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Reptile [31]
3 years ago
12

1) Stage 1: What is a property of gas?

Biology
1 answer:
Kazeer [188]3 years ago
6 0

Answer:

1.a

2.c

3.a

4.c (that's the closest)

5.d

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PLS HELP!! brainliest + extra points! it's easy but i didn't study tbh:)
NISA [10]

Answer:

Guanine to Cytosine

Explanation:

G always matches C

A always matches T

Hope it helps

Plz mark Brainiest.

4 0
3 years ago
Plz hurry, drag the characteristics to the rna and dna columns where they belong
Luda [366]

Answer:

RNA - single stranded, contains uracil, and protein synthesis.

DNA - Double stranded, contains thymine, and stored genetic material.

Hope that helps! :)

3 0
3 years ago
Help!!
mario62 [17]

Answer:

well you either have eukaryotic or prokaryotes : Eukaryotic being us humans (the one special thing we have in are cells to function is a Nucleus, which holds genetic material), and then Prokaryotic which just dont have a Nucleus

6 0
2 years ago
Why are we still here? just to suffer
sergiy2304 [10]

Answer:

and We were born just to die

3 0
3 years ago
Read 2 more answers
What are the characteristics of a cinder cone?​
yKpoI14uk [10]
Cinder cones derive their name from their steep sides, which give them a cone-like appearance. The angle of their slopes may be as steep as 35 degrees, although older, eroded cones have softer slopes. Cinder cones are small compared to other types of volcanoes. They average 100 to 400 meters in height (325 to 1,300 feet), while composite volcanoes may reach 3,500 meters (11,500 feet) and shield volcanoes can range as high as 8,500 meters (28,000 feet) -- the height of Hawaii's Mauna Loa, the world's largest, as measured from the ocean floor to its top. Most cinder cones are monogenetic, which means they erupt only once. Their eruptions tend to be relatively weak compared to those of larger volcanoes. Cinder cones often form as parasite cones along the flanks of larger volcanoes. They are formed by Strombolian eruptions, when gas forces steaming lava upwards into the air. The lava cools and falls to the earth as pebbles, which build up around the vent that ejected them, forming a cone. These parasite types of cone volcanoes usually occur in groups. Shifts in the position of the vent result in twin cinder cones. Variations in the power of eruption create nested cones. Not all cinder cones are found in groups; some are separate entities formed on basaltic lava fields.
6 0
3 years ago
Read 2 more answers
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