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Svet_ta [14]
2 years ago
9

Who was the interviewer in interview with marielle tsukamoto

English
2 answers:
OLEGan [10]2 years ago
5 0
The interviewers were 5th-grade students.
RUDIKE [14]2 years ago
3 0
I think it was 5th grade students
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Explanation:

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Importance of sports and games essay of100 words​
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Sports and games can be a great lesson in time management and they provide the spirit of competition that drives them to give extra effort. Through sports children learn to respect authority and rules. Sport increases self-esteem, mental alertness and it reduces stress and anxiety.
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What is the speaker of "the tiger" wondering in the first three stanzas of the poem?
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3 years ago
Which number is the central point
Dafna11 [192]
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3.027 X<br>5/6.00032)<br>(d)<br>823 X<br>5<br>0.00243)<br>ing​
stellarik [79]

Answer:

Serendipity has been recently discovered in the Portage-du-Fort area, Pontiac Regional County Municipality, Quebec. Dark blue, often polysynthetic twinned on {011} and with no cleavage, serendipity crystals occur exclusively in a calc-silicate rock. Fine-grained cathedral serendipity, sometimes poikiloblastic, occurs with aluminous diopside. Less commonly, serendipity may form decussate masses in the same rock type. Serendipity is biaxial negative, with indices of refraction α 1.685(2), β 1.700(2), and γ 1.712(2); 2Vmeas. = 93.6(4)°, 2Vcalc. = 91°. Orientation matrix is X ^ c = +20.5°, Y ^ b = -42.6°, and Z ^ a = -24.6°. Dispersion is strong, r 蠐 v, and there is no pleochroism. Serendipity is triclinic, space group P1¯ with cell parameters refined from an X-ray powder-diffraction pattern: a 10.035(2), b 10.423(3), c 8.648 (2) Å, α 106.47(3)°, β 95.91(2)°, γ 124.46(2)°, V 674.3(2) Å3. The seven strongest lines of the X-ray powder diffraction pattern [d in Å(I)(hill)] are: 3.328(45)(230), 3.029 (96)(012, 021, 1 22), 2.854(96)(01¯3, 03¯1, 120), 2.689(29)(31¯1), 2.604(95)(030), 2.469(100)(2¯1¯3, 033), and 2.357(28)(22¯3, 23¯3). The crystal structure determination refined to R = 2.1% for 3877 unique reflections. The borosilicate structure, a member of the aenigmatite-rhenate group, is composed of layers parallel to (011). Layers of tetrahedral chains cross-linked by octahedral polyhedral alternate with layers of octahedral chains cross-linked by square antiprism polyhedral sheets. Tetrahedral and octahedral polyhedral are partially ordered and site assignments were determined. All cation sites are disordered to some degree.

Explanation:

4 0
2 years ago
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