In the same gallery, Eric Aho's Ice Cut turns a hole in a thick
sheet of ice into a forceful void, and Yvonne Jacquette's birdseye view of a cove in Maine delineates the tide into a rhythmic composition of bending, parallel blue lines.
Once I accidentally stepped through
a sheet of ice into water while wearing them.
Not exact matches
In» The Inferno,» Dante tells
of his imagined journey
into hell, his entry
into a» kingdom
of eternal night» where he hears the voices
of the damned rise» in a bestial moan» and sees sinners stung by wasps, burnt by falling fire and frozen in a
sheet of ice.
Further, the less time an
ice sheet has to create new layers
of ice each winter, the less strong
ice is created and built
into centuries
of previous strong sea
ice, leaving ever more vulnerable and easy - to - melt sea
ice.
-- On a lower speed, add eggs one at a time and vanilla until well incorporated — Increase mixing speed to high and let it go for 10 minutes — the mixture will become really pale and will almost double in size — In a medium sized bowl, whisk together flour, baking powder, baking soda, and salt — When 10 minutes are up, add flour mixture slowly until just combined, about 45 - 60 seconds — Chop up and mix together all
of your baking and snack ingredients in a small bowl, and fold
into batter with a spatula until just incorporated — Using a medium - sized
ice cream scoop, portion cookie dough on parchment paper - lined cookie
sheet and wrap the entire thing tightly with plastic wrap — Refrigerate for a minimum
of 1 hour and up to 1 week — Heat oven to 400F and arrange cookies on cookie
sheets at least 4 ″ apart — Bake 9 - 11 minutes, until they are golden in color and slightly brown along the edges — Cool the cookies completely on the
sheet pan (or just eat them immediately...)
Using two spoons or a small
ice cream scoop, form the dough
into balls the size
of walnuts and place them on the cookie
sheet about 2 inches apart.
You can either eat the dough raw, freeze in bite - sized chunks and put
into a freezer bag to store for your next batch
of ice cream, or bake it on a lined cookie
sheet at 350 degrees for about 11 minutes.
Transfer to a container with an airtight lid, press a
sheet of plastic wrap right
into the top
of the
ice cream and freeze for several hours.
1) Mix flour, butter and
icing sugar in a bowl using two knives to cut the butter until the mixture resembles fine breadcrumbs 2) Add in the egg yolks and vanilla extracts and mix well, then add
iced water until the dough starts to come together 3) Shape the dough
into a ball on a cool, flat, floured surface 4) Flatten dough
into a disc and then wrap in plastic wrap, and chill in the refrigerator for at least 30 minutes 5) Meanwhile, peel, core and slice the apples
into as thin slices as possible 6) Mix sugar and ground cinnamon powder with sliced apples and let it rest for a while 7) Pre-heat oven to 180 deg cel 8) Once dough has chilled, roll pastry dough on a
sheet of parchment paper until it has expanded to the size
of the tart mold (I used a rough mold the size
of a large pizza) 9) Leaving at least an inch
of dough free, arrange apple slices by overlapping them slightly in the shape
of a circle, starting from the outermost part
of the circle, until you reach the inside 10) Fold the edges
of dough over the filling and then sprinkle the dough with a bit
of sugar 11) Bake for about 40 - 45 minutes, or until the crust is golden brown and the apples are soft 12) Serve warm, with a side
of whipped cream or
ice cream (optional)
after 20 minutes (or so) I checked up on it and realized it had dried up; so I took it out
of the oven scooped them
into the baking
sheet with an
ice cream scooper and they held their shape.
Things I changed: - cut the sugar by about half, using mostly dark brown sugar for the molasses kick - scratched the nutmeg and allspice but added about 1/3 extra
of all
of the other spices and also added nearly a tsp
of ground cardamon - replaced the veggie oil with melted leaf lard - scratched the raisins - baked it on a deep
sheet for only ~ 20 minutes - just barely until firm to the touch - then cut that
sheet into three layers - replaced the
icing with my own 16 ounce cream cheese, 8 ounce butter, ~ 6 ounce heavy cream, ~ 5 ounce honey, 1 tsp vanilla combo - toasted the coconut before dressing the cake.
ice cream scoop, portion out 10 balls
of dough and place on a parchment - lined baking
sheet, spacing about 3» apart (you can also form dough
into ping pong — sized balls with your hands).
While most duck shooters snuggle deeper under the blankets, the Maine seabirder gets up at 4 a.m., drives his boat through swells that wash over the decks and turn them
into sheets of ice, sets his trawl line
of decoys, anchors in the lee
of a ledge and covers his boat with rockweed.
After receiving a pass from Messi, Neymar dribbled
into the box and made City defender John Stones look as if he was trying to walk on a
sheet of ice.
How to get
into curling - an intricate, tactical back - and - forth game on a
sheet of ice, accessible to all ages.
The plume has been a factor in the
ice sheet's behavior throughout its history, and recent surges in melting are the result
of all the additional heat humans have pumped
into it.
Almost exactly a year ago, a 251 - square - kilometer
sheet of ice broke from the Petermann Glacier in Greenland and started slowly drifting
into the open ocean.
A team drills thousands
of feet
into the West Antarctic
Ice Sheet to reach a lake buried for millennia.
The icebergs that find their way
into the paths
of transatlantic liners come down from the coast
of Greenland; for the interior
of Greenland is a huge
ice sheet fringed by mountains and promontories.
Studying surging glaciers could also offer insights
into grander - scale
ice flows with global consequences: the movements
of the
ice sheets in Antarctica and Greenland, which can change abruptly, altering the
ice discharges that affect sea level.
Evidence
of past glacial advance and retreat is also more easily observed in the Dry Valleys, providing a window
into the past behavior
of the vast Antarctic
ice sheets and their influence on global sea levels.
Today's red deer, which recolonized Europe after the
ice sheet melted about 12,000 years ago, fall
into three or four distinct lineages that likely correspond to separate southern regions to which the deer had retreated during the height
of the
ice age, Stanton says.
The
ice sheet is made up
of snow that falls and never melts, but rather remains year after year and is gradually compressed
into ice.
The shelves act as a buttress to the «grounded»
ice, helping slow the flow
of the
ice sheet's glaciers
into the ocean.
Perhaps extra carbon dioxide from a period
of heightened seafloor eruptions eventually percolates through the ocean and
into the atmosphere, allowing warming that would deliver a coup de grâce to the massive
ice sheets.
The Antarctic
ice sheet, the thick layer
of ice covering much
of the continent, is anchored in place by its floating fringe, shelves
of ice that jut out
into the surrounding ocean.
The scientists looked
into the hypothesis that soot from forest fires in China, Siberia and North America could be driving the increased darkening
of the
ice sheet.
Materials scientists hope their computer model results will spark further research
into the effects
of carbon dioxide on fracturing in glaciers and
ice sheets
Many
of the glaciers that jut out
into the ocean are thinning, but whether the
ice sheet itself has remained stable and intact, even during warm interglacial periods, is a matter
of considerable debate.
The team stresses that even a little warming could cause irreversible melting
of ice sheets and turn dense Amazon forests
into dry savannah grassland.
What they found, Hansen says, is that melting
ice sheets in Greenland and Antarctica could inject enough fresh water
into the seas to slow the formation
of two key water masses: the North Atlantic Deepwater and the Antarctic Bottom Water formations.
• In Antarctica, Greenland and other places where big
ice sheets are surrounded by the ocean, sometimes big chunks
of ice fall
into the ocean after they have started to melt.
«Very old
ice probably exists in small isolated patches at the base
of the
ice sheet that have not yet been identified, but in many places it has probably melted and flowed out
into the ocean.»
By contrast, during the last
ice age, hundreds of comparatively smaller icebergs broke free of the Antarctic Ice Sheet and drifted into Pine Island B
ice age, hundreds
of comparatively smaller icebergs broke free
of the Antarctic
Ice Sheet and drifted into Pine Island B
Ice Sheet and drifted
into Pine Island Bay.
The Ross
Ice Shelf, a thick, floating tongue of solid ice the size of Spain, is the biggest of the many such barriers that ring Antarctica and keep its ice sheets from sliding into the s
Ice Shelf, a thick, floating tongue
of solid
ice the size of Spain, is the biggest of the many such barriers that ring Antarctica and keep its ice sheets from sliding into the s
ice the size
of Spain, is the biggest
of the many such barriers that ring Antarctica and keep its
ice sheets from sliding into the s
ice sheets from sliding
into the sea.
The 30 or so bits
of bone, none more than 7 centimeters long, have suffered much since they were entombed:
Ice sheets have scoured Ellesmere Island several times in the past few million years, and today's freeze - thaw cycles continue to splinter fossils
into ever - smaller fragments, Rybczynski says.
The Survey's current research programmes look
into the Antarctic
ice sheet, Antarctic climate processes, Antarctic biodiversity and management
of ecosystems, and the past tectonic forces that led to the formation
of today's Antarctic.
With light sensors sunk kilometers deep
into the
ice sheet, IceCube's detector is so huge that it could pick up traces
of a million neutrinos from a Milky Way supernova.
When parts
of the
ice melt, liquid water trickles to the base and this can lubricate the underside
of the
ice sheet, allowing it to slide more quickly
into the sea and drive up sea levels at a faster rate.
Although CryoSat - 2 is designed to measure changes in the
ice sheet elevation, these can be translated
into horizontal motion at the grounding line using knowledge
of the glacier and sea floor geometry and the Archimedes principle
of buoyancy — which relates the thickness
of floating
ice to the height
of its surface.
The slipperiness, caused by films
of water spread over large areas, helps ascertain how quickly a melting
ice sheet will slide
into the sea as the climate warms — and thus how quickly sea levels will rise.
Greenland's
ice sheet melts and sends large amounts
of fresh water
into the coastal waters, where it is
of major importance for local production but potentially also for global ocean currents.
In the mid-1990s, a lake containing 1,300 cubic miles
of water (as much as Lake Michigan) was detected 12,000 feet below the surface
of the
ice in East Antarctica, beneath where the Russians had spent years drilling
into the
ice sheet to study its history.
A new study has found that the massive Laurentide
ice sheet that covered Canada during the last
ice age initially began shrinking through calving
of icebergs, and then abruptly shifted
into a new regime where melting on the continent took precedence, ultimately leading to the
sheet's demise.
Then, as they moved
into coastal North America after
ice sheets there began retreating around 16,000 years ago, they could have continued to dine on a wealth
of coastal foods.
Not only is Greenland's melting
ice sheet adding huge amounts
of water to the oceans, it could also be unleashing 400,000 metric tons
of phosphorus every year — as much as the mighty Mississippi River releases
into the Gulf
of Mexico, according to a new study.
As climate change warms Greenland and more
ice melts and makes its way
into the sea, the
ice sheet is potentially becoming a more important source
of nutrients, he said.
«The sea
ice cap, which used to be a solid
sheet of ice, now is fragmented
into smaller floes that are more exposed to warm ocean waters.
Hawkings and his collaborators spent three months in 2012 and 2013 gathering water samples and measuring the flow
of water from the 600 - square - kilometer (230 - square - mile) Leverett Glacier and the smaller, 36 - square - kilometer (14 - square - mile) Kiattuut Sermiat Glacier in Greenland as part
of a Natural Environment Research Council - funded project to understand how much phosphorus, in various forms, was escaping from the
ice sheet over time and draining
into the sea.
Surprise find The team's actual mission was to survey ocean currents near the Ross
Ice Shelf, a slab of ice extending more than 600 miles (970 kilometers) northward from the grounding zone of the West Antarctic Ice Sheet into the Ross Sea, to model the behavior of a drill string, a length of pipe extending to the seafloor which delivers drilling fluids and retrieves sediment sampl
Ice Shelf, a slab
of ice extending more than 600 miles (970 kilometers) northward from the grounding zone of the West Antarctic Ice Sheet into the Ross Sea, to model the behavior of a drill string, a length of pipe extending to the seafloor which delivers drilling fluids and retrieves sediment sampl
ice extending more than 600 miles (970 kilometers) northward from the grounding zone
of the West Antarctic
Ice Sheet into the Ross Sea, to model the behavior of a drill string, a length of pipe extending to the seafloor which delivers drilling fluids and retrieves sediment sampl
Ice Sheet into the Ross Sea, to model the behavior
of a drill string, a length
of pipe extending to the seafloor which delivers drilling fluids and retrieves sediment samples.