查询词典 lava-capped

Its volcanic geological formation is complicated, varying from hard lava magmas to weathering pyroclastic debris.

火山形成的地层非常复杂，从坚硬的火山熔岩到松软风化的火山碎屑堆积物都有存在。

It is capable of intrusion into adjacent rocks or of extrusion onto the surface as lava or ejected explosively as tephra to form pyroclastic rock .

它有能力入侵到邻近的石块或挤压到表面的熔岩或跳伞爆炸性作为火山灰形成火山碎屑岩。

Whole towns have been wiped out by poisonous gases from volcanoes even before they were hit with pyroclastic flows or lava.

在整个村庄遭到火山灰流或熔岩的袭击之前，为了躲避来自火山的有毒气体，人们已经筋疲力尽。

Eruptions typically result in the construction of large, steep-sided, composite or strato volcanoes made up of alternating lava flows and pyroclastic deposits.

爆发通常会导致建造大型陡，片面的，综合或平流火山成立的交替熔岩流和火山的存款。

Whole towns have been wiped out by poisonous gases from volcanoes even before they were hit with pyroclastic flows or lava

在火山熔岩吞噬整个村庄前，火山毒气很有可能已经横扫整个城镇。

But, the crust rocks (included to accumulating complex, sheeted sill complex and lava) is formed by crystallization of the magma. The different rock associations of pyroxenite gabbro and troctolite gabbro in the accumulating complex are related to depth of formation of magmatic chambers and oxidation state of magma in the spreading ridge.

而壳层岩石(指堆积杂岩、岩墙杂岩、熔岩)则是由岩浆结晶作用形成的；堆积杂岩中出现辉石岩辉长岩和橄长岩辉长岩的不同岩石组合则与堆积岩岩浆房出露的深度和氧化状态有关。

During an eruption of volcano, scalding lava was ejected from it.

火山爆发时，滚烫的熔岩从里喷出。

The scoria cones surrounding the fissure are black, as is the lava flow extending to the northeast.

周围的火山渣锥是黑色的裂缝，由于是熔岩流延伸到东北部。

The scene becomes a panorama of desolation, of rocks and scrubby trees, lava fields and herds of goats.

周围变得越来越荒凉：岩石、矮小的树丛、熔岩地和成群的山羊。

The rocks from Sharp Island are of volcanic origin. One of the examples is the rhyolite formed by viscous lava spewed from the volcano vents can be found near the caldera edge. The southern part of Jin Island was being eroded by waves which led the head land was separared from the main rock to form sea stack called "Tiu Chung Rock". As the erosion proceeds, there is a 30m high long sea arch developed called "Tiu Chung Arch".

桥咀洲的岩石大多源於火山，其中包括流纹岩，由附近火山喷道喷出的稠熔岩形成，属破火山口边的产物；吊钟洲南面长期受著海浪拍打侵蚀，使岬角与岩体分离形成海蚀柱名为「吊钟岩」，因海浪持续的侵蚀，岩中续渐形成一个高30米的长形海蚀拱「吊钟洞」。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。