「lava」の共起表現一覧(1語右で並び替え)
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spots on Earth, which began to produce basaltic | lava about 145 million years ago. |
Cabana & J-Rod teamed up to defeat Hot Like | Lava afterwards. |
The pores and chambers of the | lava allow seawater to seep into the pools, where it |
a few remnants of the ring poke up through the | lava, although low ridges in the lava seem to trace |
The black or dark brown | lava and ash erupted begins to turn white within a f |
the Odeon Cinema, The Spon Gate (Wetherspoons), | Lava and Ignite (closed 27th April 2010), Jumpin Jak |
1, Tonga's chief geologist Kelepi Mafi reported | lava and ash from two vents, one on the uninhabited |
ly (?!) -- we decided to fight fire with molten | lava and turned every amp we owned on to 10+ and lea |
astic rocks are formed by explosive eruption of | lava and any rocks which are entrained within the er |
g of a log house on a foundation or basement of | lava and basaltic rock. |
by ejecta from the Mare Imbrium or by basaltic | lava, and is relatively smooth and featureless. |
ideromelane indicates higher temperature of the | lava, and solidifying of the flow closer to the vent |
s are generally composed of highly-fluid basalt | lava, and can extend for tens or even hundreds of mi |
Moltres traps Mudkip on an island in a river of | lava and asks Ginji if he would abandon his friend l |
Patidars in Charotar came to claim descent from | Lava and Kusa, legendary suns of the god Rama, this |
n found only at Mt Vesuvius, where they encrust | lava, and in Cornwall. |
ely four million years ago with the eruption of | lava and ash, such as plagioclase-hypersthene-hornbl |
form cinder cones of intermingled ash, tuff and | lava, and may have viscosity similar to thick, cold |
cupressoid ash, 3 crater, 4 water, 5 layers of | lava and ash, 6 stratum, 7 magma conduit, 8 magma ch |
volcano, built up of trachyte and sheathed with | lava, and has the shape of a double cone, whose base |
f Sita's banishment to forests and the birth of | Lava and Kusa to Sita in the forest. |
This temperature is so low that the molten | lava appears black in sunlight, rather than having t |
Spatter forms when blobs of | lava are emitted from a vent. |
K/Ar dates on the | lava are ~ 70 ka, but are considered unreliable beca |
eak is that he no longer needs to take baths in | lava, as he was once so fond of, in order to soothe |
is a species of aster known by the common name | lava aster. |
Carbonatite | lava at Ol Doinyo Lengai volcano, Tanzania. |
e king of Kosala Raghava Rama installed his son | Lava at Sravasti and Kusha at Kushavati. |
dong lies 20 km east of Kalimpong on the way to | Lava at an altitude of 1,240 metres (4.071 feet). |
Doublewide - Top Dog, | Lava, Atlantic 2000 |
LAVA batteries and flashlights have been sold in Dub | |
yed high school football for Bend High School's | Lava Bears. |
w park at Upper Soda Springs, the Trinity Alps, | Lava Beds National Monument, Clair Engle Lake, Castl |
The | lava beds made an outstanding stronghold for the Mod |
This plant is common in the | lava beds of Northwest British Columbia where it is |
s is a reproduction of Canby's Cross located in | Lava Beds National Monument Writing: Gen Canby USA w |
Canby's Cross is located in | Lava Beds National Monument, about 3 miles south of |
hern California including Lassen National Park, | Lava Beds National Monument, and Modoc National Wild |
He was engaged in the attack at the | Lava Beds on April 15, 1873. |
is home to 806 people and the Nisga'a Memorial | Lava Beds Provincial Park. |
this time he served in the Modoc War during the | Lava Beds campaign. |
oday's highway follows the wagon route over the | lava beds past the observatory site. |
ates Army during the Modoc War (also called the | Lava Beds War). |
amed for Modoc chief Captain Jack, is a part of | Lava Beds National Monument. |
Lava Beds) was a battle during the Modoc War between | |
ed position at Captain Jack's Stronghold in the | Lava Beds, but failed to capture the band. |
l that the plot was set during a meeting at the | Lava Beds, but he disregarded her advice, and was ki |
andy and clay substrates, serpentine soils, and | lava beds. |
U. S. Army had 400 troops in the field near the | Lava Beds. |
Captain Jack who was moving southeast from the | Lava Beds. |
ummit, the wagon road had to be cut through the | lava beds. |
kshops in order to free him and has to cool the | lava before lowering him. |
Mafic | lava, before cooling, has a low viscosity, in compar |
and is incinerated when she lands in the molten | lava below. |
A large | lava bench collapsed into the ocean on August 13, wh |
This occurs when the thick, nearly solid | lava breaks up into blocks and these blocks are then |
destroyed and a child's mother is killed by the | lava, but Loana saves the child from a similar fate. |
In September 1914, | Lava Butte "erupted" when the Bend Chamber of Commer |
The early history of | Lava Butte is not known, but it is assumed that Nati |
ecognized the fissure system which extends from | Lava Butte to East Lake within Newberry Caldera. |
rest Service created the 8,983 acres (3,635 ha) | Lava Butte Geological Area to protect the cinder con |
From the top of | Lava Butte, you can easily see the black lava flow l |
the upcoming Moon landings, at sites including | Lava Butte, Lava River Cave, and Newberry Crater. |
sed are chocolate fondant pudding and chocolate | lava cake. |
The | lava can easily be seen in satellite photographs, an |
ument was created encompassing Newberry Crater, | Lava Cast Forest Geological Area, Lava River Cave, a |
verns, which becomes even more dangerous as the | lava chamber they are in is full of fire and falling |
Though | Lava chose not to release the album, they would not |
They commonly display steep | lava cliffs from their interaction with glacial ice |
OpenG, as well as | LAVA Code Repository (LAVAcr), serve as repositories |
Lava Cola uses kava produced on the island of Maewo, | |
Lava Cola has been described as an "anti-energy beve | |
Lava Cola -officially Lava Cola - Vanuatu Kava Cola- | |
g that, while kava itself is an acquired taste, | Lava Cola may well be suitable for export. |
Thereafter eruptions of | lava continued and produced the current 72 peaks. |
Magma that reaches the surface to become | lava cools rapidly resulting in rocks with small cry |
Eventually, the | lava cover was mantled by thousands feet of sediment |
flooded portions of India with a vast amount of | lava, creating a plateau known as the Deccan Traps. |
Lava Creek | |
Extent of | Lava Creek ash bed. |
The | Lava Creek Tuff distributed in a radial pattern arou |
Tuff Cliff showing the | Lava Creek Tuff formation. |
Lava Creek Tuff ranges in color from light-gray to p | |
Lava Creek Tuff is a tuff formation, in Wyoming, cre | |
ed due to the geohazard posed by The Barrier, a | lava dam holding back Garibaldi Lake that has let go |
A | lava dam created a broad shallow lake in the area of |
spect Dam is the term used to describe a former | lava dam in the Grand Canyon of Arizona, United Stat |
One | lava dam a few miles downstream from the present Ame |
There are two main types: | lava dams and pyroclastic dams. |
Lava dams are formed by huge lava flows during numer | |
It was the oldest and tallest of several former | lava dams in the Grand Canyon. |
l ice, instead forming hyaloclastite and pillow | lava deep beneath the glacial ice field. |
Rumex skottsbergii, or more commonly known as | Lava Dock, is a shrub of the genus Rumex. |
Lava dome growth has produced block-and-ash flows th | |
o occur due to the disruption of the crust of a | lava dome that has formed up or over a vent during a |
3 metre high island formed, composed of a solid | lava dome above the surface. |
The eruption ended with the extrusion of a | lava dome that plugged the vent. |
mal signature of hot ash and rock and a glowing | lava dome on Mount Merapi. |
December 31 1879 up to March 26 1880 produced a | lava dome and had a VEI of 3. The lava dome reached |
of Cerro Chajnantor, a 5640 meter (18,500 feet) | lava dome in the Atacama Desert of northern Chile. |
eter and 70 m deep, and has a 49-m-high central | lava dome that is now partly covered by a crater lak |
Unlike a | lava dome, a resurgent dome is not formed by the ext |
Springs is a small volcanic field of rhyolitic | lava domes and flows in western Nevada, USA, located |
Amorong is one of a cluster of small | lava domes and diatremes. |
Later eruptions formed several | lava domes within the lake and near its shore. |
ts of a cluster of late-Pleistocene to Holocene | lava domes that were associated with thick block-lav |
The Salton Buttes are rhyolite | lava domes within the basin which were active 10,300 |
The Salton Buttes are a group of five small | lava domes in the lower Coachella Valley, in Imperia |
Numerous | lava domes, cinder cones, maars, and lava flows are |
olcanoes, including shield volcanoes, calderas, | lava domes, stratovolcanoes, and cinder cones. |
locene activity, the volcanic field consists of | lava domes, cinder cones, and maars with eruptive pr |
features, including stratovolcanoes, calderas, | lava domes, and cinder cones. |
olcanic caldera on Venus containing steep sided | lava domes. |
y at the big island of Hawaii was caused by the | lava entering the ocean |
Pahoehoe | lava enters the Pacific at Hawaii Volcanoes National |
a where Washington and Oregon are now, basaltic | lava erupted there. |
e eruption is a type of volcanic eruption where | lava erupts under an ocean or sea. |
This type of volcano forms when | lava erupts beneath a thick glacier or ice sheet. |
A | lava escarpment ten feet high formed a southern boun |
xample, a fire drill for ice, a water drill for | lava, etc. |
The eruption, | lava explosions and lava flows were composed of a mi |
Lava extruded from the volcano is primarily trachyda | |
Liquids (water, oil, and | lava) fall from "droppers" and will bounce around th |
located in the southwest corner of Four Craters | Lava Field in the Deschutes National Forest. |
of the Nazcha Creek and comprises the West Tuya | lava field with West Vent and Grizzly Butte. |
of the Nazcha Creek and comprises the West Tuya | lava field with West Vent and Volcano Vent. |
The eruptions from the Four Craters | Lava Field were accompanied by a slight sinking of t |
rently uncommon; growing on a relatively barren | lava field has protected it from fire, animals, and |
Hell's Half Acre | Lava Field, Idaho, USA |
The | lava field, at 1,495 m (4,905 ft) elevation, and its |
They soon end up in | lava fields with Deinonychus and soon the boss, a Eu |
The extent of large | lava fields is most readily grasped from the air or |
ars, a few families have re-built houses on the | lava fields where vegetation is still sparse. |
Starting in the | lava fields, going to a hot geyser field, in a cave, |
constantly-submerged | lava filters (for treatment ponds, combined treatmen |
a series of herringbone drains are placed (with | lava filters these are placed at the bottom layer). |
not-sumerged | lava filters (for wastewater treatment; wastewater i |
on the Isle of Eigg was originally formed as a | lava flow in a valley. |
point of being able to survive submerging in a | lava flow (following the destruction of Davine Lu Li |
The Barrier, a typical ice-marginal | lava flow in the Garibaldi Volcanic Belt of southwes |
S P Crater can be climbed, and the | lava flow can be viewed from the crater rim. |
A | lava flow extends to the north of the cone for ~7 km |
till survive; the remainder being overlaid by a | lava flow that joins to the nearby mare. |
springs, the stream is blocked by a solidified | lava flow and disappears below the surface again. |
or how far the | lava flow was travelling, even the lava lake , pleas |
The source for this | lava flow was the Tseax Cone. |
From the Perl Design Wiki: | Lava Flow is "when code ... spews forth and becomes |
The latter feeds a | lava flow down the west flank. |
ion years old, as well as an adjacent rhyolitic | lava flow using the uranium-lead dating technique. |
In the Vestfold district, one | lava flow was deposited on average every 250,000 yea |
An ice-marginal | lava flow is a lava flow that has impounded against |
It consists of a | lava flow in the Fort Selkirk Volcanic Field of the |
Lava flow is considered an anti-pattern, a commonly | |
Gitlakdamix is located overlooking a | lava flow that erupted in the 18th century. |
Some workers consider the | lava flow to have slightly predated the cinder cone |
A large | lava flow that partly filled Ruby Creek may have ori |
occurs when the outer edges and surfaces of the | lava flow begin to harden. |
In computer programming jargon, | lava flow is a problem in which computer code writte |
cted to a 330 kilometres (210 mi)-long compound | lava flow by a narrow channel. |
flank (excentric) vent, explosive eruption and | lava flow(s). |
such as a newly exposed rock or sand surface, a | lava flow, glacial tills, or a newly formed lake, th |
the Jala eruption, there is record of one major | lava flow, called the Destiladero flow. |
volcano, eruption of just volcanic ash and not | lava flow, not much glowing material, it is not very |
The crater has been covered by | lava flow, leaving only a ring-shaped trace in the s |
its present location just ahead of an advancing | lava flow. |
about 5000 years ago produced a tuff ring and a | lava flow. |
round the steam plumes mark the active vent and | lava flow. |
e forest and crosses a 65-square-mile (170 km2) | lava flow. |
tumuli in plural form) is created in an active | lava flow. |
t appears to be breached with the remnants of a | lava flow. |
It was formed about 1.2 million years ago as | lava flowed down the walls of the Grand Canyon, and |
Wakes are caused by | lava flowing over a source of steam. |
basalt ridge is the product of several massive | lava flows hundreds of feet deep that welled up in f |
They make a hurried escape, chased by | lava flows they find a secret cave and a rocket ship |
The youngest lunar | lava flows identified from orbital images are tentat |
Lava flows have overflowed this western rim and subm | |
As the Earth's crust stretched, volcanoes and | lava flows erupted along a line from Ireland to the |
onsists of a series of continental flood basalt | lava flows of the Mackenzie Large Igneous Province w |
Patterns resembling | lava flows have also been observed, suggesting cryov |
Ice-marginal | lava flows are products of glaciovolcanism. |
is a large number of basaltic cinder cones and | lava flows are located in the Royal Society Range of |
located 7 km to NE and produced basalt-andesite | lava flows that cover an area of 10 km2. |
Basaltic | lava flows often display columnar jointing as a resu |
Lava flows generated by effusive eruptions vary in s | |
Radially spreading | lava flows which have digitate and broad sheet-like |
Pressure ridges also develop on | lava flows when the solid colder top layer is deform |
Basaltic scoria cones and associated | lava flows dominate, but trachytic-phonolitic lava d |
Both land masses' shapes have been formed by | lava flows from volcanic eruptions, causing both sur |
The | lava flows are more viscous, and therefore shorter a |
The lorne plateau lavas are basaltic | lava flows extruded in the late Silurian, -9 million |
Ancient basaltic | lava flows gave birth to much of the region. |
Cooled | lava flows preserved around the volcano keep a recor |
Samples from interlayered limestone in | lava flows provided unreliable palynological data. |
The flood basalt | lava flows are similar to those of the Columbia Rive |
Lava flows are often exacerbated by changes in the d | |
000 years ago during the Pleistocene Ice Age as | lava flows came through the permafrost creating viol |
part due to the presence of dense mare basaltic | lava flows that fill some of the impact basins. |
However, | lava flows by themselves can not explain the entiret |
en one of the first plants to be found on fresh | lava flows and grows in extremely arid conditions. |
the sandstone and shale surrounding the basalt | lava flows of Goffle Hill. |
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