very nearly the size that just toppled Haiti.

For perspective on the wall of water headed for Hawaii – it is about three times the size of the 2004 Tsunami in Indonesia.

There have also been 28 after shock quakes of 5.0 – 5.9 magnitude at depths of 35km in the region of Chili since that time.

We will update you on this event with more information about quakes and current geological states of the earth today.

If you are living in a coastal area, you might just want travel in shore a ways today even if you are not in Hawaii.

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Written By: HeySal on January 23, 2010 No Comment

HEY NEW JERSEY ROCKHOUNDS

If you have a puzzling specimen sitting on the shelf that you just can’t identify or have other questions about mineral identification, you really don’t want to miss the 42nd annual open house at The Geology Museum at Rutgers, The State University of New Jersey, on January 30th.

At the open house people can have their own samples professionally examined.  There will also be a mineral sale for those looking to add some great material to their own collections, as well as hands-on geology activities for children.

Along with the rock and mineral identification program, earth science presentations include:
Earthquake Detection for the Citizen Seismologist 3:00 pm
Madagascar’s Buried Treasure: Dinosaur and other Vertabrate Fossils from the Land that Time Forgot 2:00 pm
Paleoclimatic Framework of Human Evolution: Examples from Olduvia Gorge 11:00 am
Monitoring our Ocean Planet: The Scarlet Knights Trans-Atlantic Challenge 10:00 am

Saturday, Jan. 30, 9 a.m. to 4 p.m.

The Geology Museum at Rutgers
The State University of New Jersey
Scott Hall
43 College Avenue
New Brunswick presentations in room 123
mineral sale in room 135
hands-on children’s activities in room 115.

Additional presentations in Geology Hall
85 Somerset Street
New Brunswick
rock and mineral identification, children’s activities in Geology Museum, 2nd floor

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