The waters of Marah sweetned A sermon preached at the funeral of Mrs. Clare Wittewronge, eldest daughter to Joseph Alston Esq; and late wife to John Wittewronge Esq;: who was interred at Stantonbury in the county of Bucks. Octob. 22. 1669. By Mr. John Mason, minister.
Mason, John, 1646?-1694
Publisher: printed by John Macock
Place of Publication:
London
Publication Year: 1671
Approximate Era: CharlesII
TCP ID: A52175 ESTC ID: R213830 STC ID: M923
Subject Headings:
Bible. -- N.T. -- Hebrews IX, 27-28;
Funeral sermons -- 17th century;
Wittewrong, Clare, 1644 or 5-1669;
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| Location | Text | Standardized Text | Parts of Speech |
|---|---|---|---|
| In-Text | 2. It is not enough for us to meditate on the Death of Christ, but we must apply it to our selves by a lively Faith, that it may have an influence upon our death. | 2. It is not enough for us to meditate on the Death of christ, but we must apply it to our selves by a lively Faith, that it may have an influence upon our death. | crd pn31 vbz xx av-d p-acp pno12 pc-acp vvi p-acp dt n1 pp-f np1, cc-acp pns12 vmb vvi pn31 p-acp po12 n2 p-acp dt j n1, cst pn31 vmb vhi dt n1 p-acp po12 n1. |
Quotations and Paraphrases (QP)
Adjacent References with Relevance: Romans 6.3 (AKJV)
Only the top predictions per textual unit are considered for adjacency. An adjacent reference is located either in the same or an immediately neighboring segment/note as a given query reference. A reference is relevant to the query if they are identical, parallel texts of each other, or one is a known cross references of the other.
| Verse & Version | Verse Text | Text | Is a Partial Textual Segment/Note | Cosine Similarity Score | Cross Encoder Score | Okapi BM25 Score |
|---|---|---|---|---|---|---|
| Romans 6.3 (AKJV) | romans 6.3: know ye not, that so many of vs as were baptized into iesus christ, were baptized into his death? | 2. it is not enough for us to meditate on the death of christ, but we must apply it to our selves by a lively faith, that it may have an influence upon our death | False | 0.673 | 0.229 | 0.401 |
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