Going indepth on Cowboys' Murray

Thursday, June 28, 2012

I have been writing about the NFL since I graduated from college seven years ago. Particularly as a Rotoworld writer whose responsibility it was to present the work of others on our aggregative player news page, I have come across many impressive football minds. The reporting of Adam Schefter and Jay Glazer, the film study of Ron Jaworski, the multi-dimensional knowledge of Mike Florio, Gregg Rosenthal, and Adam Caplan. The college-to-pro projections of Mike Mayock.

But no one's analysis, opinions, and evaluations are quite as fascinating or instructive as Greg Cosell's. I'm going to assume you already know a little bit about Cosell because we pass along his work so often on the website. If not, do a quick Google search.

Entering my Thursday morning interview with Cosell, I had planned to do one column discussing five NFL running backs. The interview was finished after 14 minutes, and Cosell provided so much information that I was compelled to turn it into a six-part series.

For the most part, I'm just going to let Cosell do the talking. It's better that way. He speaks incredibly concisely. We first discussed Cowboys tailback DeMarco Murray.

I began by asking for Cosell's general impressions.

"DeMarco Murray ended up playing better in Dallas than I thought he would based on watching his college tape," Cosell acknowledged. "I thought watching him at Oklahoma, he was somewhat of a straight-line guy. Very good downhill when he put his foot in the ground, but pretty much a straight-line runner. And while I wouldn't call him overly shifty or elusive, I thought that he showed much more of that in the NFL.

"And the other thing, which I found really intriguing watching him in Dallas, was I thought he ended up having a little more natural power than I thought, watching his college tape. And I think those two elements -- a little more lateral agility and a little more natural power and strength -- really made him an effective runner. Because there's no question that he has good speed and good short-area acceleration. Clearly, when he put his foot in the ground and got downhill, there was a burst to his game. And you need that, you certainly need that. But I thought those two other elements were things that I did not think he would be able to show in the NFL. Because I didn't really feel like I saw them when I watched him at Oklahoma."

I asked Cosell to expand on his definition of "straight-linish" as it related to Murray, and he explained how either possessing or lacking that characteristic might impact success for an NFL back.

"He's certainly not elusive the way you think of Adrian Peterson as being shifty or elusive," Cosell said of Murray. "Or the way you would think of a guy like LaDainian Tomlinson in his prime, being laterally explosive. He wasn't quite like that. But he showed enough of it. Because you have to be able to do that in the NFL. In the NFL, it's more important for a back to be laterally agile and explosive than it is for him to be fast in terms of long speed.

"There's very few long runs in the NFL where guys run in a straight line. That doesn't happen very much. In the NFL, you must really be able to create space for yourself in confined areas. And the way you create space in confined areas is with lateral movement. And if you can't do that, you have limitations as a runner. And he did that much better than I anticipated based on his college tape."

I asked Cosell how Murray could have suddenly become a laterally gifted runner after failing to show that ability in college.

"Look, I could have misevaluated him," Cosell conceded. "Hey, just because I do this and I think I'm pretty good at it, that doesn't mean that I don't misevaluate players. That's just the way it goes. I'll give you a perfect example, and I think I misevaluated him, too: Donald Brown of the Colts. First-round pick. And I thought he'd be a very good NFL back. And I think the reason he's not become one up to this point -- and I don't think he will become a great one -- is he has not shown that lateral movement. I thought he had it when I watched him at Connecticut. He hasn't shown it in the NFL. So, he's become a guy who, if he doesn't really have room to run based on the blocking scheme, then he doesn't do very much.

"Murray, I thought would be like that. But it's turned out, he's shown the kind of lateral movement where he has been able to create space for himself."

Murray is a popular 2012 breakout candidate after rushing for 897 yards on 164 carries (5.47 YPC) in 13 games with seven starts last season. If Murray stays healthy and continues to run like he did as a rookie, he?ll have every opportunity to fulfill those lofty expectations.

Next up: Redskins running back Roy Helu.

I have been writing about the NFL since I graduated from college seven years ago. Particularly as a Rotoworld writer whose responsibility it was to present the work of others on our aggregative player news page, I have come across many impressive football minds. The reporting of Adam Schefter and Jay Glazer, the film study of Ron Jaworski, the multi-dimensional knowledge of Mike Florio, Gregg Rosenthal, and Adam Caplan. The college-to-pro projections of Mike Mayock.

But no one's analysis, opinions, and evaluations are quite as fascinating or instructive as Greg Cosell's. I'm going to assume you already know a little bit about Cosell because we pass along his work so often on the website. If not, do a quick Google search.

Entering my Thursday morning interview with Cosell, I had planned to do one column discussing five NFL running backs. The interview was finished after 14 minutes, and Cosell provided so much information that I was compelled to turn it into a six-part series.

For the most part, I'm just going to let Cosell do the talking. It's better that way. He speaks incredibly concisely. We first discussed Cowboys tailback DeMarco Murray.

I began by asking for Cosell's general impressions.

"DeMarco Murray ended up playing better in Dallas than I thought he would based on watching his college tape," Cosell acknowledged. "I thought watching him at Oklahoma, he was somewhat of a straight-line guy. Very good downhill when he put his foot in the ground, but pretty much a straight-line runner. And while I wouldn't call him overly shifty or elusive, I thought that he showed much more of that in the NFL.

"And the other thing, which I found really intriguing watching him in Dallas, was I thought he ended up having a little more natural power than I thought, watching his college tape. And I think those two elements -- a little more lateral agility and a little more natural power and strength -- really made him an effective runner. Because there's no question that he has good speed and good short-area acceleration. Clearly, when he put his foot in the ground and got downhill, there was a burst to his game. And you need that, you certainly need that. But I thought those two other elements were things that I did not think he would be able to show in the NFL. Because I didn't really feel like I saw them when I watched him at Oklahoma."

I asked Cosell to expand on his definition of "straight-linish" as it related to Murray, and he explained how either possessing or lacking that characteristic might impact success for an NFL back.

"He's certainly not elusive the way you think of Adrian Peterson as being shifty or elusive," Cosell said of Murray. "Or the way you would think of a guy like LaDainian Tomlinson in his prime, being laterally explosive. He wasn't quite like that. But he showed enough of it. Because you have to be able to do that in the NFL. In the NFL, it's more important for a back to be laterally agile and explosive than it is for him to be fast in terms of long speed.

"There's very few long runs in the NFL where guys run in a straight line. That doesn't happen very much. In the NFL, you must really be able to create space for yourself in confined areas. And the way you create space in confined areas is with lateral movement. And if you can't do that, you have limitations as a runner. And he did that much better than I anticipated based on his college tape."

I asked Cosell how Murray could have suddenly become a laterally gifted runner after failing to show that ability in college.

"Look, I could have misevaluated him," Cosell conceded. "Hey, just because I do this and I think I'm pretty good at it, that doesn't mean that I don't misevaluate players. That's just the way it goes. I'll give you a perfect example, and I think I misevaluated him, too: Donald Brown of the Colts. First-round pick. And I thought he'd be a very good NFL back. And I think the reason he's not become one up to this point -- and I don't think he will become a great one -- is he has not shown that lateral movement. I thought he had it when I watched him at Connecticut. He hasn't shown it in the NFL. So, he's become a guy who, if he doesn't really have room to run based on the blocking scheme, then he doesn't do very much.

"Murray, I thought would be like that. But it's turned out, he's shown the kind of lateral movement where he has been able to create space for himself."

Murray is a popular 2012 breakout candidate after rushing for 897 yards on 164 carries (5.47 YPC) in 13 games with seven starts last season. If Murray stays healthy and continues to run like he did as a rookie, he?ll have every opportunity to fulfill those lofty expectations.

Next up: Redskins running back Roy Helu.

Evan Silva is a senior football editor for Rotoworld.com. He can be found on Twitter .
Email :Evan Silva

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Intermission: Sunset Crater

(Apologies to Mount St. Helens fans. I didn?t have this week?s installment written up in advance, and now my uterus has attacked. We?ll get on with the saga next week. For now, I?ll chuck a repost from En Tequila Es Verdad at you, introducing you to a volcano of my youth. This was written in July of 2009. I?ve prettified the photos for you a bit. I didn?t have teh super-awesome photo editing software back in the old days. I hope you like this sweet little cinder cone as much as I do ? she?s a beaut, although not a butte. Ah-ha-ha. Sorry, I couldn?t help myself just there. You know geologists and puns?)

Sunset Crater, a fabulously beautiful cindercone just outside Flagstaff, AZ. I spent much of my childhood learning to love volcanoes here. Photo is taken from a meadow created by lahars from the San Francisco Peaks, a stratovolcano that dominates the view to the southwest. Image courtesy Cujo359.

The winter of 1064-65* wasn?t a particularly good one for the locals. There was the 6 mile fissure that opened and began pumping out lava. Then one end of the fissure started throwing scoria at them, collapsing the roofs of their pit houses under hot heaps of fresh cinders and ash. Then more lava flows filled in forested valleys. By the end of it, fields of corn lay buried, the landscape had undergone a fairly dramatic makeover, and the severely surprised Sinagua had discovered?the art of basalt corn cobble making. They relocated to points less explosive nearby, where a beautiful new volcano formed a backdrop and gave a fertility boost to their fields.

These things happen when you live in the San Francisco Volcanic field.

This digital elevation model (DEM) of the San Francisco Volcanic Field shows many of the more than 600 vents which have erupted in the area during the past 6 million years. Some lava flows (flat lobate features) are easily recognized by their proximity to vents. Larger tectonic structures such as the northeast-trending Mesa Butte Fault and Doney Fault are also seen. Flagstaff lies at the south-central edge of the volcanic field nestled between the base of Elden Mountain and the Observatory Mesa flow emitted from A-1 Mountain. Image courtesy USGS.

Northern Arizona would be a flat, arid plateau if it wasn?t for the hot spot beneath it. For 6 million years, volcanoes have erupted here, steadily marching east. The field extends from Williams in the west to the banks of the Little Colorado River in the east, and from just below Flagstaff in the south nearly to Cameron in the north ? an area of roughly 1,800 square miles. It contains the highest point in Arizona ? 12,633? Humphreys Peak ? as well as the youngest volcano, Sunset Crater. If you?re looking for a particular type of volcano, chances are the San Francisco Volcanic Field has it, from lava domes to a stratovolcano to dozens of cinder cones of all shapes and sizes. With 600+ volcanoes to choose from, you can?t complain. And if you?re really lucky, you might get a chance to see a new volcano born, since the field?s still potentially active. Geologists think any future eruptions will be small enough to get a spectacular show without inconveniencing the locals?too much.

Sunset Crater would have put on quite the show itself. The six mile long?curtain of fireserved as the opening act, and while it probably wasn?t quite as vigorous as many Hawaiian fissure eruptions, brilliant red lava shooting up from the ground is still an impressive sight. But that was merely the prelude. Activity along the fissure slowed quickly, becoming concentrated at the northern end, where the?real?show was starting. Explosions ejected fragments of lava high into the air; as those fragments cooled mid-air, the dissolved gasses within them exsolved and created dozens of vesticles, peppering the fragments with petrified bubbles. They rained down around the vent, piling into a cone. The heat, the smell, and the noise would have been overwhelming.

We have a good idea what the Sinagua saw. It would have been quite a bit like Paricut?n?s birth:

Loud, isn?t it? One begins to understand why the Sinagua fed it corn: I imagine they were trying desperately to calm it down.

If they found a good vantage point on nearby mountains, they might have seen bits of the newly-birthed crater rafting away on lava flows. You can still see chunks of?red oxidized agglutinate, pieces of the original cone, trapped in the Bonito flow.

Red oxidized agglutinate in the Bonito Lava Flow, Sunset Crater, AZ. Image courtesy Cujo359.

The explosions continued, filling Sunset Crater?s gaping wounds with fresh scoria, and leaving the volcano with smooth, unblemished flanks.

As the eruption waned, something wonderful happened. Fumaroles formed near the crater?s rim, venting hot gasses that oxidized the basalt scoria. The iron contained within basically rusted, painting the rim in gorgeous sunset colors. The fumaroles cemented the rim with?silica,?gypsum and iron oxide; as a finishing touch, they deposited?sulfur compounds,?opal,?hematite,?jarosite, and?magnetite. Nature had created a masterpiece.

When all was said and done, the volcano topped out at 1000 feet in height, a mile in width, and contained a crater 400 feet deep, which itself hosts a 160 foot deep secondary crater. The local Sinagua might have considered it a decent consolation prize for getting volcanically evicted from their forested valley.

The visible?interior of Sunset Crater is covered with a smooth coating of scoria, but we can get a look inside her if we head over to Red Mountain, many miles to the west.

Red Mountain cinder cone, near Flagstaff, AZ. Check out that interior! Image courtesy Cujo359.

This is the eroded interior of a cinder cone. Steam and percolating water welded its layers of cinder and ash together with the same sorts of mineral oxides that cemented Sunset Crater, creating a volcanic material called?tuff. We get this inside-look at the anatomy of a cinder cone because the entire western side of Red Mountain got itself rafted away by a lava flow, leaving an enormous ampitheater carved out of the cone. This time, there was wasn?t any explosive action to replace the missing bits.

Lava can do some pretty outrageous things. And thanks to Northern Arizona?s cool, dry climate, we can get a nearly unweathered view of its antics. Rain and snowmelt just sink right in without disturbing the surface of the flows too much. If it wasn?t for the lichens and hardy bushes peppering the flows, you?d think they?d just erupted last week.

The Bonito Lava Flow, Sunset Crater, AZ.

Most of the flows around Sunset Crater are composed of a?a lava. There is a good reason why the Hawaiians call it a?a, which means, basically, ?stony, rough lava.? It?s a stony, rough lava comprised of clinker, broken chunks of lava carried along the top by a dense, pasty core. As?that hotter core oozes its way downslope, the clinker goes along for the ride, tumbling over the leading edge like a bunch of over-excited kids at a slow-motion water park. The tumbled chunks get buried as the flow ambles on. Thus, you get a sort of lava sandwich: clinker top and bottom, paste in the middle. Don?t bite into a fresh flow, though: it?s erupting at temperatures of 1000-1100 degrees C. That?s 1800-2000 degrees F. That?s bloody?hot.

Back when I was a wee kiddie, our teachers showed us a video of an a?a flow filmed in Iceland. I?ll never forget the sound. As the clinker tumbles, it makes a cacophony like a monstrous china cabinet getting knocked over. This video from Hawaii demonstrates that nicely:

?

Is that, or is that not, simply awesome?

There are two ways a?a is formed from a basalt flow. One of them is when the basalt is high in gas bubbles and (relatively) low in temperature, thus high in viscosity. The other is when the strain rate of the flow is high ? such as when it hits steep ground. Remember this, as it will factor in to the following discussion.

Sunset Crater?s lava flows weren?t limited to a?a. The Bonito flow began close to the western margin of the volcano as pahoehoe, a Hawaiian word meaning ?smooth, unbroken lava.? It?s a far more liquid basalt that forms a beautiful, smooth surface, sculpted into undulating billows or ropy loops. It forms that way because of the way very fluid lava moves under a congealing surface crust. It?s hot stuff, 1100-1200 degrees C (2000-2100 degrees F), with a low gas bubble content.

Now, the interesting thing is this: pahoehoe can easily turn to a?a, depending on how the flow goes. If pahoehoe hits an uphill climb, it?ll cool down, slow down, and get all clinkered up. Same thing can happen as the flow cools further from its eruption site. Isn?t that neat?

You can get an idea of what something like that looks like from this video of pahoehoe and a?a flows merging:

Pahoehoe also means ?good to walk? in Hawaiian. When I was a kid visiting the Crater, our field trip guide explained the name origins thusly: the Hawaiians, walking barefoot over flows, would try to tiptoe over the rough stuff, exclaiming: ?Ah! Ah!? And then, when their feet hit the smooth, soothing surface, they?d sigh in relief: ?Mmmm,pahoehoe!?

You?ll never forget the difference now, will you?

The Bonito flow turned from pahoehoe to a?a as it lost its gas on the trip out from the mountain. Big cracks formed in its surface from the frictional drag of the liquid lava below the cooler crust, and as that weak crust collapsed when lava drained away from beneath it. It?s the youngest and biggest of Sunset Crater?s two flows. It covers almost two square miles, and ranges from 100 feet deep in its center to less than 6 feet along the margins. It filled in a basin surrounded by older volcanoes. The other major flow, Kana?a, flowed down an old stream bed for several miles, and never got more than 1000 feet wide. Sunset Crater?s continued eruptions covered it in cinders, allowing a lot more vegetation to take root along its surface. Both flows, as well as the cinders, are alkai olivine basalt, which is composed of microscopic crystals of?plagioclase,?olivine and?augite. The occasional big white chunk of stone embedded in the basalt is a?xenolith, in this case formed when lava ripped a hunk of Kaibab limestone out of the underlying formations and took it along for the ride.

Crack in the Bonito Flow. This stuff's rough!

The Bonito lava flow is where you?ll see most of the interesting formations. For a crash course in lava, there?s nothing better than the trail that meanders through it. You can take?an online field trip, but we?ll hit some of the high points here.

A squeeze-up in the Bonito Lava Flow. Image courtesy Cujo359.

If you?ve never used ?lava? and ?toothpaste? in the same sentence before, that?s probably because you?ve never seen a squeeze-up. These form when gummy, partially-cooled lava squeezes its way through already-hardened cracks in the flow. It?s pretty much the consistency of toothpaste. A close inspection will show you the marks left as it scrapes by the solid stone around it.

The Bonito flow also contains lava tubes, formed when molten rock drained from its solidified surroundings. Those tubes are cold ? basalt?s a terrible material for trapping heat. In colder, wetter Arizona days, the tubes used to contain ice full time. Now, they?re usually dry, but frigid. Alas, Bonito?s main tube collapsed some time ago, so you can?t go exploring it anymore. This is good news for the claustrophobic set, not such good news for the spelunkers among us.

You can console yourself with a hornito.

A hornito on the Bonito Lava Flow. Image courtesy Cujo359.

Yes, I know most of you associate the word ?hornito? with tequila, for good reason ? Hornitos is an excellent brand. In this case, though, hornito means a small spatter cone formed on the surface of a basalt flow. It?s created when lava is forced up through the cooled surface. Hornitos are fed by the flow itself, rather than its own magma source as is the case with a regular spatter cone. They?re steep-sided heaps of splattered lava that splashed down and over the developing cone, welding itself as it goes. The lava?s still partially liquid when it falls, which is why it doesn?t form distinct cinders, although the principle?s roughly the same.

Watching one form is a fascinating experience:

Sunset Crater?s hornito used to be taller, but volcanoes aren?t all that good at welding, and people broke it down by sitting on it and taking away chunks. It?s still an impressive feature, though.

Just past the hornito, you?ll catch sight of something that looks like a mini-cinder cone. It?s a cinder dune. This gives you some idea of just how much material Sunset Crater ejected.

Cinder dune at Sunset Crater. Image courtesy Cujo359.

Sunset Crater is a geologists? dream. There are few places in the continental United States where volcanism is so wonderfully demonstrated, without all the pesky plants in the way. And, just over the horizon, ancient oceans lie exposed, and prehistoric apartments look out over Painted Desert vistas.

But that?s a story for another Sunday Sensational Science. For now, I?ll just leave you with a portrait of Sunset Crater and her lava flows, and let you ponder the power of hot rock to create a work of art:

Sunset Crater, seen from the trail through the Bonito Lava Flow.

?

References:

Bezy, John V. (2003): A Guide to the Geology of the Flagstaff Area. Tucson, AZ: Arizona Geological Survey.

Hanson, Sarah L. (2003): Roadside Geology: Wupatki and Sunset Crater Volcano National Monuments. Tucson, AZ: Arizona Geological Survey.

Priest, Susan S. et al (2001): The San Francisco Volcanic Field, Arizona. U.S. Geological Survey Fact Sheet 017-01.

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92% Safety Not Guaranteed

All Critics (75) | Top Critics (27) | Fresh (69) | Rotten (6)

Neatly, the script embarks on one journey while dangling the possibility of another: the prospect of taking a sudden leap from comic reality into the realm of pure imagination.

"Safety Not Guaranteed" is most vibrant and vital at its edges, in the way that the characters interact with each other while waiting for something to happen.

It's brisk and assured and never begs the audience's indulgence. No time is wasted. The movie is, at every moment, either funny or pushing the story forward, or both.

The film is modest but skillful and heartfelt, spiced just so by Plaza and company.

Safety Not Guaranteed casts an enchanting spell from its opening scene.

Expectedly funny but unexpectedly touching, too.

Hope is a powerful thing and Safety Not Guaranteed delivers in its tale of longing, deliverance and connection during the here and now.

An intriguing yet erratic effort...

Less of a philosophical argument and more of a character piece driven deep into the heart by Duplass and Plaza.

Have you ever wondered what mumblecore sci-fi would look like? Wonder no more.

Rather than trying to beat Hollywood at its own game of high-tech gadgets and weaponry, director Colin Trevorrow and writer Derek Connolly achieve a sly mix of the insane and the mundane.

A character-driven piece about regret and true partnership - our basic, primal need for someone to take the journey with us even if safety is not guaranteed.

Aubrey Plaza is the best thing about this iffy mock-sci-fi doohickey.

As a hipster rom-com about people trying to shake off their pasts to make present-day connections, it's pretty satisfying.

A strange, light-hearted bit of quasi-sci-fi, with no small amount of heart.

The material is played mostly for laughs and succeeds in that regard. The undercurrent of lament in Safety Not Guaranteed, though, is what holds the film together.

If safety isn't guaranteed by the film's title, a viewer's satisfaction with this genial, warm-hearted movie pretty much can be.

One central recasting and brutal editorial session away from being a lovely little short film, where its mystery and sentiment is more easily controlled and considered.

With its well-constructed screenplay, sharp dialogue and unapologetic sincerity, this first feature from former SNL interns Colin Trevorrow and Derek Connolly is its own act of nostalgia...

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Watch british tv online | TV 2M

Watch british tv online

Posted by TV2M.com on June 17th, 2012 ? Posted in Television

? Tags: British, Online, Watch

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Nonetheless, the most crucial thing is to study with an open mind and be willing to revise your understanding if necessary.It was in 1962 that the extremely initial television signal was up linked from Europe on to the Telstra satellite television and beamed more than North America. How Does Satellite tv Television Function?!?Properly, without having going technical, it will interest you to note that the tv set indicators you obtain from communications satellites are actually very first sent up from ground stations by means of really large (9 ? 12 meters) dishes to an orbiting satellite that in turn beams the indicators down to earth and on to your receiver?s parabolic dish?s focal point and a LNB or reduced noise blocker component converts ands send the signs to your decoder box where the final conversion is carried out to the signs so that it becomes the sound and images you view.In this case satellite television tv set indicators are received with a satellite television antenna and directed via a satellite tv decoder box and an oscillator converts it to L-band variety of frequencies that an on-board electronics lastly converts to the regular frequency usable by regular television sets.What Is A TVRO?!?As soon as you commence to move beyond fundamental background details, you commence to recognize that there?s more to the long term of satellite television Television vis a vis World wide web television software program than you might have initial thought.DBS is satellite tv Tv broadcast thorough Ku-Band satellites that function on higher frequencies with more powerful indicators than C-Band or TVRO, which creates it feasible for you to set up smaller dishes for getting their indicators.This is produced feasible simply because DBS tv set satellites are usually in geosynchronous orbit that is stationary in the sky relative to the Earth, simply because every satellite television is released into area at around 7,000 mph to settle at close to 22,200 miles above the Earth.With this speed and height, the satellite television revolves all-around the earth as soon as each and every 24 hours in juxtaposition with Earth?s very own rotation. This is what creates it feasible for your 18 inches dish to continue to be in a fixed position with the satellite tv without having requiring adjustment.What is Internet Tv and Is It Better than Direct Broadcast Satellite television??World wide web television as the name implies refers to Television applications streamed onto a Personal computer or Laptop computer through the Web. There are different kinds of Web tv services. Some of them are recorded rebroadcasts although other people are live broadcasts created feasible with ingenious software program. You don?t need any hardware such as decoder, wire, dish or antenna making. You can watch your preferred programs, even outdoors, from all above the globe, so long as you have web connection. World wide web tv is just a headache free of charge way of viewing a lot more numbers of satellite tv Television programs and channels free of monthly satellite television television subscription costs.What would be the long term of Satellite tv Tv set depends on a number of factors: For instance, even just before the advent of Web tv satellite tv businesses did not depend on subscription fees for their survival.For instance, If you are in the UK and you have gear that is capable of receiving Tv indicators then the law states you should pay for a Tv license.Nowadays, there currently exist broadcasters who use only promoting to spend for their support and so enable viewers free of charge viewing of their software programs, so in my opinion watching satellite television television applications free on your Computer or Laptop computer will not kill satellite tv tv, rather World wide web tv will improve the amount of viewers for satellite tv solutions and lead to much more and far better priced advertising charges.

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Whirlpool Gladiator GarageWorks Fold-Away ... - Garage - EzineMark

If you?re running out of floor space in your garage, but still want to expand the storage space, then the Whirlpool Gladiator Fold-Away Work Station available at Nebraska Furniture Mart is just what you need! Designed exclusively for the space-conscious garage owners, this convenient storage unit also doubles up as a workstation when required. Now, let?s take a closer look at the features that make this garage workstation a must-buy!

Ample Storage Space:

With three shelves, this Gladiator GarageWorks cabinet provides plenty of room for a variety of tools, car equipment, and garden supplies. The lower shelf has a convenient access hole, so you can power up your radio, work station lamps, and more.

Space-Saving Fold-Down Work Surface:

This Gladiator garage cabinet folds down to provide a sturdy stainless steel work surface.

So whether you want to do small repairs or some gardening tasks, this work surface is sure to keep you comfortable. So how does it work? A heavy-duty latch with round pin together with a recessed handle makes it easy for you to fold out the workspace. Well, when you don?t need it, you can always fold it out of way! The door has a tread plate pattern, so if you have filled your garage with products from Gladiator GarageWorks, then it will certainly blend well with them.

Built to Last:

When this garage cabinet is from Gladiator GarageWorks, you don?t really have to worry about its durability! Steel cabinet panels together with heavy-duty screws make this cabinet extra durable to serve in your garage for years to come. Plus, it comes with protective powder coating, which means your cabinet will not rust or corrode over time!

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Mounting the Whirlpool Gladiator Fold-Away Work Station on the wall isn?t complicated too! Simply use the included hanger to mount on reposition it as you desire.

With so many pluses, this Gladiator garage cabinet is just too hard to resist, isn?t it? Well, you don?t really have to spend a fortune to get this convenient storage unit. At NFM, you?ll find it at a price that?s easy on your pocket.

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Texas Rangers Forget Southern Hospitality, Destroy Toronto Blue Jays

Jim Cowsert-US PRESSWIRE

The Texas Rangers returned from their first off day in three weeks with a vengeance on Friday night, smashing the Toronto Blue Jays 14-3 in a game that wasn?t even that close. The Rangers jumped on the Blue Jays early by scoring six runs in the first inning, knocking starter Brandon Morrow from the game after 44 pitches, but before he could record a third out. On the other side of the coin, Derek Holland delivered his best start of the year, pitching 7.1 innings, giving up just two runs, walking one, and striking out nine.

Quick-hit style notes from tonight?s game:

• Ian Kinsler started the Rangers big first inning off with a 13-pitch walk. He would go on to see 41 pitches in his five at-bats on the night.
• Holland struck out the side twice. In the 1^st inning he sat down all three Blue Jays hitters he faced on swinging strikeouts. In the 6^th inning he gave up a solo home run to Edwin Encarnacion, but the other three hitters he faced in the inning were punchouts.
• Nelson Cruz finished the night with eight RBIs, punctuated by an opposite-field 414 foot grand slam in the 7^th inning. Cruz now has five home runs for the year, two of which have been grand slams. Before this year, his last regular season grand slam was in 2009 (he did hit a walk-off grand slam in the 2011 ALCS).
• The Rangers have won 4 games at home in the month of May. Their average margin of victory in those four games is 6.5 runs. Three of those games were started by C.J. Wilson, Jered Weaver, and Brandon Morrow.
• Wilson, Weaver, and Morrow entered their games against Texas with a combined 2.28 ERA. In their games against Texas, they have an 18.00 ERA. After those games, their combined ERA on the season rose to a combined 3.24, almost a full run higher than prior to facing the Rangers.
• Blue Jays pitchers threw 203 pitches in the game, while Rangers pitchers only had to throw 126 pitches in one more inning of work. The most effective pitcher of the night for Toronto was Jeff Mathis. Mathis is a catcher.
• Six different Rangers had multi-hit nights.
• The Rangers raised their MLB leading team batting average from .284 to .288.
• Josh Hamilton hit his MLB leading 19^th home run. Yorvit Torrealba hit his 1^st home run of the year, leaving Alberto Gonzalez as the lone position player on the Rangers without a home run.
• The Rangers run differential is now +90. The next closest team in run differential is St. Louis at +62.

This was a happy game for the Rangers team and its fans. The rest of the series is set up nicely for Texas as well, considering the beleaguered Toronto bullpen, the well-rested Texas bullpen, and the promise of two more sellout crowds for Saturday?s and Sunday?s games.

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