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123 Sentences With "levels out"

How to use levels out in a sentence? Find typical usage patterns (collocations)/phrases/context for "levels out" and check conjugation/comparative form for "levels out". Mastering all the usages of "levels out" from sentence examples published by news publications.

Skateboarding levels out age differences in the face of skill.
Maybe once that levels out we'll start offering more project baking.
Power of the people However, would taking these levels out affect our health?
I'm a shopaholic, but also a workaholic, so I think it levels out.
"The beauty is that there are levels out there for every taste," he said.
As long as that all kind of levels out, then everybody gets a kind of fulfilling experience.
Their brevity and focus make them the best levels out of any of the Shovel Knight campaigns.
It seems solar power gets cheaper up to the 280 MW to 20 MW range, and then levels out.
Energy is sometimes mistaken for acidity, which levels out sweetness in fruits and is necessary for balance in wines.
And so somebody's got to wrap their arms around this young man and just sit on him until he levels out.
"The Macallan has seen steep growth that levels out," said Isabel Graham-Yooll, auction and private client director at Whiskey Auction.
Buffalo Wild Wings also sees a change after the game, when demand for chicken wings falls slightly, but soon levels out, Freeman said.
Inches before impact, he levels out the machine, its propellers gnashing the grass like a weed whacker, and gently lands it 5 feet away.
In 2015, one man made an entire video game to propose to his girlfriend, building levels out of specific memories of their time together.
In rare cases (most commonly among hardcore athletes), you can drink so much water that it throws your body's sodium levels out of whack.
The Panaray system even levels out satellite radio, dialing back the overly sharp tones and injecting a bit of life into the clinical sound.
When share prices are high, you're able to buy less, but when prices drop, you can buy more, and it all levels out in the end.
But next to it is Jorge's orange and yellow curtain and Rirkrit's curtain that says "The sun is gone but we have the light," it kind of levels out.
"It causes some pause, but if we can be convinced that it levels out some other areas that we're concerned about, then it's not a deal-breaker," he said.
So it goes up into the low reaches of space, and then turns immediately back down and then levels out and flies at a very high level of speed.
They've never played any of these levels before… and they're all made by people known in the Super Mario Maker community for making the most infuriatingly creative levels out there.
On the other hand, fintech levels out the playing field between bigger and smaller firms such as his own, according to certified financial planner George Gagliardi, founder of Coromandel Wealth Management.
Although the DNA did sustain a little damage from the high radiation levels out in space, the offspring still turned out OK. Some were even able to make babies of their own.
But when the party gets raging — when economies accelerate and stock prices ascend to levels out of whack with fundamentals — central bankers play killjoy, lifting interest rates to snuff out attendant dangers.
"With some degree of growth, that actually doesn't take U.S. debt levels out of the sort of comfort zone that governments around the world have achieved in the last few months," he said.
"It's absolutely true to say the Graham-Cassidy bill over time levels out on a per-person basis the way we distribute money on healthcare, which I think resonates with most Americans," Pence said.
"If you effectively at certain points of the day can just draw on a battery that's been stored at some other point, it kind of levels out the curve, which creates less need for generation," said Ferguson.
The one thing I'd like to relate so that people can understand is – grief is a journey and at first the mountains are really steep and the valleys are deep and dark and then it gradually levels out.
It rises in the morning to a little hump before noon, levels out over midday, and then rises to a higher hump in the evening, when everyone gets home from work and turns on their TVs and stoves.
Acronyms abound, many of them without explanation or context, and since the point of view is tightly limited to Kir (who naturally doesn't bother to explain concepts that are second nature to her), the learning curve for this story never quite levels out.
Few people think the pound will rise much further, but if it levels out, it should help tame inflation and ease the strain on consumers, whose spending accounts for about two thirds of economic output, breaking the "stagflationary" spiral of higher inflation and lower growth.
Washington (CNN)Debate over the threat posed by Iran took on a partisan hue after Trump administration officials briefed lawmakers Tuesday, with Democrats charging that the White House is blowing normal threat levels out of proportion and Republicans insisting that deterrence, not war, is the goal.
The game was released as shareware with the trial version containing 10 levels out of 87 of the full version.
The plane then levels out at 9,000 feet. London control can now see them on radar, and proceed to clear a runway. Concorde then makes a beautiful landing. Brody is relieved.
Leaving Denver, I-70 levels out and traverses the wide plains through eastern Colorado. East of Denver, I-70 makes a broad turn to the south-southeast for before reaching Limon and resuming its eastward journey toward Kansas.
However, the private sector only had the ability to provide 2,500 per year, and at price levels out of reach of the low-income population. As many as 51,031 housing units were built between 1960 and 1965 by the HDB.
The summit of High Hartsop Dodd bears a small cairn at the point where the ridge briefly levels out. The view is not extensive given the high ring of surrounding fells, but many of these are seen in close detail, particularly Dove Crag.
The Cherokee Tallassee is sometimes referred to as "Tallassee Old Town." Great Tellico (Talikwa) – located in present-day Monroe County, in Tellico Plains, where the Tellico River levels out at the base of the Unicoi Mountains. Great Tellico rose to prominence in early 18th century under its chief Moytoy.
Burdett's Landing plaqueBurdett's Landing lay adjacent to a bluff formerly known as Mt. Constitution,Adams, Hudson River Guidebook, p. 106 now known as Fort Lee Historic Park. The bluff slopes downward on the south side and levels out sufficiently to make access practical. Burdett's Landing was created here in a small cove.
The tunnel of Philanthus triangulum can be as much as 1 m long. The first part of the tunnel slopes downward at an angle of 30°, after which it levels out. Up to 34 lateral tunnels, each ending in a brood chamber, branch off from the main tunnel. Each brood chamber is stocked with one to six honeybees.
When it reaches a range of 60 to 70 kilometers it levels out at an altitude of between 800 and 1,000 meters where it cruises until it reaches a range of 10 to 16 kilometers, when the missile's active radar homing guidance is engaged. It then enters a dive, striking the target vessel close to or below the waterline.
View of the fjord in eastern Masfjorden Masfjorden municipality lies to the east of the Fensfjorden and Austfjorden. The Masfjorden runs east to west bisecting the municipality. The eastern part has mountains and as one heads westward, the land levels out before reaching the fjord in the east. The municipality lies along the west coast in the central part of the county.
The lowest part has a natural spring and the upper part has a deep, unexplored cave. The Cueva de los Riscos (Cave of the Crags) is named after the crags which appear in various of its chambers. The entrance begins with a rocky descent then levels out to an area with sand. The center has a hillock with looks like a monolith rock.
SR 42 continues near the Cowpasture River past Nimrod Hall to State Route 39 at Millboro Springs. It turns east with SR 39, rising from about 1300 feet (396 m) at Millboro Springs to about 1780 feet (543 m) near Hotchkiss. There the ground levels out, and the combined SR 39 and SR 42 continue east, paralleling Mill Creek into Rockbridge County at Panther Gap.
For example, openness to values decreases substantially with age, while openness to aesthetics is more stable. Neuroticism can be broken into the two facets of anxiety and depression. Anxiety has the same trend as Neuroticism for both males and females. For females, anxiety increases from childhood to adolescence, at emerging adulthood it levels out, and then starts to decrease into and throughout middle age.
Over the course of an individual's lifespan, the stability of their personality has been shown to be variable, although this variability levels out in adulthood. Behavioral genetics can account for the variability experienced across the lifespan. This is highly evident in the transitions between childhood, adolescence, and adulthood. From childhood to mid- adolescence, the rate of individual differences in personality increases, primarily due to environmental influences.
K-181 begins at K-232 (Post Rock Scenic Byway) near the Wilson Lake Dam just west of the Lincoln-Russell county line. The highway begins by traveling to the east through small rolling hills for just over . The roadway then levels out entering rural farmlands and travels roughly before turning north. K-181 continues north, and after crosses West Twin Creek, and then the Saline River.
Briar Creek begins where Knob Mountain, Huntington Mountain, and Lee Mountain meet in western Briar Creek Township. It flows east for a short distance before turning south through a gap in Lee Mountain, briefly descending quite steeply. The course levels out as it leaves the mountain behind and begins flowing through a valley after a short distance. It flows under Pennsylvania Route 93, leaving the valley behind.
The ride then dips to the left and an on-ride photo is taken. The track then levels out and enters a tunnel parallel with the station. Upon entering the tunnel, another set of friction wheels are activated to launch the riders to the faster speed of . The opposite end of the tunnel is covered in mist preventing riders from seeing the approaching track.
Upon exiting the loop, the train climbs a hill, levels out and reaches the first set of trim brakes. Next, the train turns left in a slight decline before leveling out. Once leveled, it enters the diving helix into the ravine. This is achieved by the left rail lowering much more steeply than the right rail as the train descends into a left-turning helix.
West of Sixth Street West, South Hill dips sharply to the southwest. The limits of South Hill are less clearly defined than North Hill. Though the neighborhood levels out past Sixteenth Street South, the name South Hill is generally applied to all areas south up to the city limits. Neighborhoods in the Mouse River Valley include Bel Air, Downtown, Eastwood Park, Oak Park and West Minot.
A picture of Oblivion's drop taken from the guest observation area. The cars accommodate sixteen passengers in two rows of eight with a tiered seating arrangement. The roller coaster has a simple layout with a 180 ft drop at 87 degrees. The car slowly ascends 60 feet at a 45-degree angle to build tension, then levels out and travels a turn towards the drop.
Through the forest, the ground rises sharply, climbing from the plain below to the moors behind. There are several rocky outcrops on the steep slope, including Highcliff Nab and the Hanging Stone. The woods are crossed by several rights of way, including Cleveland Way, but other paths and commission tracks are also open to walkers. Beyond the woods, the ground levels out to form Gisborough Moor.
The difference appears to be in the timing: with Fall one hears a high level tone that then falls, whereas the falling allophone of Low starts falling and then levels out. (That is, one falls on the first mora of the vowel, whereas the other falls on the second mora.) This is unusual because it has been theorized that such timing differences are never phonemic.
Soon the road levels out again as OR 219 descends into the Tualatin Valley. The next named location is Scholls, where the route intersects with OR 210. Keeping on OR 219, one then heads in a general northwesterly direction, running parallel to the western bank of the Tualatin River. Just northwest of the intersection with OR 210 is Brown's Corner, followed by the 90 degree turn at the Midway Curve.
There is a right turn for North Rauceby. The Viking Way joins from the east, and follows the road, where the boundary is between Normanton to the west, and North Rauceby. The road levels out at around a height of 85 metres, and passes Ermine Street Farm to the right. There is a staggered junction and the B6403 finishes at the T-junction at Byard's Leap with the A17.
A wingover (also called a wing-over-wing, crop-duster turn or box-canyon turn) is an aerobatic maneuver in which an airplane makes a steep climb, followed by a vertical flat-turn (the plane turns to its side, without rolling, similar to the way a car turns). The maneuver ends with a short dive as the plane gently levels out, flying in the opposite direction from which the maneuver began.
Northeast of the city is the Coburg Hills. Spencer Butte is a prominent landmark south of the city. Mount Pisgah is southeast of Eugene and includes Mount Pisgah Arboretum and Howard Buford Recreation Area, a Lane County Park. Eugene is surrounded by foothills and forests to the south, east, and west, while to the north the land levels out into the Willamette Valley and consists of mostly farmland.
The road levels out to a parking area on the south side. A U.S. Forest Service sign indicates the Continental Divide and gives the elevation as .. See Video Log at mile 61.13. The Divide also marks the Lake County line. A paved path leads to a scenic overlook with views to Mount Elbert () and La Plata Peak (), respectively the highest and fifth- highest peaks in Colorado and the Rocky Mountains.
The Wallace River flows north through the valley to the Northumberland Strait from its source in Dicks Meadows on Higgins Mountain. The trough descends abruptly north of Folly Lake where over a distance of approximately the valley floor levels out at approximately elevation. From there, the valley floor and the serpentine Wallace River gradually descends over the next to approximately elevation at the junction with the West Branch Wallace River.
Pflanzgarten 1 is made up of a slightly banked, downhill left hander which then suddenly switches back left, then right. Then immediately, giving the driver nearly no time to react (knowledge of this section is key) the road drops away twice: the first jump is only slight, then right after (somewhat like a staircase) the road drops away very sharply which usually causes almost all cars to go airborne at this jump; the drop is so sudden. Then, immediately after the road levels out very shortly after the jump and the car touches the ground again, the road immediately and suddenly goes right very quickly and then right again; this is what makes up the end of the first Pflanzgarten- a very fast multiple apex sequence of right hand corners. Sprunghügel Stefan Bellof S The road then goes slightly uphill and then through another jump; the road suddenly drops away and levels out and at the same time, the road turns through a flat-out left hander.
While less decorative, it follows the same basic form and massing as the Spreckels, with flame finials, and a concentration of Baroque detail at the cornice and side openings. They differ in that the proscenium arch and the side pavilions are simpler in design. The music pavilion is a concrete structure built on a raised stone podium. It is rectangular in shape with a peaked roof which levels out to the north and south walls.
The ride begins with a right-hand turn out of the station, where the train then climbs the 6.5 metre tall lift hill. The train then drops approximately 3 metres to the right, with a downwards left helix following. After exiting the helix, the train makes right-hand turn, before the track levels out on the brake run. The train then makes another right had turn, which goes back into the station.
This lower tunnel, "number two", is a few yards shorter than "number one" and the descent is again about 50 feet. From the exit of this tunnel the line continues down the valley in the original direction, towards Field. The constructions and extra track effectively double the length of the climb and reduce the ruling gradient to 2.2%. The new distance between Field and Wapta Lake, where the track levels out, is .
Originally a separate settlement, Stop-and-Call has now become contiguous with Goodwick. It is at the point where Goodwick Hill levels out after climbing about from the centre of Goodwick.Photograph at Geograph The 1841 Census for the Parish of Llanwnda indicates the presence of three inhabited houses in 'Stop and Call'.'1841 England, Wales & Scotland Census', The National Archives, London, England However, it does not appear on a map which dates from ca. 1850.
Beyond Red Pike to the west are Starling Dodd, Great Borne and the Loweswater Fells. High Crag forms the eastern terminus of the Buttermere Fells, its most arresting feature being the great scree slopes of Gamlin End where the high ground falls away. 700 ft below, the ridge levels out once more and throws up the craggy top of Seat (1,840 ft). A final steep descent then leads to Scarth Gap, a walkers' pass between Buttermere and Ennerdale.
Hunter Mountain chairlift After these turns, it begins a more pronounced climb up the side of the brook valley, heading more to the northeast. This levels out at about when the road reaches Taylor Hollow, the low point between Hunter and East Rusk. An abandoned road continues north down the hollow to private property in the Schoharie Valley below. It is a wide, grassy clearing, and hitching posts are available for horses that wish to take a break.
From the double summit of Heron Pike, a grassy ridge descends south westerly, gradually narrowing until a rougher section falls more steeply at Lord Crag. Beyond here it levels out, curving back a little to the east and passing over a couple of low mounds. The second of these is taken as the summit of Nab Scar. A few hundred yards further on is the scar itself, dropping steeply to the lake with woodland on the lower slopes.
Its first mile remains relatively level as it follows the brook on that side closely, passing the lean-to site on that side and a developed spring. The Mine Hollow Trail's yellow markers fork off to the left from the parking lot. Almost a mile later, the trail crosses another tributary and begins to climb steeply, ascending in the next . After passing another spring below a rock ledge, the trail levels out and reaches the junction.
From Basalt, Highway 82 has climbed . It levels out at Aspen, entering the city's residential West End along West Hallam Street. A block east of Castle Creek, it turns south on North Seventh Street; the intersection's southwest corner has been rounded to smooth the traffic flow, leaving a triangular traffic island in the middle of the road. Two blocks further south, at another intersection with a rounded corner, SH 82 turns east to follow West Main Street across Aspen.
K-152 begins at an intersection with K-7 south of Cadmus and begins traveling east through small rolling hills with rural farmlands and scattered trees. It passes an intersection with Kettle Road then Lamb Road and after roughly reaches an intersection with Long Road. At this point it curves northward for then passes Prairie View High School as it curves back eastward. It continues east and passes through a dip that an unnamed creek runs through then levels out again.
The train begins to climb and level out after reaching the bottom of the ravine, producing significant positive G-forces. After exiting the top of the helix, the train enters a hill followed by a U-turn and a second set of trim brakes as the track levels out. The train then travels down another hill toward the ground and into the final loop. Upon exiting, the train passes through a tunnel and over a hill into another descending U-turn.
It then begins to ascend gently alongside the brook, crossing it one mile (1.6 km) from the summit of Sugarloaf. It then turns north and steepens into a ascent of an unnamed summit. After 0.3 mile (400 m), the trail levels out for about the same distance, then makes a climb to a summit, the highest elevation it reaches in Dutchess County. There is another viewpoint to the north and west similar to that from the north end of Sugarloaf.
From Salt Springs Road, after a short, but rigorous ascent, it levels out and meanders a bit between the top of the gorge and an outcropping of shale (which the Wheatons "mined" for their own use). :Border Trail is a moderate to difficult trail marked with blue blazes. It begins behind the dairy barn, following Silver Creek Trail into the woods. When Silver Creek branches off to the left, the Border Trail continues straight until it reaches the western park border.
K-106 begins at an intersection with K-18 and begins travelling north through small rolling hills covered with a mix of farmlands and grasslands. After about the highway crosses Battle Creek, a tributary of the Solomon River. It continues north to an intersection with Ivy Road, which connects to Rock City, a group of 200 spherical boulders designated as a National Natural Landmark. Here K-106 levels out and transitions to farmlands, as it continues north past an AG by Air airport.
Upon entering the attraction, the queue winds through a narrow rock wall and passing by the tracks. The surrounding walls were originally created from 100 tons of gold ore from Rosamond. Leaving the outdoor station, trains enter a bat-infested tunnel, make a right hand turn, then a left hand turn before climbing the first lift hill, which takes trains through a cavern full of stalactites. Leaving the lift hill, the train drops away to the right, then levels out and makes a left hand turn.
This entire section is considered very scenic and is prone to rockslides in many locations. Around milepost 130, about from Rocky Top, I-75 begins its first major ascent for a few miles before leveling out, and at exit 134, near the community of Caryville, US 25W splits off and I-75 begins a concurrency with SR 63. The Interstate then begins another ascent, this one steeper, adding a truck climbing lane going northbound. About later, the highway levels out once again and the truck lane terminates.
After the viewpoint the dale swings west and levels out with gentle gradients, becoming just a shallow depression as it peters out onto the open pastureland between Castleton and Chapel-en-le-Frith. Cave Dale was initially formed by glacial meltwater carving a deep narrow valley in the local soluble limestone. The river then found a route underground leaving a dry valley with caverns underneath. Later on the caverns below Cave Dale collapsed making the valley even deeper and gorge-like at the northern end.
SR 80 descends from Hayters Gap to the East Fork Wolf Creek. There it turns southwest, following the creek to the community of Hayters Gap, and then following Wolf Creek through a gap in Little Mountain to the North Fork Holston River at the community of River Bridge. It crosses the river and follows Logan Creek uphill to Lindell, where the land levels out. It continues to follow Logan Creek past Yellow Springs and Giesley Mill, then crossing a low summit to Meadow View.
The Wide Field Channel (WFC) was returned to service by STS-125 in May 2009 but the High Resolution Channel (HRC) remains offline. On January 8, 2019, Hubble entered a partial safe mode following suspected hardware problems in its most advanced instrument, the Wide Field Camera 3 instrument. NASA later reported that the cause of the safe mode within the instrument was a detection of voltage levels out of a defined range. On January 15, 2019, NASA said the cause of the failure was a software problem.
A half-mile (800 m) further to the south and 150 feet (50 m) below the foot of the ridge, still surrounded by woods, it flows under Indian Springs Road for its first road crossing. From here it veers to the southeast, crossing under two long dead-end roads in its next mile of woodlands with some cleared areas near the stream. The surrounding terrain levels out. alt=A waterfall in a wooded area against striated grayish rock For its next mile, the Verkeerder Kill returns to its southerly heading through unbroken forest.
Words that have these third morae are referred to as nakadaka ("middle-high"), while words that lack falling-pitch morae are said to be odaka ("tail-high"). # If the word doesn't have an accent, the pitch rises from a low starting point on the first mora or two, and then levels out in the middle of the speaker's range, without ever reaching the high tone of an accented mora. Japanese describe the sound as "flat" ( heiban) or "accentless". Note that accent rules apply to phonological words, which include any following particles.
The western flanks of the fell fall to Buttermere, the village itself standing on Robinson's territory. The top and bottom sections are quite steep but the slope levels out at 1,500 ft to accommodate Buttermere Moss, in Wainwright's words “ a wide marshy depression from which water cannot escape except by being carried away in the boots of pedestrians.” At the head of the lower slope is the subsidiary top of High Snockrigg (1,725 ft), a fine viewpoint for the Buttermere valley. On the south western rim of the Moss is Goat Crag, overlooking Buttermere lake.
The river bed widens significantly and levels out to become very slow moving and turns northward about a half mile, then westward at river mile 8 (river kilometer 13). It meanders westward the rest of the way to the ocean. The sand and stone beach at the river bar is normally very shallow, which allows the tide to change the length of the river as much as a mile. Named tributaries from source to mouth are Grass Creek, School Fork, then Keller, Stump, and Neiglick creeks followed by the North Fork Yachats River.
Development of a thermal equilibrium in a closed system over time through a heat flow that levels out temperature differences Two physical systems are in thermal equilibrium if there is no net flow of thermal energy between them when they are connected by a path permeable to heat. Thermal equilibrium obeys the zeroth law of thermodynamics. A system is said to be in thermal equilibrium with itself if the temperature within the system is spatially uniform and temporally constant. Systems in thermodynamic equilibrium are always in thermal equilibrium, but the converse is not always true.
By measuring the concentrations at different latitudes, Rowland was able to see that CCl3F was mixing between hemispheres quite rapidly. The same measurement was repeated 8 years later and the results showed a steady increase in CCl3F concentrations. Rowland's work also showed how the density of the ozone layer varied by season increasing in November and decreasing until April where it levels out for the summer only to increase in November. Data gained throughout successive years showed that although the pattern was consistent, the overall ozone levels were dropping.
Manual gas control valve Griddles with manual controls require constant attention by an operator to control the temperature of the griddle plate. Without food products to remove the heat from a griddle surface, the unregulated heat source can cause the plate surface temperature to rise continuously until it levels out at temperatures well beyond those normally used for cooking (over ). At these temperatures the griddle plate material may take on a bluish tint as the surface of the carbon steel plate oxidizes. Manual controls are not typically used on electric griddles.
As this limit is approached, very little additional binding occurs and the curve levels out as the hemoglobin becomes saturated with oxygen. Hence the curve has a sigmoidal or S-shape. At pressures above about 60 mmHg, the standard dissociation curve is relatively flat, which means that the oxygen content of the blood does not change significantly even with large increases in the oxygen partial pressure. To get more oxygen to the tissue would require blood transfusions to increase the hemoglobin count (and hence the oxygen-carrying capacity), or supplemental oxygen that would increase the oxygen dissolved in plasma.
The lower 600 m of the climb consist of a narrow asphalt road, the upper 1600 m are paved with cobblestones. The first 500 m of cobbled section are particularly difficult, it is the steepest and narrowest part of the climb with a bad, very uneven cobbled surface. Halfway up the climb, near the church of Kwaremont village, the gradient gradually levels out from 11% to just 2%, but with still a cobbled kilometer to go to the top. The top is situated just after the cobbled section, at 111 m, after a 93 m altitude gain.
The route is the main access road to parts of Auburn, Dryden, Newark Valley and Port Byron. It passes through mountainous terrain in Tioga and Cortland counties, but the terrain levels out as it heads through the Finger Lakes area and Cayuga County. The route intersects several long-distance highways, including NY 13 in Dryden, U.S. Route 20 (US 20) and NY 5 in Auburn, and NY 31 in Port Byron. It passes over the New York State Thruway (Interstate 90 or I-90) north of Port Byron; however, there is no connection between the two.
The bottom cascade is smallest of the three, after which the Beck enters a small wooded gorge containing further smaller falls. The Beck then levels out in the bottom of the Newlands Valley as it is joined by High Hole Beck and becomes Keskadale Beck. Moss Force is a popular stop with visitors and tourists."A Pictorial Guide To The Lakeland Fells - The North Western Fells", Alfred Wainwright, "...one of the few paths in Lakeland owing their existence very largely to motorists exercising their legs from cars left at the Hause, where wide verges provide plenty of space for parking".
Ninety percent of the world's flat glass is produced by the float glass process invented in the 1950s by Sir Alastair Pilkington of Pilkington Glass, in which molten glass is poured onto one end of a molten tin bath. The glass floats on the tin, and levels out as it spreads along the bath, giving a smooth face to both sides. The glass cools and slowly solidifies as it travels over the molten tin and leaves the tin bath in a continuous ribbon. The glass is then annealed by cooling in an oven called a lehr.
Goose Creek rises at Manassas Gap on the Blue Ridge near Linden. The creek initially flows eastward down the mountain, falling in its first . At Delaplane the creek levels out and turns in a northeasterly direction for another 10 miles, whereupon it passes under U.S. Route 50 and enters Loudoun County. Once in Loudoun, the creek continues in a northeastward direction for to the western foot of Catoctin Mountain, where it turns to the north briefly, before reaching the confluence of the North Fork and then turning to the east and cutting through a gap in the mountain.
The roadway has many switchbacks and on both the eastern and western slopes, with White's Gap at the peak. After descending on the eastern side, travelers reach Amherst, where Route 60 intersects north-south U.S. Route 29. View west along US 60 at the bridge over the James River between Appomattox and Nelson counties Continuing east, there is an additional shorter section of mountainous terrain before the road levels out somewhat into the rolling Piedmont region through the middle belt of the state. At Sprouse's Corner in Buckingham County, north-south U.S. Route 15 is crossed.
Once riders are seated and secured, a siren sounds and the train exits the station down a small dip, turning 180 degrees straight into a tunnel decorated as a Pepsi Max pop can. After the brief tunnel, the train climbs the lift hill, which has height markers every showing riders the rising elevation, crossing over Icon's track. After reaching a height of , the train drops after first entering a quarter right turn before rapidly descending a 65-degree drop. As the drop levels out, riders experience up to 3.5G and rise up a large hill with minimal airtime.
Level design focused on providing a large variety of situations, including splitting levels between Puzzle and Action types, to avoid having the player develop a limited toolbox of common words and not exploring other possible solutions. Much of the initial level development was done on paper and to explore situations not commonly found in video games, due to their vocabulary system. They ended up selecting more than a hundred levels out of over seven hundred they had generated internally for the game. Both Merits and Ollars were added to reward the player for completion, with Slaczka comparing these to Xbox Live Achievements.
Wunder von Lengede, illustration (1963) by Helmuth Ellgaard On 7 November 1963, 11 West German miners were rescued from a collapsed mine after surviving for 14 days, an event that later became known as the Wunder von Lengede ("miracle of Lengede"). On 24 October 1963, the Lengede-Broistedt Iron Mine near Salzgitter was flooded with of muddy water after a sedimentation pond had broken its ground and the tunnels between the and levels. Out of 129 workers, 79 escaped during the first few hours. They used underground mine ventilation raises and further shafts which had been provided with ladders due to safety regulations.
Fuchsröhre Adenauer Forst The Fuchsröhre is soon after the very fast downhill section succeeding the Flugplatz. After negotiating a long right hand corner called Aremberg (which is after Schwedenkreuz) the road goes slightly uphill, under a bridge and then it plunges downhill, and the road switches back left and right and finding a point of reference for the racing line is difficult. This whole sequence is flat out and then, the road climbs sharply uphill. The road then turns left and levels out at the same time; this is one of the many jumps of the Nürburgring where the car goes airborne.
The coastline at the edge of Predannack Downs To the south of the village the land gently rises and levels out onto a plateau at a height of around above sea level. In contrast to the northern part of the parish this area remains as semi-natural heath, the growth of which is encouraged by the change in geology south of Mullion Cove to magnesium rich serpentine rock. Known as Predannack Downs, it is part of the Lizard National Nature Reserve. In the centre of the downs lies the World War II, Predannack Airfield, currently a satellite of nearby RNAS Culdrose.
In the southeast corner is the small brick Italian villa-style James Hall Office, a National Historic Landmark now annexed to a former elementary school building. Between it and the city's southern limit at I-787 are residential neighborhoods around Second Avenue, with the open space of school athletic fields and two smaller city parks on either side. To the west of the bluff the land generally levels out again. Across the one-block West Capitol Park from the capitol, on the corner of Washington Avenue (at that point also New York State Route 5 (NY 5)) is another tall state office tower, the Art Deco Alfred E. Smith Building.
The energy recovered by braking the trains is used to spin the flywheel inverter where potential energy is stored and used to launch the trains. Riders start by turning into a dark tunnel with a siren and a loud boom, before shooting straight up the 110 ft vertical launch hill at 40 MPH, cresting, and then descending vertically down the other side of the tower at speeds reaching 55 MPH. Riders then go up and over a small airtime hill with a trim brake, before going up and quickly flipping around an Immelmann turn. The track levels out before sending riders up into a heartline roll.
The next most popular route starts from the southeast, via the Devil's Path at Stony Clove Notch. The red-blazed trail begins steeply, switching back past some impressive shale cliffs known as the Devil's Portal, then following an old barkpeeler's road through an area where the hemlock are beginning to regenerate and red spruce have sprung up as associates. It returns to a more standard trail at the upper limit of the hemlocks and levels out just under , a vertical ascent of about in its first . The next is a pleasant, level stroll through the heavily logged areas now dominated by paper birch and red spruce.
The narrow wood on the scarp of Edge Hill, in the south-east overlooks the lower slope and the plain on which the battle was fought. The battle of Edge Hill was fought on Sunday 23 October 1642 and was the first major battle in the English Civil War between the Royalist forces of King Charles I and the Parliamentarian army commanded by the Earl of Essex. The King's army started the day on the plateau above the scarp and Parliament's front line was about away. From Edge Hill, the ground drops steeply, levels out, then rises to Battleton Holt and a little beyond it are the Oaks and Graveground Copice.
However, these efforts were not successful enough then in convincing the people living in the squatter settlements to move into these flats. It was after 25 May 1961, the day of the Bukit Ho Swee fire, that HDB's efficiency and earnestness won the people over. The HDB estimated that from 1959 to 1969, an average of 147,000 housing units—80,000 from the current deficit, 20,000 due to the redevelopment of the Central Area, and 47,000 due to population increase—would need to be constructed; an average of about 14,000 a year. However, the private sector only had the ability to provide 2500 per year, and at price levels out of reach of the low-income.
The sharply banked side has a concrete surface, and there is a foot-wide tarmac surface on the bottom of the banking for cars to get extra grip through the very rough concrete banking. Cars drop into the concrete banking, and keep the car in the corner (which is 210 degrees, much like a hairpin bend) until the road levels out and the concrete surface becomes tarmac again. This corner is very hard on the driver's wrists and hands because of the prolonged bumpy cornering the driver must do while in the Karrusell. Usually cars come out of the top of the end of the banking to hit the apex that comes right after the end of the Karrusell.
It then goes through a few curves, but maintains a generally eastward direction from here. It forms the northern terminus for various streets in Arlington including Fielder, Davis, and Cooper, at which point it finally becomes Northeast Green Oaks Boulevard. A mile farther east, it crosses Farm to Market Road 157 again, this time being carried on North Collins Street. It then dips to the southeast to meet the northern end of Ballpark Way, which can take traffic to Globe Life Park, then comes back northeast, and levels out due east again, crossing Holly Brook, Arlington's city limit for a final time a few dozen yards past this, then terminating at Texas State Highway 360 again.
Graduated payments are repayment terms involving gradual increases in the payments on a closed-end obligation. A graduated payment loan typically involves negative amortization, and is intended for students in the case of student loans, and homebuyers in the case of real estate, who currently have moderate incomes and anticipate their income will increase over the next 5–10 years. All Federal Housing Administration (FHA) lenders can offer a FHA Graduated payment mortgage loan, which begin with a lower monthly payment that increases annually over the first 5–10 years of the loan, and then it levels out to a fixed monthly payment for the remaining years of the mortgage. There are five FHA Graduated Payment Mortgages offered in 15-year and 30-year terms.
After crossing just below the outlet of Notch Pond, the trail shortly begins to climb and switchback, passing a massive pair of stone outcrops known as the Devil's Portal. Above, the trail follows an old wood road into an area where a few hemlocks remain from tannin-seeking loggers in the late 19th century. Some spruce may be found along here, too. Leaving the old road shortly before it dead-ends, the trail goes through a slightly more level area where hungry hikers can snack on wild blackberries and raspberries in season, then levels out just below , in an area where paper birch, red spruce and fern make up the forest ... a sign of the heavy logging of this area a century ago by the West Virginia-based Fenwick Lumber Company.
A raven turn is a half-inversion which looks like half a loop followed by a drop and then levels out near the same height as it began. The raven turn is only usable on either flying roller coasters or 4D roller coasters at the moment and has only been used on three 4D coasters and one flying coaster. The general term raven turn refers to any inversion that follows the design described above; however, there are two types of raven turns. Assuming the train is going round the half-loop first, an inside raven turn is where the rails are below the train at the start whereas an outside raven turn is one in which the rails are above the train at the start of the element.
Then, the road drops away again very suddenly, which is the second huge jump of the Pflanzgarten known as the Sprunghügel. The road then goes downhill then quickly levels out, then it goes through a flat-out right hander and this starts the Stefan Bellof S (named as such because Bellof crashed a Porsche 956 there during the 1983 Nurburgring 1000 km), which was known as Pflanzgarten 2 prior to 2013. The Stefan Bellof S is very tricky because the road quickly switches back left and right—a car is going so fast through here that it is like walking on a tightrope. It is very difficult to find the racing line here because the curves come up so quickly, so it is hard to find any point of reference.
Mount Osmond is a small suburb of 2,497 people in the South Australian capital city of Adelaide. It is part of the City of Burnside local government area and located in the foothills of the Adelaide Hills, five kilometres south east of the city centre. The suburb is high on the hill of the same name, which is the last hill on the right when approaching Adelaide down the South Eastern Freeway before the road levels out onto the Adelaide Plains. It is bounded to the north by the suburb of Beaumont, to the north-east by Burnside, to the east by Waterfall Gully, to the south by Leawood Gardens/Eagle On The Hill, to the south-west by Urrbrae, to the west by Glen Osmond and to the north-west by St Georges.
In standard Japanese, pitch accent has the following effect on words spoken in isolation: # If the accent is on the first mora, then the pitch starts high, drops suddenly on the second mora, then levels out. The pitch may fall across both morae, or mostly on one or the other (depending on the sequence of sounds)—that is, the first mora may end with a high falling pitch, or the second may begin with a (low) falling pitch, but the first mora will be considered accented regardless. The Japanese describe this as atamadaka (literally, "head-high"). # If the accent is on a mora other than the first or the last, then the pitch has an initial rise from a low starting point, reaches a near-maximum at the accented mora(e), then drops suddenly on any following morae.
Detectable levels of pharmaceuticals and personal care products, in the parts per trillion, are found in many public drinking water systems in the US as many water treatment plants lack the technological know-how to remove these chemical compounds from raw water. There are now increasing worries about how these compounds degrade and react in the environment, during the treatment process, inside our bodies, and the long-term exposure to multiple contaminants at low levels. Out of over 80,000 chemicals registered with the EPA, the US federal drinking water rules mandate testing for only 83 chemicals, which calls for increased monitoring of pharmaceuticals on the presence and concentrations of chemical compounds in rivers, streams, and treated tap water. As traditional waste water regulations and treatment systems target microorganisms and nutrients, there are no federal standards for pharmaceuticals in drinking water or waste water.
A significant gap in research at Gondolin occurred in the 1980s, during which time all of the excavated blocks were processed (but no further in situ or ex situ sampling is known to have occurred). The first description of the result fossil assemblage in 1993 only partially described 4,344 individual specimens that could be assigned to a specific taxonomic levels (out of the 90,663 total specimens recovered from acetic acid processing of the 43 trays/blocks). In 1997 a survey of the sediments at Gondolin included the first sampling of the extensive ex situ dumpsite deposits at the locality via a test trench (Trench A). Materials removed from Trench A included fossiliferous breccia blocks from most, if not all, of the stratigraphic units present at the site (as well as loose fossil specimens sifted from decalcified sediments).
Corte Madera Creek has its origin just northeast of Borel Hill in the Coal Creek Open Space Preserve (part of the Midpeninsula Regional Open Space District, and follows Alpine Road northwesterly along the San Andreas Fault to pick up Coal Creek, Rengstorff Gulch, Damiani Creek, Jones Gulch, Hamms Gulch - all draining the northeastern slope of the Santa Cruz Mountains. It levels out upon reaching Portola Valley and crosses under Portola Road at Brookside Drive. Before reaching Searsville Reservoir it arrives in a large laguna or freshwater marsh formed by the nexus of several creeks, including Westbridge Creek, Sausal Creek, Dennis Martin Creek, and Alambique Creek. Just south of the intersection of Mountain Home Road and Portola Road, Alambique Creek enters a historic wetland pond (Lloyd's Pond) which is currently impounded by the road-fill of Portola Road and a culvert.
Classes are also provided for refugees from the neighbouring countries. Early in 1952, in response to the growing need in Belize for higher levels of academic training, St. John's College expanded its traditional four-year high school program, offering a limited number of post- secondary school courses under the direction of Fr. Robert Raszkowski, S.J. This expanded into what in the British tradition is called Sixth Form, a two- year program leading to Advanced Level Examinations ("A-Levels") out of Cambridge University in England. In the mid-1960s, in an effort to provide wider opportunities for further education to graduates of the Sixth Form, St. John's College broadened the program of studies so that it met the requirements of the associate degree awarded by junior and community colleges in the United States. It received membership in the American Association of Community and Junior Colleges.
So the sequence "hashi" spoken in isolation can be accented in two ways, either háshi (accent on the first syllable, meaning 'chopsticks') or hashí (flat or accent on the second syllable, meaning either 'edge' or 'bridge'), while "hashi" plus the subject-marker "ga" can be accented on the first syllable or the second, or be flat/accentless: háshiga 'chopsticks', hashíga 'bridge', or hashigá 'edge'. In poetry, a word such as omoshirói, which has the accent on the fourth mora ro, is pronounced in five beats (morae). When initial in the phrase (and therefore starting out with a low pitch), the pitch typically rises on the o, levels out at mid range on the moshi, peaks on the ro, and then drops suddenly on the i, producing a falling tone on the roi. In all cases but final accent, there is a general declination (gradual decline) of pitch across the phrase.
The creek is then blocked to the northwest by a ridge of the Santa Ana Mountains running northeast to a steep 1577 foot summit overlooking the deep canyon between it and Estelle Mountain. This ridge divides the Temescal Valley below from the upper valley of Temescal creek. Descending through this unnamed canyon, the creek makes a half circle around the ridge to the north of Lee Lake to enter the Temescal Valley. The creek levels out after leaving the Estelle Mountain canyon, passing through a natural riverbed, the creek receives Mayhew Canyon Wash from the left, Dawson Canyon Wash from the right, Coldwater Canyon Creek and the waters of Brown Canyon Wash and its tributary of McBribe Canyon Creek from the left, Olsen Canyon Wash and Cajalco Creek from the right and Bedford Canyon Wash and Joseph Canyon from the left before entering Temescal Canyon.
Adobe Creek Purisima Creek at the bottom of the Packard Pathway at Elena Road, Los Altos Hills Purisima Creek consists of two minor forks (a north and west fork) which embrace the apricot orchards now owned by the David and Lucile Packard Foundation. The creek's source is at the top of the west fork between Dezahara Way and Altamont Road. The "Packard Pathway" is a public walking and riding path that descends the north fork from its origin below the Packards' Taafe House on Taafe Road. At the base of the property the two forks come together to form the creek mainstem which levels out as it passes through the remains of an old walnut grove, then crosses Elena Road, flowing along Josefa Lane and the northwestern edge of Foothill College to where it passes under I-280, then along O'Keefe Lane and the O'Keefe Open Space Preserve to its confluence with Adobe Creek just inside Los Altos.
The circuit has three layouts, the 1.3 miles International layout with 9 corners, the 1 mile National layout with 10 corners and the 0.5 mile tri-oval On all layouts the circuit is 10 metres wide and has a total elevation change of 37 metres. A Porsche at the top of Duffus Dip A lap of Knockhill, beginning at the start line (which unusually for a motor racing circuit is at a different point to the finish line. Whilst the start line is roughly in the middle of the pit straight, the finish line is situated slightly to the west, towards the final corner), first involves passing over the crest which marks the highest point of the circuit. The circuit then levels out and passes under the pedestrian bridge before a short braking zone preceding the first of the nine corners, Duffus Dip, a fast, blind apexed downhill right hand corner widely regarded as one of the most challenging corners in the United Kingdom.
SR 107 then levels out and passes through Houston Valley before entering South Greene and becoming concurrent with SR 70. They then turn northwest and have an intersection with SR 351 and SR-107 Cutoff. The highway then leaves South Greene and crosses over the Nolichucky River just yards from the historic Nolichucky Dam and Davy Crockett Lake. SR 70/SR 107 then continue north into Greeneville where they come to an intersection with US 321/SR 35, where SR 107 leaves SR 70 to become concurrent with US 321/SR 35 to enter downtown. They then have a short concurrency with SR 350 before becoming concurrent US 11E Bus. They continue north through downtown before US 321/SR 35 splits off and goes north while US 11E Bus/SR 107 continue through town before coming to an intersection with US 11E/US 321/SR 34, where US 11E Bus ends and SR 107 becomes concurrent with that highway as they enter the neighboring town of Tusculum.
Bartenev, G. M., Structure and Mechanical Properties of Inorganic Glasses (Wolters – Noordhoof, 1970) This concept leads to defining the glass transition in terms of the vanishing or significant lowering of the low- frequency shear modulus, as shown quantitatively in the work of Zaccone and Terentjev on the example of polymer glass. In fact, the shoving model stipulates that the activation energy of the relaxation time is proportional to the high-frequency plateau shear modulus, a quantity that increases upon cooling thus explaining the ubiquitous non-Arrhenius temperature dependence of the relaxation time in glass-forming liquids. The velocities of longitudinal acoustic phonons in condensed matter are directly responsible for the thermal conductivity that levels out temperature differentials between compressed and expanded volume elements. Kittel proposed that the behavior of glasses is interpreted in terms of an approximately constant "mean free path" for lattice phonons, and that the value of the mean free path is of the order of magnitude of the scale of disorder in the molecular structure of a liquid or solid.
Hikers typically park at the trailhead lot, in elevation, where Ulster County Route 47 bends sharply about three-quarters of a mile (1.3 km) north of Winnisook Lake, midway up or down the hill between it and Big Indian Hollow. Here the P-EB leaves the road again and leads southeast uphill 0.7 mile (1.1 km) and 500 vertical feet (150 m) to the GP in the level area between the ledge and Slide's north ridge. The former route of the P-EB, now closed, leads downhill to the southwest to its former route across the Winnisook Club. Turning north on the GP, the trail remains level, passing an official campsite and some muddy spots until it reaches the base of Giant Ledge 0.6 mile (1 km) later, where a good, reliable spring can be found via a short side trail. A climb of 0.15 mile (240 m) up the steep, rocky south slope of the ledge, sometimes assisted by rock steps, levels out at 3,200 feet (975 m), where the trail stays close to the east side.

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