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Corolla tube cylindric or campanulate, widest at throat or with parallel sides.

花冠筒圆筒状的或钟状,宽在喉部或具平行的边。

Inflorescence a dichasium, arising from leaf axils near branch apex, long peduncled; flowers white, ca. 6 mm in diam.; sepals 5, base connate, ovate-oblong, ca. 3 mm long; petals 5, broadly orbicular, 2.5 times as long as sepals; stamens 10, exserted, up to 2 cm long.

二歧聚伞花序生於枝的近顶端叶腋部,具长的总花梗;花白色,直径约6毫米;萼片5片,基部合生,卵状长圆形,长约3毫米;花瓣5片,阔圆形,约长於萼片1.5倍;雄蕊10枚,伸出花冠外,长达2厘米。

Corolla purple, with purple galea; galea twisted.

花冠紫色,具紫色的盔瓣;盔瓣扭曲。

Corolla galea often navicular; beak short.

花冠盔瓣通常舟形;具喙的短。

Corona lobes as high as anthers and with interior angle forming an acute tooth incumbent on top of the anthers; inflorescences long pedunculate umbel-like clusters of cymules; follicles often with longitudinal or transverse ridges or wings

象花药并且具内角形成一有义务的锐尖齿在花药之上的一样高的副花冠裂片;花序长花序梗小聚伞花序的象伞形花序一样的簇生;蓇葖果通常具纵向的或横裂的脊或翅 35 Dregea 南山藤属

Cm; labellum with yellow midvein and purple stripes on each side, ca.

花冠裂片玫瑰色,椭圆形,约3厘米;唇瓣具黄的中脉和紫色的条纹在每边,约 3.2 * 1.6 厘米 6 AMOMUM scarlatinum 红花砂仁

Corolla galea navicular; beak short.

花冠盔瓣舟形;具喙的短。

Lighter than thistledown, it is as fragile and ephemeral as it is stunning to behold.

比蓟花冠毛还要轻,脆弱,转瞬即逝,却有一种极具冲击力的美。

Corolla campanulate; leaf blade with distant teeth or subentire.

花冠钟状叶片具远的齿或近全缘。

Biennial herbs; corolla with spreading limb, 4-6(-8) mm across.

二年生草本花冠具平展的瓣片,4-6(-8)毫米直径。

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Finally, according to market conditions and market products this article paper analyzes the trends in the development of camera technology, and designs a color night vision camera.

最后根据市场情况和市面上产品的情况分析了摄像机技术的发展趋势,并设计了一款彩色夜视摄像机。

Only person height weeds and the fierce looks stone idles were there.

只有半人深的荒草和龇牙咧嘴的神像。

This dramatic range, steeper than the Himalayas, is the upturned rim of the eastern edge of Tibet, a plateau that has risen to 5 km in response to the slow but un stoppable collision of India with Asia that began about 55 million years ago and which continues unabated today.

这一引人注目的地域范围,比喜马拉雅山更加陡峭,是处于西藏东部边缘的朝上翻的边框地带。响应启始于约5500万年前的、缓慢的但却不可阻挡的印度与亚洲地壳板块碰撞,高原已上升至五千米,这种碰撞持续至今,毫无衰退。