Sentences with phrase «forming ridges»

Ridges forming ridges.

Mullican painted in a style influenced by printmaking, forming ridges of paint and using the edge of a palette knife to achieve a line raised and puckered; the resulting surfaces caught light and cast shadows, ultimately assuming a tapestry - like quality.

Repeat for the remaining dough pieces, setting your finished baguette doughs next to ridge of the most recent baguette dough, and forming another ridge on the other side of the most recent dough.

To form the ridges on the gnocchi, take a bite - sized pillow of dough, and roll it down and off the tines of a fork.

One of the inserts now has formed a ridge from maybe the material bunching up from inside.

Dip a fork in the tapioca starch and press onto the top of the gnocchi pieces to form the ridged indentations.

Alveolar bone forms the ridges in which the teeth are embedded.

And then he goes on to explain that evolutionary anthropologists and psychologists speculate that the large glans forms a ridge all the way around the shaft — a perfect tool to scrape the inside of the vagina of any other man's sperm.

The plastic forms a ridged, crudely lenticular surface, which means that the images change, slanting in and out of view as the angle of sight shifts.

The jet stream has been directed northward and around the high pressure, forming a ridge.

Not exact matches

Set your baguette dough on your couche or floured kitchen towel and form two ridges on either side of the dough with the floured fabric.

This forms the crispy, ridged texture that makes these cookies so distinct.

Having them in a mini tin also helps the ridges form in the chocolate.

I was hunting along a ridge that completely encircled a large gully forming a bowl.

Most knitters learn the knit stitch first, and they are used to seeing the... MORE bumpy ridges of Garter Stitch that are formed by knitting every stitch on every row.

The footplate features diamond ridging for improved grip and is set to a 20 - degree pitch for the best form to target the quads and glutes.

Mid-ocean ridges form at the boundaries between tectonic plates, circling the globe like seams on a baseball.

The ridges form when mantle material melts, rises into the cracks between tectonic plates, and solidifies again.

Scientists aren't sure why the blob formed, though many blame a ridge of high pressure that brought sunnier weather and less mixing of surface water with colder, deeper water.

Troughs and ridges, which are thought to form through very different processes, are not expected to be found lying side by side.

One was the chemistry of basalts, the rock that forms from solidification of magma at the mid-ocean ridge.

The authors analyzed the chemistry of nearly 17,000 basalts formed along mid-ocean ridges around the globe.

The tiny planet cooled quickly, shrinking in size and causing its crust to crumple up and form wrinkly ridges.

«The hypothesis that the floor of the oceans has been spreading seeks to explain some characteristics of ocean basins and the continents by supposing that material welling up from the interior of the earth forms mid-ocean ridges and then, as new material rises, moves outward, away from the ridges.

Three basic forces are believed to drive oceanic plate movement: plates are «pushed» away from mid-ocean ridges as new sea floor forms; plates are «pulled» as the oldest parts of the plate dive back into the earth at subduction zones; and convection within the asthenosphere helps ferry the plates along.

The opening, located in the Afar region of Ethiopia, presents a unique opportunity for geologists to study how mid-ocean ridges form.

The ridge acted as a dam, holding back a lake that had formed in front of a nearby glacier.

Dunes form on Earth when suitable winds scatter sand - sized grains — usually quartz, gypsum or basalt — across the surface, creating ridges that grow to enormous sizes.

Such vents line the midocean ridges, where magma wells up to form new ocean crust.

Eventually the lake overflowed, eroding away large craters in what is now the channel's floor and gradually breaking down the ridge to help form the English Channel we know today.

The researchers were the first to discover that the Pacific Plate is formed by a combination of mechanisms: The plate thickens as the rocks of the mantle cool, the chemical makeup of the rocks that form the plate changes with depth, and the mechanical behavior of the rocks change with depth and their proximity to where the plate is being formed at the mid-ocean ridge.

Oceanic plates form at ocean ridges and disappear into the Earth's mantle, a process known as subduction.

The green layer is the lithospheric plate, which forms at the mid ocean ridge, then cools down and thickness as it moves away from the ridge.

The cooling of the plate overprints a compositional boundary that forms at the ridge by dehydration melting and is preserved as the plate ages.

The seafloor forms along great cracks in Earth's skin called mid-ocean ridges.

For people with this mutation, «the ridges don't even form to begin with, so that's going to interfere with sweat glands,» Reed says.

Also, ridges are not everything — each crease and fold in your hands and feet forms a unique pattern, which forensic scientists can use for identification.

And Francis notes another ridge is currently forming in the North Pacific.

A second study, led by Hailan Wang of NASA's Goddard Space Flight Center, used different model simulations and came to a similar conclusion: While a warming sea surface did make it more likely that a high - pressure ridge could form, the signal was not strong enough to explain its extreme nature.

New crust forms at midocean ridges where the sea floor spreads apart.

The material forms three gently concave faces, separated by three remarkably sharp ridges.

Abyssal hills form at mid-ocean ridges, such as the Mid-Atlantic Ridge (shown).

So Olive and his team devised a new explanation: At fast - spreading ridges with abundant magma eruptions, the cooling, stretching crust forms new faults in rapid succession as it continues to spread.

Retreating Ice Glacier National Park, Montana Most of the ice that carved Glacier National Park's ridges and valleys melted more than 10,000 years ago, but by the time fur trappers ventured into the area in the 1800s, new glaciers had formed.

The material forms three gently concave faces, separated by three remarkably sharp ridges that extend down from the dervish's belt.

Pan orbits Saturn in a gap in the planet's rings and pulls material from them, so the ridge around it likely started accumulating soon after the moon formed, researchers say.

Recent studies have proposed that the bathymetric fabric of the seafloor formed at mid-ocean ridges records rapid (23,000 to 100,000 years) fluctuations in ridge magma supply caused by sealevel changes that modulate melt production in the underlying mantle.

«There were very few [indigenous] people living along the coast then,» says lead author and geologist Daniel Belknap of the University of Maine, and without humans to create the protective covering, newly formed beach ridges simply eroded and vanished.

By mapping and examining the ridges themselves, the team determined that they formed under a specific combination of events.

Before the Spaniards arrived, inhabitants of the arid northern Peruvian coast clad massive sand dune — like ridges with an accidental form of «armor»: millions of discarded mollusk shells, which protected the ridges from erosion for nearly 4700 years and produced a vast corrugated landscape that «is visible from space,» says archaeologist Dan Sandweiss of the University of Maine, Orono, one of the paper's authors.