Question

this process happens in ________ or ________,
which are both areas that experience a lot of deposition of
sediment. it is due to their ______________ levels and
__________ to sediment that washed down with the rain.

even though the sediment is compressed together, the
individual sediment grains are still __________, which
means that there are tiny pockets of __________ in
between each individual sediment grain. this also means that
no ________ transformation has happened, the sediment is simply ________ together.

cementation
__________ involves the final step in turning grains of
sediment into actual rock. it is the process where sediment
are ______________ together when minerals
precipitate from the water they are dissolved in and fill the
______________ between compressed sediment.

______________ is water with certain quantities of
minerals mixed into it. minerals in the supersaturated
water are ______________ out and become the
__________ that holds sedimentary rock together.
minerals that form cement include __________,
________, and other ________.

Explanation:

To solve this fill - in - the - blank problem about sedimentary rock formation (compaction and cementation), we analyze each blank based on geological knowledge:

Part 1: Compaction - Related Blanks

1. Areas of Deposition: Sediment deposition is common in low - energy environments like lakes and oceans (or river deltas, but lakes and oceans are typical). So the first two blanks can be "lakes" and "oceans" (or other low - lying, sediment - accumulating areas like river deltas).
2. Reasons for Deposition: These areas have low elevation (low levels) and are receptive (or "exposed" or "prone") to sediment carried by rain. So the next two blanks: "low" (for elevation) and "receptive" (or "prone" etc. to describe their relationship with sediment).
3. Sediment Grain State After Compaction: After compaction, sediment grains are still separate (they haven't undergone chemical change yet). So the next blank is "separate".
4. Pockets Between Sediment Grains: Between separate sediment grains, there are tiny pockets of air or water. So the next blank is "air" (or "water").
5. Type of Transformation: Since the grains are just compressed, no chemical transformation has occurred. So the next blank is "chemical".
6. Sediment State After Compaction: The sediment is simply "compressed" together.

Part 2: Cementation - Related Blanks

1. Process Name: The process that is the final step in turning sediment into rock is "Cementation". So the first blank here is "Cementation".
2. Sediment in Cementation: In cementation, sediment grains are "cemented" (or "bound") together. So the next blank is "cemented".
3. Spaces Filled in Cementation: Minerals precipitate and fill the "pores" (or "spaces") between compressed sediment. So the next blank is "pores".
4. Type of Water in Cementation: The water with dissolved minerals is "supersaturated water". So the next blank is "Supersaturated water".
5. Mineral Action in Supersaturated Water: Minerals in supersaturated water are "precipitated" out. So the next blank is "precipitated".
6. Substance Holding Sediment Together: The precipitated minerals become the "cement" that holds sedimentary rock together. So the next blank is "cement".
7. Minerals for Cement: Common cement - forming minerals are calcite, silica (quartz), and other minerals like iron oxides. So the last three blanks can be "calcite", "silica", and "minerals".

Final Answers (Filling the Blanks in Order)

1. lakes; oceans (or other suitable sediment - depositing areas)
2. low; receptive (or other appropriate adjectives)
3. separate
4. air (or water)
5. chemical
6. compressed
7. Cementation
8. cemented
9. pores
10. Supersaturated water
11. precipitated
12. cement
13. calcite; silica; minerals (answers may vary slightly based on textbook - specific terminology, but these are the standard concepts)

Answer:

To solve this fill - in - the - blank problem about sedimentary rock formation (compaction and cementation), we analyze each blank based on geological knowledge:

Part 1: Compaction - Related Blanks

1. Areas of Deposition: Sediment deposition is common in low - energy environments like lakes and oceans (or river deltas, but lakes and oceans are typical). So the first two blanks can be "lakes" and "oceans" (or other low - lying, sediment - accumulating areas like river deltas).
2. Reasons for Deposition: These areas have low elevation (low levels) and are receptive (or "exposed" or "prone") to sediment carried by rain. So the next two blanks: "low" (for elevation) and "receptive" (or "prone" etc. to describe their relationship with sediment).
3. Sediment Grain State After Compaction: After compaction, sediment grains are still separate (they haven't undergone chemical change yet). So the next blank is "separate".
4. Pockets Between Sediment Grains: Between separate sediment grains, there are tiny pockets of air or water. So the next blank is "air" (or "water").
5. Type of Transformation: Since the grains are just compressed, no chemical transformation has occurred. So the next blank is "chemical".
6. Sediment State After Compaction: The sediment is simply "compressed" together.

Part 2: Cementation - Related Blanks

1. Process Name: The process that is the final step in turning sediment into rock is "Cementation". So the first blank here is "Cementation".
2. Sediment in Cementation: In cementation, sediment grains are "cemented" (or "bound") together. So the next blank is "cemented".
3. Spaces Filled in Cementation: Minerals precipitate and fill the "pores" (or "spaces") between compressed sediment. So the next blank is "pores".
4. Type of Water in Cementation: The water with dissolved minerals is "supersaturated water". So the next blank is "Supersaturated water".
5. Mineral Action in Supersaturated Water: Minerals in supersaturated water are "precipitated" out. So the next blank is "precipitated".
6. Substance Holding Sediment Together: The precipitated minerals become the "cement" that holds sedimentary rock together. So the next blank is "cement".
7. Minerals for Cement: Common cement - forming minerals are calcite, silica (quartz), and other minerals like iron oxides. So the last three blanks can be "calcite", "silica", and "minerals".

Final Answers (Filling the Blanks in Order)

1. lakes; oceans (or other suitable sediment - depositing areas)
2. low; receptive (or other appropriate adjectives)
3. separate
4. air (or water)
5. chemical
6. compressed
7. Cementation
8. cemented
9. pores
10. Supersaturated water
11. precipitated
12. cement
13. calcite; silica; minerals (answers may vary slightly based on textbook - specific terminology, but these are the standard concepts)