Sentences with phrase «far as the crust»

As far as the crust, I suggest chopping the pecans into finer pieces.

As far as the crust goes, I'll include my very favorite below, the one I use most often - it makes enough for one 9 or 10 - inch double - crust pie.

Not exact matches

Further, the color of the crust wasn't as defined, uniform, or intense as we'd like.

For as far I know this specific product is only available in the Netherlands at the Albert Heijn supermarkets, but I'm sure there are more beet pizza crusts around the world so keep reading for a yummy recipes, you'll love it!

As far as repurposing, every kind of crumbs can be turned into something yummy: some of my favourites are crumb crusts for pie, crusty breading for fish or chicken, British steamed sweet puddings using breadcrumbs (wonderful with custard sauceAs far as repurposing, every kind of crumbs can be turned into something yummy: some of my favourites are crumb crusts for pie, crusty breading for fish or chicken, British steamed sweet puddings using breadcrumbs (wonderful with custard sauceas repurposing, every kind of crumbs can be turned into something yummy: some of my favourites are crumb crusts for pie, crusty breading for fish or chicken, British steamed sweet puddings using breadcrumbs (wonderful with custard sauce!)

As far as shrinkage, my baking instructor said to make sure the crust was pressed very firmly into the sides of the pan, that it wasn't pulled too tight, and that it was cold when it went into the oveAs far as shrinkage, my baking instructor said to make sure the crust was pressed very firmly into the sides of the pan, that it wasn't pulled too tight, and that it was cold when it went into the oveas shrinkage, my baking instructor said to make sure the crust was pressed very firmly into the sides of the pan, that it wasn't pulled too tight, and that it was cold when it went into the oven.

As far as crispy panko crusted things to put on pizza go, I could think of nothing better than eggplanAs far as crispy panko crusted things to put on pizza go, I could think of nothing better than eggplanas crispy panko crusted things to put on pizza go, I could think of nothing better than eggplant.

Press the crust as far up the sides as you can to hold in the filling.

As far as the texture of the pizza, the crust is crunchy and the cheese is creamy giving it that drool - worthy pizza factoAs far as the texture of the pizza, the crust is crunchy and the cheese is creamy giving it that drool - worthy pizza factoas the texture of the pizza, the crust is crunchy and the cheese is creamy giving it that drool - worthy pizza factor.

It was both flaky and easy - the two most essential qualities of a pastry crust as far as Im concerned.

As far as pie crust, I would cut the edges off to form a square from a circle and lay it dowAs far as pie crust, I would cut the edges off to form a square from a circle and lay it dowas pie crust, I would cut the edges off to form a square from a circle and lay it down.

So, I have made this pumpkin cheesecake dip many times before, but I decided to take it a step further and make it a fancy little 2 - bite dessert, using cute little toasted Eggo mini-waffles as a crust.

As far as I'm concerned, an authentic gluten free pizza crust recipe is more than just a way to eat bread and cheese (I know, cue the violinsAs far as I'm concerned, an authentic gluten free pizza crust recipe is more than just a way to eat bread and cheese (I know, cue the violinsas I'm concerned, an authentic gluten free pizza crust recipe is more than just a way to eat bread and cheese (I know, cue the violins).

As far as grain - free crusts go, I think this one is pretty awesomAs far as grain - free crusts go, I think this one is pretty awesomas grain - free crusts go, I think this one is pretty awesome.

The density of the crust makes this so satiating, and as far as figuring and mixing goes, this is a fairly easy gluten - free maneuver for delicious pizza.

Make the crust as far in advance as you like, then roll it out, wrap up the cheese and bake.

A team of Soviet scientists began drilling at Kola in the spring of 1970, with the goal of penetrating as far into Earth's crust as their technology would allow.

Today, there is a number of detectors placed approximately a couple of kilometres below Earth's surface, and there is a very specific reason for their placement so far below ground: if dark matter interacts weakly with ordinary matter (as also the neutrinos do), only these two species can penetrate kilometres of Earth's crust without being stopped.

A high - magnitude earthquake in Japan, one notion goes, might redistribute stress in Earth's crust, subsequently triggering another temblor in the following months or years — a quake that could even strike as far away as the western shores of the U.S..

It also would be far easier to get a water sample from Enceladus, which has plumes of water vapor, ice and particles shooting more than 300 miles off its surface, than from other moons, such as Jupiter's Europa, where a massive ocean is believed to be buried beneath a thick icy crust.

Dr. Lovelock, who in 1972 conceived of Earth's crust, climate and veneer of life as a unified self - sustaining entity, Gaia, foresees humanity in full pole - bound retreat within a century as areas around the tropics roast — a scenario far outside even the worst - case projections of climate scientists.

As far as this historic period is concerned, the reconstruction of past temperatures based on deep boreholes in deep permafrost is one of the best past temperature proxies we have (for the global regions with permafrost — polar regions and mountainous regions)-- as a signal of average temperatures it's even more accurate than historic direct measurements of the air temperature, since the earth's upper crust acts as a near perfect conservator of past temperatures — given that no water circulation takes place, which is precisely the case in permafrost where by definition the water is frozeAs far as this historic period is concerned, the reconstruction of past temperatures based on deep boreholes in deep permafrost is one of the best past temperature proxies we have (for the global regions with permafrost — polar regions and mountainous regions)-- as a signal of average temperatures it's even more accurate than historic direct measurements of the air temperature, since the earth's upper crust acts as a near perfect conservator of past temperatures — given that no water circulation takes place, which is precisely the case in permafrost where by definition the water is frozeas this historic period is concerned, the reconstruction of past temperatures based on deep boreholes in deep permafrost is one of the best past temperature proxies we have (for the global regions with permafrost — polar regions and mountainous regions)-- as a signal of average temperatures it's even more accurate than historic direct measurements of the air temperature, since the earth's upper crust acts as a near perfect conservator of past temperatures — given that no water circulation takes place, which is precisely the case in permafrost where by definition the water is frozeas a signal of average temperatures it's even more accurate than historic direct measurements of the air temperature, since the earth's upper crust acts as a near perfect conservator of past temperatures — given that no water circulation takes place, which is precisely the case in permafrost where by definition the water is frozeas a near perfect conservator of past temperatures — given that no water circulation takes place, which is precisely the case in permafrost where by definition the water is frozen.

The Earth's crust is responding to rising temperatures: volcanoes previously imprisoned below ice sheets are more likely to erupt; earthquakes in the Himalayas, the Andes and Alaska may be triggered as the ice load shrinks; and, the solid Earth beneath Greenland is bouncing back quickly as the ice above it melts, perhaps with the Antarctic land mass not far behind.

Similarly, iron which is far more abundant in the crust, thermodynamically and kinetically prefers to exist as ferric (Fe111) in our oxidising atmosphere unlike its ferrous form in the crust eg pyrite.