Final answer:
Relative ages of geologic features are determined using principles like cross-cutting relationships and sediment deposition, but without the specific image to refer to, the statements about the age of each feature cannot be confirmed.
Step-by-step explanation:
The student's question pertains to relative dating methods in geology, specifically the principle of cross-cutting relationships, and the sequence of geological events depicted in an image likely related to sequence stratigraphy or a geological map. To determine the correct sequence of events, we use the principle that geologic features like faults, intrusions, or erosion must be younger than the features they affect. Without the specified image, we can't give a definitive answer to the statements provided, but we can explain how to interpret such information:
- Clinoforms are indicative of a sequence of sedimentary layers that are tilted and can help in determining the relative ages of features based on their order of deposition.
- Unconformities suggest a period of erosion or non-deposition that can separate younger strata from older.
- The principle of cross-cutting relations states that the geologic feature which cuts another is the younger of the two.
- Geologic folds, intrusions, faults, and erosional features provide insights into the relative order of events and ages.
For example, if a sedimentary layer is cut by a fault, we know that the fault is younger than the layer. Therefore, using this principle, each statement can be evaluated if we have the image in question. Unfortunately, without the image, it is not possible to determine the truthfulness of each statement.